This page lists publications and reports for studies and projects that we are aware used MGET in some way. If you know of something that is not listed here, please @


Lins L, Guilini K, Veit-Köhler G, Hauquier F, Alves RMS, Esteves AM, Vanreusel A (in press) The link between meiofauna and surface productivity in the Southern Ocean. Deep Sea Research Part II: Topical Studies in Oceanography. doi: 10.1016/j.dsr2.2014.05.003

Mugo R, Saitoh S-I, Takahashi F, Nihira A, Kuroyama T (in press) Evaluating the role of fronts in habitat overlaps between cold and warm water species in the western North Pacific: A proof of concept, Deep Sea Research Part II: Topical Studies in Oceanography. doi: 10.1016/j.dsr2.2013.11.005


Afán I, Navarro J, Cardador L, Ramírez F, Kato A, Rodríguez B, Ropert-Coudert Y, Forero MG (2014) Foraging movements and habitat niche of two closely related seabirds breeding in sympatry. Marine Biology 161: 657-668. doi: 10.1007/s00227-013-2368-4

McClellan CM, Brereton T, Dell’Amico F, Johns DG, Cucknell A-C, et al. (2014) Understanding the Distribution of Marine Megafauna in the English Channel Region: Identifying Key Habitats for Conservation within the Busiest Seaway on Earth. PLoS ONE 9(2): e89720. doi: 10.1371/journal.pone.0089720

Farrell ER, Boustany AM, Halpin PN, Hammond DL (2014) Dolphinfish (Coryphaena hippurus) distribution in relation to biophysical ocean conditions in the northwest Atlantic. Fisheries Research 151: 177-190. doi: 10.1016/j.fishres.2013.11.014

Fontes J, Schmiing M, Afonso P (2014) Permanent aggregations of a pelagic predator at shallow seamounts. Marine Biology 161: 1349-1360. doi: 10.1007/s00227-014-2423-9

Miller RR, Field JC, Santora JA, Schroeder ID, Huff DD, et al. (2014) A Spatially Distinct History of the Development of California Groundfish Fisheries. PLoS ONE 9(6): e99758. doi: 10.1371/journal.pone.0099758

Williams R, Kelly N, Boebel O, Friedlaender AS, Herr H, Kock K-H, Lehnert LS, Maksym T, Roberts J, Scheidat M, Siebert U, Brierley AS (2014) Counting whales in a challenging, changing environment. Scientific Reports 4: 4170. doi: 10.1038/srep04170


Abdul-Hadi A, Mansor S, Pradhan B, Tan KC (2013) Seasonal variability of chlorophyll-a and oceanographic conditions in Sabah waters in relation to Asian monsoon—a remote sensing study. Environmental Monitoring and Assessment 185: 3977-3991. doi: 10.1007/s10661-012-2843-2

Álvarez-Romero JG, Devlin M, da Silva ET, Petus C, Ban NC, Pressey RL, Kool J, Roberts JJ, Cerdeira-Estrada S, Wenger AS, Brodie J (2013) A novel approach to model exposure of coastal-marine ecosystems to riverine flood plumes based on remote sensing techniques. Journal of Environmental Management 119: 194-207. doi: 10.1016/j.jenvman.2013.01.036

Boehm JT, Woodall L, Teske PR, Lourie SA, Baldwin C, Waldman J, Hickerson M (2013) Marine dispersal and barriers drive Atlantic seahorse diversification. Journal of Biogeography. doi: 10.1111/jbi.12127

Cecere JG, Calabrese L, Rocamora G, Catoni C (2013) Movement Patterns and Habitat Selection of Wedge-tailed Shearwaters (Puffinus pacificus) Breeding at Aride Island, Seychelles. Waterbirds 36(4): 432-437. doi: 10.1675/063.036.0414

Chesney TA, Heppell SA, Montero J, Graham J (2013) Interannual Variability of humboldt squid (Dosidicus gigas) off Oregon and southern Washington. CalCOFI Rep., Vol. 54, 2013. PDF

Coelho R, Infante P, Santos MN (2013) Application of Generalized Linear Models and Generalized Estimation Equations to model at-haulback mortality of blue sharks captured in a pelagic longline fishery in the Atlantic Ocean. Fisheries Research 145: 66-75. doi: 10.1016/j.fishres.2013.02.010

Crochelet E, Chabanet P, Pothin K, Lagabrielle E, Roberts J, Pennober G, Lecomte-Finiger R, Petit M (2013) Validation of a fish larvae dispersal model with otolith data in the Western Indian Ocean and implications for marine spatial planning in data-poor regions. Ocean and Coastal Management 86: 13-21. doi: 10.1016/j.ocecoaman.2013.10.002

Fernández M, Hamilton H, Kueppers LM (2013) Characterizing uncertainty in species distribution models derived from interpolated weather station data. Ecosphere 4:art61. doi: 10.1890/ES13-00049.1

Foley AM, Schroeder BA, Hardy R, MacPherson SL, Nicholas M, Coyne MS (2013) Postnesting migratory behavior of loggerhead sea turtles Caretta caretta from three Florida rookeries. Endangered Species Research 21: 129-142. doi: 10.3354/esr00512

Gorman D, Bajjouk T, Populus J, Vasquez M, Ehrhold A (2013) Modeling kelp forest distribution and biomass along temperate rocky coastlines. Marine Biology 160: 309-325. doi: 10.1007/s00227-012-2089-0

Lua L, Guo H, Wang C, Li Q (2013) Assessment of the SeaWinds scatterometer for vegetation phenology monitoring across China. International Journal of Remote Sensing 34: 5551-5568. doi: 10.1080/01431161.2013.794986

Mattio L, Zubia M, Loveday B, Crochelet E, Duong N, Payri CE, Bhagooli R, Bolton JJ (2013) Sargassum (Fucales, Phaeophyceae) in Mauritius and Réunion, western Indian Ocean: taxonomic revision and biogeography using hydrodynamic dispersal models. Phycologia 52(6): 578-594. doi: 10.2216/13-150.1

Muhling BA, Reglero P, Ciannelli L, Alvarez-Berastegui D, Alemany F, Lamkin JT, Roffer MA (2013) Comparison between environmental characteristics of larval bluefin tuna Thunnus thynnus habitat in the Gulf of Mexico and western Mediterranean Sea. Marine Ecology Progress Series 486: 257-276. doi: 10.3354/meps10397

Palaiologou P, Kalabokidis K, Kyriakidis P (2013) Forest mapping by geoinformatics for landscape fire behaviour modelling in coastal forests, Greece. International Journal of Remote Sensing 34: 4466-4490. doi: 10.1080/01431161.2013.779399

Pikesley SK, Maxwell SM, Pendoley K, Costa DP, Coyne MS, Formia A, Godley BJ, Klein W, Makanga-Bahouna J, Maruca S, Ngouessono S, Parnell RJ, Pemo-Makaya E, Witt MJ (2013) On the front line: integrated habitat mapping for olive ridley sea turtles in the southeast Atlantic. Diversity and Distributions. doi: 10.1111/ddi.12118

Regueira M, González AF, Guerra A (2013) Habitat selection and population spreading of the horned octopus Eledone cirrhosa(Lamarck, 1798) in Galician waters (NW Atlantic). Fisheries Research. doi: 10.1016/j.fishres.2013.09.003

Ross RE, Howell KL (2013) Use of predictive habitat modelling to assess the distribution and extent of the current protection of ‘listed’ deep-sea habitats. Diversity and Distributions 19: 433-445. doi: 10.1111/ddi.12010

Schick RS, Roberts JJ, Eckert SA, Halpin PN, Bailey H, Chai F, Shi L, Clark JS (2013) Pelagic movements of Pacific Leatherback Turtles (Dermochelys coriacea) highlight the role of prey and ocean currents. Movement Ecology 1: 11. doi: 10.1186/2051-3933-1-11


Alonso H, Granaderio JP, Paiva VH, Dias AS, Ramos JA, Catry P (2012) Parent–offspring dietary segregation of Cory’s shearwaters breeding in contrasting environments. Marine Biology 159: 1197-1207. doi: 10.1007/s00227-012-1900-2

Best BD, Halpin PN, Read AJ, Fujioka E, Good CP, LaBrecque EA, Schick RS, Roberts JJ, Hazen LJ, Qian SS, Palka DL, Garrison LP, McLellan WA (2012) Online cetacean habitat modeling system for the US east coast and Gulf of Mexico. Endangered Species Research 18: 1-15. doi: 10.3354/esr00430

Dalla Rosa L, Ford KJB, Trites AW (2012) Distribution and relative abundance of humpback whales in relation to environmental variables in coastal British Columbia and adjacent waters. Continental Shelf Research 36: 89-104. doi: 10.1016/j.csr.2012.01.017

Dellabianca N, Scioscia G, Schiavini A, Raya Rey A (2012) Occurrence of hourglass dolphin (Lagenorhynchus cruciger) and habitat characteristics along the Patagonian Shelf and the Atlantic Ocean sector of the Southern Ocean. Polar Biology 35: 1921-1927. doi: 10.1007/s00300-012-1217-0

Krigsman LM, Yoklavich MM, Dick EJ, Cochrane GR (2012) Models and maps: predicting the distribution of corals and other benthic macro-invertebrates in shelf habitats. Ecosphere 3: 3. doi: 10.1890/ES11-00295.1

Lydersen C, Freitas C, Wiig Ø, Bachmann L, Heide-Jørgensen MP, Swift R, Kovacs KM (2012) Lost Highway Not Forgotten: Satellite Tracking of a Bowhead Whale (Balaena mysticetus) from the Critically Endangered Spitsbergen Stock. Arctic 65: 76-86. PDF

McKinney JA, Hoffmayer ER, Wu W, Fulford R, Hendon JM (2012) Feeding habitat of the whale shark Rhincodon typus in the northern Gulf of Mexico determined using species distribution modelling. Marine Ecology Progress Series 458: 199-211. doi: 10.1890/ES11-00295.1

Monk J, Ierodiaconou D, Harvey E, Rattray A, Versace VL (2012) Are We Predicting the Actual or Apparent Distribution of Temperate Marine Fishes? PLoS One 7: e34558. doi: 10.1371/journal.pone.0034558

Mora C, Treml EA, Roberts J, Crosby K, Roy D, Tittensor DP (2012) High connectivity among habitats precludes the relationship between dispersal and range size in tropical reef fishes. Ecography 35: 89-96. doi: 10.1111/j.1600-0587.2011.06874.x

Neves VC, Bried J, González-Solís J, Roscales JL, Clarke MR (2012) Feeding ecology and movements of the Barolo shearwater Puffinus baroli baroli in the Azores, NE Atlantic. Marine Ecology Progress Series 452: 269.285. doi: 10.3354/meps09670

Payne MC, Brown CA, Reusser DA, Lee II H (2012) Ecoregional Analysis of Nearshore Sea-Surface Temperature in the North Pacific. PLoS ONE 7: e30105. doi: 10.1371/journal.pone.0030105

Robert A, Paiva VH, Bolton M, Jiguet F, Bried J (2012) The interaction between reproductive cost and individual quality is mediated by oceanic conditions in a long-lived bird. Ecology 93: 1944-1952. doi: 10.1890/11-1840.1

Tamburello L, Benedetti-Cecchi L, Ghedini G, Alestra T, Bulleri F (2012) Variation in the structure of subtidal landscapes in the north-western Mediterranean Sea. Marine Ecology Progress Series 457: 29-41. 10.3354/meps09703

Tomlinson CJ, Thornes JE, Baker CJ (2012) Derivation of Birmingham’s summer surface urban heat island from MODIS satellite images. International Journal of Climatology 32: 214-224. doi: 10.1002/joc.2261

Treml EA, Halpin PN (2012) Marine population connectivity identifies ecological neighbors for conservation planning in the Coral Triangle. Conservation Letters 5: 441-449. doi: 10.1111/j.1755-263X.2012.00260.x

Ubertini M, Lefebvre S, Gangnery A, Grangeré K, Le Gendre R, Orvain F (2012) Spatial Variability of Benthic-Pelagic Coupling in an Estuary Ecosystem: Consequences for Microphytobenthos Resuspension Phenomenon. PLoS ONE 7: e44155. doi: 10.1371/journal.pone.0044155


Payne MC, Reusser DA, Lee II H, Brown CA (2011) Moderate-resolution sea surface temperature data for the nearshore North Pacific: U.S. Geological Survey Open-File Report 2010-1251.

Lydersen C, Freitas C, Wiig Ø, Bachmann L, Heide-Jørgensen, Swift R, Kovacs KM (2011) Lost Highway Not Forgotten: Satellite Tracking of a Bowhead Whale (Balaena mysticetus) from the Critically Endangered Spitsbergen Stock. Arctic 65: 76-86.

Mugo R, Saitoh S-I, Nihira A, Kuroyama T (2011) Application of Multi-Sensor Satellite and Fishery Data, Statistical Models and Marine-GIS to Detect Habitat Preferences of Skipjack Tuna. In: Morales J, Stuart V, Platt T, Sathyendranath S, editors. Handbook of Satellite Remote Sensing Image Interpretation: Applications for Marine Living Resources Conservation and Management, EU PRESPO and IOCCG, Dartmouth, Canada, pp 169-185. PDF

Pohle G, Iken K, Clarke KR, Trott T, Konar B, et al. (2011) Aspects of Benthic Decapod Diversity and Distribution from Rocky Nearshore Habitat at Geographically Widely Dispersed Sites. PLoS ONE 6(4): e18606. doi: 10.1371/journal.pone.0018606

Scheidat M, Friedlaender A, Kock K-H, Lehnert L, Boebel O, Roberts J, Williams R (2011) Cetacean surveys in the Southern Ocean using icebreaker-supported helicopters. Polar Biology 34: 1513-1522. doi: 10.1007/s00300-011-1010-5

Schick RS, Halpin PN, Read AJ, Urban DL, Best BD, Good CP, Roberts JJ, LaBrecque EA, Dunn C, Garrison LP, Hyrenbach KD, McLellan WA, Pabst DA, Palka DL, Stevick P (2011) Community structure in pelagic marine mammals at large spatial scales. Marine Ecology Progress Series 434: 165–181. doi: 10.3354/meps09183

Wooton CE, Klinkenberg B (2011) A landscape-level analysis of yellow-cedar decline in coastal British Columbia. Canadian Journal of Forest Research 41: 1638-1648. doi: 10.1139/x11-061

Žydelis R, Lewison RL, Shaffer SA, Moore JE, Boustany AM, Roberts JJ, Sims M, Dunn DC, Best BD, Tremblay Y, Kappes MA, Halpin PN, Costa DP, Crowder LB (2011) Dynamic habitat models: Using telemetry data to project fisheries bycatch. Proceedings of the Royal Society B 278: 3191-3200. doi: 10.1098/rspb.2011.0330


Benedetti-Cecchi L, Iken K, Konar B, Cruz-Motta J, Knowlton A, et al. (2010) Spatial Relationships between Polychaete Assemblages and Environmental Variables over Broad Geographical Scales. PLoS ONE 5: e12946. doi: 10.1371/journal.pone.0012946

Kalabokidis K, Palaiologou P, Kyriakidis P (2010) Forest Fire Fuels Mapping by Geoinformatics for Fire Behavior Modeling. Proceedings of the VI International Conference on Forest Fire Research, Coimbra, Portugal, 15-18 November 2010. PDF

Mugo R, Saitoh S, Nihira A, Kuroyama T (2010) Habitat characteristics of skipjack tuna (Katsuwonus pelamis) in the western North Pacific: a remote sensing perspective. Fisheries Oceanography 19: 382-396. doi: 10.1111/j.1365-2419.2010.00552.x

Williams R, Friedlaender A, Kock K-H, Lehnert L, Roberts J, Scheidat M (2010) Antarctic minke whale density in relation to sea ice: helicopter surveys in the Weddell Sea. Paper SC/62/IA13 presented to the Scientific Committee of the International Whaling Commission. PDF

Young MA, Iampietro PJ, Kvitek RG, Garza CD (2010) Multivariate bathymetry-derived generalized linear model accurately predicts rockfish distribution on Cordell Bank, California, USA. Marine Ecology Progress Series 415: 247–261. doi: 10.3354/meps08760


Ardron J, Dunn D, Corrigan C, Gjerde K, Halpin P, Rice J, Vanden Berghe E, Vierros M (2009) Defining ecologically or biologically significant areas in the open oceans and deep seas: Analysis, tools, resources and illustrations: A background document for the Convention on Biological Diversity expert workshop on scientific and technical guidance on the use of biogeographic classification systems and identification of marine areas beyond national jurisdiction in need of protection, Ottawa, Canada, 29 September – 2 October 2009. PDF

Lagabrielle E, Maina J, Massé L, Séré M, Watson R (2009) Mapping anthropogenic drivers of change for biodiversity conservation planning in the Western Indian Ocean. Report prepared for: Marine Protected Area Network of the Indian Ocean Commission countries, Indian Ocean Commission Project implemented by WWF Madagascar & West Indian Ocean Programme Office, study funded by FFEM, 53 p. PDF

Louzao M, Bécares J, Rodríguez B, Hyrenbach KD, Ruiz A, Arcos JM (2009) Combining vessel-based surveys and tracking data to identify key marine areas for seabirds. Marine Ecology Progress Series 391: 183-197. doi: 10.3354/meps08124

McClellan CM, Read AJ (2009) Confronting the gauntlet: understanding incidental capture of green turtles through fine-scale movement studies. Endangered Species Research 10: 165-179. doi: 10.3354/esr00199

Schick RS, Halpin PN, Read AJ, Slay CK, Kraus SD, Mate BR, Baumgartner MF, Roberts JJ, Best BD, Good CP, Loarie SR, Clark JS (2009) Striking the right balance in right whale conservation. Canadian Journal of Fisheries and Aquatic Sciences 66: 1399-1403. doi: 10.1139/F09-115

Schmiing M, Afonso P, Tempera F, Santos R (2009) Integrating Recent and Future Marine Technology in the Design of Marine Protected Areas – the Azores as Case Study. Proceedings of OCEANS´09 IEEE Bremen, Balancing technology with future needs, Bremen (Germany), 11-14 May 2009. doi: 10.1109/OCEANSE.2009.5278178


Eckert SA, Moore JE, Dunn DC, van Buiten RC, Eckert KL, Halpin PN (2008) Modeling Loggerhead Turtle Movement in the Mediterranean: Importance of Body Size and Oceanography. Ecological Applications 18: 290-308. doi: 10.1890/06-2107.1

Iampietro PJ, Young MA, Kvitek RG (2008) Multivariate Prediction of Rockfish Habitat Suitability in Cordell Bank National Marine Sanctuary and Del Monte Shalebeds, California, USA. Marine Geodesy 31: 359-371. doi: 10.1080/01490410802466900

Lennert-Cody CE, Roberts JJ, Stephenson RJ (2008) Effects of gear characteristics on the presence of bigeye tuna (Thunnus obesus) in the catches of the purse-seine fishery of the eastern Pacific Ocean. ICES Journal of Marine Science 65: 970-978. doi: 10.1093/icesjms/fsn075

In MGET 0.8a42, we introduced a simplified workflow for predictive modeling, shown here for generalized linear models (GLMs).

The new workflow is the same for all model types (GLM, GAM, etc.) and consists of three steps:

  • Fit the model to training data in a table. This works the same as before. The model formula specifies the fields of the input table will be used as the response variable and predictor variables.
  • Evaluate the predictive power of the fitted model by performing predictions on test data in a table and comparing the predicted values of the response variable to the observed values. This uses a new tool, Predict <Model Type> From Table, which provides new functionality and replaces the Plot ROC of Binary Classification Model and the Plot Performance of Binary Classification Model tools. The new tool generates ROC and other plots for binary models, as well as new summary statistics, including Cohen’s Kappa (for classification models) and Kendall’s tau and % Variance Explained (for regression models). The new tool can also (optionally) store the predicted values back to the table, so you can perform your own comparison of the predicted and observed values.
  • Create a raster for the response variable by performing predictions on rasters representing the predictor variables. This works the same as before but new parameters have been added to allow you to specify constant values for predictor variables that do not vary spatially and therefore do not have rasters representing them. In previous versions of MGET, these variables could only be supplied by generating a constant raster having the necessary value; that awkward design has been eliminated.

As part of our recent overhaul of the predictive modeling tools, we added support for random forests as a new modeling type.

Random forest (Breiman, 2001) is machine learning algorithm that fits many classification or regression tree (CART) models to random subsets of the input data and uses the combined result (the forest) for prediction. A principal feature of random forests is their ability to estimate the importance of each predictor variable in modeling the response variable. MGET’s Fit Random Forest Model tool outputs the importance estimate as text and a plot:

The tool can also output partial dependence plots that show the effect of each predictor on the response variable when the rest of the predictors are held constant:

MGET’s tools can fit both classification and regression forests using either the R randomForest package (Liaw and Wiener, 2002) which implements Breiman’s classic algorithm, or the cforest function from the R party package (Hothorn et al, 2006; Strobl et al, 2007; Strobl et al, 2008).

For a detailed description of random forests and practical advice their application in ecology, see Cutler et al. (2007).


Breiman L (2001) Random forests. Machine Learning, 45: 5-32.

Cutler DR, Edwards Jr. TC, Beard KH, Cutler A, Hess KT, Gibson J, Lawler JJ (2007) Random Forests for Classification in Ecology. Ecology 88: 2783-2792.

Hothorn T, Buehlmann P, Dudoit S, Molinaro A, Van Der Laan M (2006) Survival Ensembles. Biostatistics 7: 355-373.

Liaw A and Wiener M (2002) Classification and Regression by randomForest. R News 2: 18-22.

Strobl S, Boulesteix A-L, Kneib T, Augustin T, Zeileis A (2008) Conditional Variable Importance for Random Forests. BMC Bioinformatics 9: 307.

Strobl S, Boulesteix A-L, Zeileis A, Hothorn T (2007) Bias in Random Forest Variable Importance Measures: Illustrations, Sources and a Solution. BMC Bioinformatics 8: 25.

For additional help with these tools, please contact

We are pleased to announce a major update to MGET’s larval connectivity modeling tools. Prior to MGET 0.8a62, the larval connectivity modeling tools were based on the approach described in Treml et al. (2008). In MGET 0.8a62, we added new tools that implement the Treml et al. (2012) approach, which provides numerous advantages, including:


  • Larvae now settle. The old approach dispersed larvae without settling them and reported connections between patches based on the maximum number of larvae dispersed by a source patch that were suspended over a destination patch over the course the the simulation. In the new approach, when larvae drift over a patch they settle there and are removed from the simulation and become unavailable to downstream patches, providing a more realistic simulation of dispersal.
  • Competency and settlement behavior are configurable. You can control the rate at which larvae become competent to settle (via a gamma cumulative distribution function), the rate that they settle over habitat patches once they are competent (via a simple linear rate), and whether all larvae within a grid cell can sense and move to the habitat available there, or just the fraction that are over that habitat (i.e. whether or not the larvae have a “sensory zone”).
  • The advection algorithm is more accurate. The new approach is based on the Multidimensional positive definite advection transport algorithm (MPDATA) (Smolarkiewicz 1983; Smolarkiewicz and Margolin 1998; Smolarkiewicz 2006).
  • Larvae can die. You can specify a mortality rate. Different rates can be tested quickly without rerunning the entire hydrodynamic algorithm.
  • The connectivity network can be represented in two ways. Depending on your research question, you may want to characterize connectivity according to the absolute quantity of larvae transmitted from one site to another, or to the probability that a larva released from the first site will settle on the second.

The new tools use a four-step workflow:

  1. Create a simulation using three rasters that define the study area and habitat patches.
  2. Load ocean currents into the simulation for dates of interest. You may choose from several popular sources of currents data.
  3. Run the dispersal algorithm for the patches and the settlement parameters you desire.
  4. Visualize the results as a series of rasters showing larvae density through time and a line feature class showing connections between patches. If desired, you apply mortality at this step.

Here’s the toolbox:

Here’s an example model:

Example analysis

For this example, we’ll examine connectivity of coral reefs within the central and western Gulf of Mexico. I chose this region because it is relatively small, allowing my example simulation to run quickly, and because I had data readily available from a recent paper, Schill et al. (2015). Although this covers a specific dataset and region, I’ll offer hints for how you can best configure the tools for your own data and region. (But please, do not contact me asking for step-by-step instructions on how to do basic GIS tasks, such as how produce a water mask from publicly available GIS data. If you do not already have the GIS skills to do these kinds of things yourself, you are not ready to use the connectivity tools.)

Step 1: Create the simulation

The first step is to create the simulation. In order to do that, we need three rasters: a water mask raster, a patch IDs raster, and a patch cover raster. The rasters must all have the same coordinate system, cell size, extent, and number of rows and columns. Before discussing each raster in detail, I’ll discuss their coordinate system, cell size, and extent. You should select these parameters very carefully; they strongly influence on the results, the length of time required to run the simulation, and the likelihood that the simulation will fail due to insufficient memory.

Coordinate system

The rasters should use a projected coordinate system such as Mercator with meters as the linear unit. The hydrodynamic algorithm performs calculations using Cartesian coordinates with meters as the unit. The coordinate system should, as much as possible, be configured such that its rows and columns run parallel to lines of longitude and latitude. When MGET loads ocean currents data into the simulation, it reprojects the original data into the coordinate system of your rasters. The original data come as vector components–pairs of u and v images giving current speed in the north/south and east/west directions. When MGET reprojects them, it does not know how to adjust the results to account for the fact that north/south/east/west may no longer be up/down/right/left on portions of your map. Projections in which north/south/east/west deviate strongly from up/down/right/left will not have accurate results. This can problem is easy to avoid for study areas near the equator but is increasingly difficult as latitude increases.

If you do not know what to choose, I recommend ArcGIS’s “WGS 1984 Mercator” projection. (I do not recommend any of the “Web Mercator” projections, however, due to the difficulty in properly reprojecting ocean currents data to these projections.) Feel free to contact us for advice.

Cell size, extent, and number of rows and columns

Choosing a cell size is difficult. Often you are working with coral reef data at resolutions of 1 km or higher. High resolution maps are nice, so you should just use the cell size of your reef data for the connectivity analysis, right? There are three reasons why this is probably not a good idea:

  1. Most ocean currents data are much coarser resolution. Most of the global currents datasets are derived from remote sensing observations reported by satellite altimeters which have along-track resolutions on the order of 10 km. The resulting gridded products typically range in resolution from 10-25 km at the equator. If you use a very fine scale such as 1 km, MGET will interpolate these products at that resolution but that does not mean the results will be accurate at that scale. Indeed, it is not possible to know whether or not the results are accurate because the ocean currents datasets are not able to resolve phenomena at that scale.
  2. Simulation run time increases dramatically as cell size decreases. Decreasing the cell size increases the number of cells in the study area; halving the cell size quadruples the number of cells. When you reduce cell size, you must also reduce the time step of the simulation so that the hydrodynamic algorithm remains numerically stable. This means that more time steps are needed to span a given simulation length. The increased number of cells and time steps can greatly lengthen the time it takes to complete the simulation.
  3. The tool may run out of memory. At present, the tool is restricted to running as a 32-bit process, which means that in practice it can access about 2 GB of memory before it fails, regardless of how much memory you have on your computer. We aim to remove this limitation in a future release, but until then, you must be careful about the number of rows and columns of your rasters, and the number of time steps in the simulation.

I recommend that you:

  • First research ocean currents datasets and select one. As you will see in the next bullet, I recommend that you limit the resolution of your analysis to that of the ocean currents data. To follow this advice, you need to select an ocean currents dataset that matches your region and time period of interest. I discuss this further in the Step 2 section below.
  • Choose a cell size that is not smaller than half the resolution of your ocean currents. For example, if you’re using AVISO 0.25° currents in a tropical area, their resolution is about 28 km at the equator, so I’d recommend not going smaller than about 14 km, or perhaps 10 km if you are working somewhat north or south of the equator. Working at a finer scale than that does not seem likely to produce results that will be plausible at that finer scale. (I have not tested this assertion, however.)
  • Keep your rasters to less than 200,000 cells. For example, 500 columns x 400 rows = 200,000 cells. If fewer would work, by all means make your rasters smaller! The fewer cells you have, the faster your simulation will run. Simulations with 200,000 cells and a few hundred patches often max out available memory and run the risk of failing.
  • Do not clip your rasters tightly around habitat patches. Leave a buffer between habitat patches and the edges of rasters, to allow currents to circulate in this area and perhaps return larvae to the spawning patch. Once larvae move beyond the edge of the raster, they are lost and cannot return.

Finally, if you are trying to model fine scale processes around small extents–e.g. nearshore movements of larvae around a small island or atoll–this may not be the tool for you. The tool is intended for use at regional scales where dominant mesoscale circulation features connect patches over 10s to 100s of km.

The Gulf of Mexico example

The Gulf of Mexico example uses data from Schill et al. (2015). In that analysis, we were interested in coral reef connectivity throughout the entire Caribbean, Gulf of Mexico, southeastern U.S., and Bermuda. We used currents data from NOAA’s Atlantic Real-Time Ocean Forecast System (RTOFS), a basin-scale ocean forecast system based on the HYbrid Coordinate Ocean Model (HYCOM). Atlantic RTOFS used a variably-spaced grid that ranged from about 4 km resolution in the western Gulf of Mexico to about 17 km near Africa. We resampled the RTOFS to an 8 km cell size, the coarsest resolution in our study area (the eastern Caribbean). We used the WGS 1984 Mercator projection. The rasters were 594 columns by 413 rows.

For the example here, I clipped the Schill et al. (2015) data to the central and western Gulf of Mexico (see below). I maintained the same coordinate system, but clipped the rasters to 180 columns by 198 rows. I focused on the smaller region to limit the run time of the tool. At this extent, the simulation takes about 25 minutes to run on my circa-2015 laptop, vs. about 20 hours for the full Schill et al. (2015) extent.

The variably-spaced Atlantic RTOFS data we used in Schill et al. (2015) could not be represented as rasters in ArcGIS, which requires constant cell spacing. To work around this, we developed a custom MATLAB script for resampling it into the Mercator projection. We have not had time to redevelop this script for use in MGET, so the Gulf of Mexico example presented here does not use Atlantic RTOFS. Instead I used the HYCOM Global GLBa0.08 dataset, which has a resolution of about 9 km and uses a Mercator projection. These characteristics make it quite suitable for the 8 km rasters we developed for the Schill et al. (2015) paper. Because the Gulf of Mexico is within the extent of the HYCOM Gulf of Mexico GOMl0.04 dataset, it would have worked as well. It offers a 4.5 km resolution.

You can download the Gulf of Mexico example data here.

Now I will discuss the details of the three rasters needed to create the simulation.

Water mask raster

The water mask indicates which cells are land and which are water. It must have an integer data type. The value 0 or No Data indicates land, all other values indicate water. During the simulation, larvae are allowed to move between water cells but cannot enter land cells. Larvae that are moved in the direction of land are “blocked” and remain in the adjacent water cell. Larvae that are moved beyond the extent of the raster from water cells on the edge are lost.

You can produce water masks from bathymetry datasets, which are usually given in raster form. SRTM30_PLUSETOPO, and GEBCO are widely used global bathymetries. Depending on your study area, you may also be able to find a regional bathymetry. Assuming you followed our advice about selecting a cell size that is not too small relative to your ocean currents data, it is very likely that the bathymetry has a smaller cell size than you want to use. You should project your bathymetry to your selected coordinate system at high resolution, clip it, use the ArcGIS Spatial Analyst to flag cells as water or land (e.g. with the Con tool or Raster Calculator), and then use the Resample tool to increase the cell size to your desired coarseness. I do not recommend using the Project Raster tool to increase the cell size; I have observed it introducing spatial error in the results. Check your results carefully.

You can also build water masks from shoreline databases, such as GSHHG, which are often distributed as land polygons. Reproject the polygons to the desired coordinate system and clip them. (It might be faster to first clip them to a region larger than your study area, then reproject them.) Then convert them to rasters at the desired cell size. You’ll probably have data for land and No Data for water. Use ArcGIS Spatial Analyst tools (e.g. Is Null, Raster calculator) to convert them to have 1 for water and 0 or No Data for land.

Here’s the water mask for our Gulf of Mexico example:

Patch IDs raster

This raster specifies the locations and IDs of habitat patches from which larvae will be released and upon which larvae can settle. It must have an integer data type. Each patch is defined as one or more cells having the same integer ID value. Patch IDs may range from 1 to 65535, inclusive. The value 0 may not be used. No Data indicates that the cell is not part of a patch. Typically, each patch’s cells form a single contiguous blob, but this is not required; the cells of a patch may be separated by No Data cells. All patches must occur in cells labelled as water by the water mask raster. If your patches occur close to land, you may need to carefully edit the patch IDs and water mask rasters together to ensure no desired habitat is missed.

Here’s the patch IDs raster for our Gulf of Mexico example. Note how this does not fully follow our recommendation above to buffer patches near the edge of the study area: in the southeast, the fringing reefs along the Yucatán penninsula extend all the way to the bottom edge of raster. The real reason for this is laziness; I clipped the Caribbean-wide data from Schill et al. (2015)and did not bother to edit out the southeasternmost reefs. But I can also offer some reasonable justifications. In this example, I’m not very interested in self recruitment and connectivity between those southeastern reefs. Also, the dominant current patterns flow from south to north here, so there is reduced risk that larvae will be carried off the southern edge of the study area.

How should patches be defined?

These fringing reefs also prompt the questions: how big should patches be? Should long runs of continuous habitat cells be grouped into a single patch or split into multiple patches? If they are split into multiple patches, how should it be done? And would it be better to have each cell of the raster be its own patch?

The answers to these questions depend on the question you’re seeking to answer, and also on a trade-off between level of detail and speed of execution. Adjacent areas of suitable habitat are usually highly connected. There is usually no benefit to treating each cell as a distinct patch. This usually results in a very large number of patches, greatly increasing execution time. Also, the connectivity network that results is usually very dense and must be further summarized to clearly communicate the results.

On the other hand, it may not be sufficiently informative to create a single patch for all the cells of a reef that extends for hundreds of kilometers, especially when it spans multiple political jurisdictions or management zones and the purpose of your study is to investigate connectivity in the context of human uses of the ocean. In this situation, it may be best to break up the reef into multiple patches at political or management boundaries. It is also appropriate to split patches up at locations where physiography or oceanography might strongly affect the flow of larvae. For example, if a reef extends around both sides of a peninsula, it might be appropriate to split the reef into two patches–one for either side of the peninsula–or three–one for either side and one for the tip.

There are no hard-and-fast rules for grouping cells into patches. I recommend you take the approach that seems most appropriate for your situation and document it accordingly. That said, I prefer to to have no more than “a few hundred” patches in a large analysis, or “a few dozen” in a small analysis, as is presented here. Once you exceed a few hundred patches, the simulation time stretches into days for little apparent benefit. When the number of patches is limited to a few dozen, the number of connections is often in the low hundreds, which is not too difficult to visualize on a map.

I followed your advice and selected a coarse cell size commensurate with the ocean currents I’m using. But now some cells only have a little suitable habitat and some have a lot. How should I handle this?

Elaborating on this question: When a cell has only a tiny amount of reef, it seems wrong to mark the cell as being part of a patch. That makes the patch extend over a much larger area than occurs in reality. But if I don’t mark the cell as being part of patch, that reef will be lost. How do I resolve this dilemma?

Mark the cell as being part of a patch, then use the patch cover raster to specify how much of the cell is covered by suitable habitat. See below for details.

Where can I get coral reef data for my own analysis?

UNEP-WCMC Global Distribution of Coral Reefs is a good place to start.

Patch cover raster

The patch cover raster specifies the proportion of each cell’s area that is occupied by habitat from which larvae can be released or upon which larvae can settle. It must have a floating point data type. The raster values must be greater than or equal to 0 and less than or equal to 1. The value 1 indicates that the entire cell is occupied by suitable habitat, while 0.5 indicates that only half of it is. For example, if the cell size is 8 km, the values 1 and 0.5 mean the cell contains 64 and 32 square km of suitable habitat, respectively.

At the start of the simulation, cells are allocated quantities of larvae according to the patch cover raster. A cell with a patch cover of 1 receives 1 unit of larvae; a cell with a patch cover of 0.2 receives 0.2 units of larvae. The simulator assumes that both suitable habitat and larvae are distributed uniformly across the cell at all times. As the simulation progresses, when larvae that are competent to settle drift over a cell, by default only the fraction of the cell that is occupied by suitable habitat receives settlers. (This behavior can be modified by the Use Sensory Zone parameter, described further below.)

Use the patch cover raster to account for the loss of resolution you experienced rescaling your high resolution reef data to the lower resolution ocean currents data–e.g. that some of the low resolution cells are completely covered by habitat, while others are only slightly covered. You can use the ArcGIS Spatial Analyst Block Statistics tool to compute how many high resolution cells occupy the lower resolution cells and obtain a proportion ranging from 0 to 1. This will work both for high resolution presence/absence data (classified as 0 or 1) or high resolution percent cover data (ranging from 0 to 100). In the latter case, if values range from 0 to 100, you may have to divide by 100 to rescale them to 0 to 1.

Here is the patch cover raster for the Gulf of Mexico example:

Note how most of the raster is the value 0. For 0 or No Data, the tool assumes that the cell does not contain any suitable habitat, even if the patch IDs raster indicates that suitable habitat is there. Conversely, if the value is greater than 0 but the corresponding patch IDs raster contains No Data, it is assumed that the cell does not contain any suitable habitat.

Running the tool

Once you have the rasters created, running the Create Larval Dispersal Simulation From ArcGIS Rasters tool is simple:

(If you wish to try this yourself using the Gulf of Mexico example data, download it here.)

You must specify a Simulation Directory that the tool will create, as well as your three rasters. The tool will create the directory, initialize it with some private files and directories, and make copies of your three rasters. Do not manually tamper with the contents of the simulation directory. It is not intended to be read or modified directly.

If you do not see the documentation on the right, click the Show Help >> button and it will appear. Show Help >> will then change to << Hide Help, as you see above.

Step 2: Load ocean currents into the simulation

After creating the simulation, you must load ocean currents data into the Simulation Directory. These will be used in Step 3 to run the simulation. But before you load currents, you must determine which ocean currents product you will use.

Selecting an ocean currents product

At the time of this writing, MGET included support for five ocean currents products for larval dispersal simulations. (At the time of this writing, it was not possible to use products other than these, but see below for further discussion).

ProductSpatial extentTime rangeCell sizeTime stepDepth range
AVISO DUACS 2014Global1993-now1/4° (~28 km at equator)1 daySurface only
Mediterranean Sea1993-now1/8° (~11-14 km in Med)1 daySurface only
HYCOM GLBa0.08Global, 66°S-60°NSept 2008-now
9 km1 day0-5500m
HYCOM GOMl0.0476-98°W, 18-32°N2003-now4.5 km1 day0-5500m
OSCARGlobal, 80°S-80°NOct 1992-now1/3° (~37 km at equator)5 daysSurface only (15m)
Pacific ROMS-CoSiNE100°E-70°W, 45°S-65°N1991-201513.9 km73 hoursSurface to seafloor

First, you should eliminate the products that do not match the spatial extents and time ranges of interest to you. Next, consider the cell size and time step. Also read up on each product and see how it works. After building an understanding, select the product that best meets your needs, in terms of resolution and any other characteristics important to you.

Note that for products that support multiple depth ranges, MGET does allow you to pick a depth of interest, but it does not presently implement vertical migration as a larval behavior. MGET assumes that larvae remain at a constant depth throughout the simulation. For experiments in which larvae remain near the surface, this assumption may be reasonable. For larvae that inhabit sub-surface layers, it may not be reasonable. If not, this tool may not be useful for your research question.

For the Gulf of Mexico example, the best product might be HYCOM GOMl0.04, an 4.5 km resolution ocean model specifically designed for the Gulf of Mexico. I definitely would have chosen that had the reef rasters been of comparable resolution. But I already had reef rasters readily available at 8 km resolution and did not want to undertake the effort of producing new ones at a higher resolution just for this example. Plus, had I done so, it would greatly increase the run time of the tool, probably by a factor of four or more. Finally, it is likely that many more MGET users will be interested in the global HYCOM model (GLBa0.08), and its 9 km cell size is similar to the reef rasters, so I’m demonstrating it instead.

Running the tool

After you select a currents product, run the “Load” tool for that product. The procedure and tool parameters are similar for all of the products. For the Gulf of Mexico example, the tool was Load HYCOM GLBa0.08 Currents Into Larval Dispersal Simulation:

The purpose of this tool is to download currents data for a specified range of dates and add them to the Simulation Directory, thereby making it possible to run simulations for dates within that range. The values you provide for Start date and End date do not control when a simulation starts and ends. You’ll decide that during Step 3, below, when you actually run simulations. The load currents tool performs the job of downloading the currents, storing them locally, and making them ready for use by the simulator, so that when it needs them they can be retrieved quickly. The Start date and End date tell the tool the range of dates for which the currents data should be prepared.

You can run this tool multiple times to load different ranges of dates into the same Simulation Directory. For example, if you want to run simulations during the August-October periods of three different years, you could run the tool three times, once for each year, providing 1 August as the Start date and 31 October as the End date. The tool can take a long time to run, so if speed matters it is better to run the tool multiple times for short ranges of dates (e.g. August-October for three different years), rather than once for a single long range (e.g. August of year 1 through October of year 3).

In the Gulf of Mexico example, I wanted to simulate dispersal of larvae for 30 days; this is known as a 30 day pelagic larval duration (PLD). Repeating what was done by Schill et al. (2015), I wanted the larvae to be released on the last quarter moon of September 2011, which fell on 20 September. So I put in 20 September 2011 as the Start date and 20 October 2011 as the End date. Because these dates are just those for loading data, not for running the simulation, I could have put in an earlier start date or later end date and obtained more data while still covering the focal period. For example, if I wanted to simulate August 2011 last quarter moon as well, as was done by Schill et al. (2015), I could have used 21 August as the start date and loaded two months of currents, which I would use to run two consecutive 30-day simulations (in Step 3 below).

I assumed my larvae occupied the surface, so I used 0 for Depth. I used the default resampling technique of CUBIC for projecting the ocean currents to the coral reef raster coordinate system.

I selected Del2a for the Method for estimating missing currents values. This parameter tells the tool how to fill in cells that are marked as water by your water mask but are missing currents data. It is important that you do this; if the cells are left as No Data, then larvae cannot leave the cells by advection, only by diffusion. Then when you run the simulation in Step 3, the tool will report a warning (see Step 4 below for what this looks like). If you select a Method for estimating missing currents, the tool will interpolate values for those missing cells using values from nearby cells that do have data. You should review the documentation of the parameter in ArcGIS. (Thanks to John D’Errico for the MATLAB implementation of the algorithms underlying this parameter.)

In my experience, the results of the various Del2 methods are fairly similar. I recommend Del2a as a default. All of them can take a significant amount of time to execute for large rasters. The Del4 method while more numerically accurate, is much slower and can require significantly more memory, so I tend not to use it. If you receive an OUT OF MEMORY error while loading currents, switch to the Del2c method. If you still receive the error, you’ll probably have to recreate the simulation at a coarser cell size to reduce the number of cells. You are welcome to contact me for advice.

Finally, this parameter is intended to fill in small areas of missing data for which these interpolation algorithms are reasonable. If your currents product always lacks data in a certain area–e.g. a nearshore environment or at shallow depths–you should not blindly assume that this interpolation procedure will produce correct results! Instead, you should try to find another currents product that offers estimates for your areas of interest. Most likely the developer of the currents data, usually oceanographers, will have a better way of estimating currents values than the simple interpolation algorithms offered by this tool.

I left the other parameters at default values except for Cache Directory, which I set to a different folder than the Simulation Directory. The cache directory is optional; it tells MGET to store a private copy of whatever data were downloaded, so that if MGET needs those data again–if you recreate the simulation directory, for example–it can pull the data from there, which is much faster than downloading them again from the server.

Can I load several different products into a single Simulation Directory, e.g. for different time ranges?

No. At the time of this writing, the tools would only allow you to load a single product in a given simulation directory. You may load as many different time ranges as you like for that product. If you need to use a different product, create another Simulation Directory.

Does MGET support the global HYCOM GLBu0.08 datasets?

Short answer: No, but you might be able to do it yourself, and you are welcome to contact us to advocate we add it.

Long answer: The global HYCOM GLBu0.08 datasets span October 1992 to the present day using a 0.08° equirectangular coordinate system (a.k.a. “geographic” projection) spanning 80.48°S-80.48°N. By contrast, the global HYCOM GLBa0.08 datasets span September 2008 to the present day using a complex “tripole grid”; MGET can access a 9 km Mercator-projected portion of this grid spanning 66°S-60°N. HYCOM produces both from the same underlying results, thus they are effectively the same data, just on a different projection.

We only had time to build a tool for loading GLBa0.08 into connectivity simulations. You are welcome to contact us and advocate we add it. Meanwhile you can try to do it yourself. In a different part of the MGET toolbox there is a tool called Create Rasters for HYCOM GLBu0.08 4D Variable that can download GLBu0.08 rasters and store them in a directory. After reverse engineering the format of the Simulation Directory (see next question below), you could run then run the MGET Find ArcGIS Rasters and Project to Template tool to reproject the rasters to the same coordinate system, cell size, and extent as your patch rasters, interpolate cells missing data that are marked as water by your mask, and store the results in the Simulation Directory.

Can I load my own ocean currents data in the Simulation Directory?

As I am writing this, we do not provide a tool for loading your own currents data into the simulation. If this is something that is absolutely critical for your project, please inquire with us and maybe we can collaborate on it.

You may also try to do it yourself by reverse engineering the format that currents are stored in the Simulation Directory. The currents go into a subdirectory named Currents. In it, there are subdirectories u and v for the horizontal and vertical vector components rasters. In each of those, there are subdirectories by year. In the year directories, the currents rasters appear as .img files with the name uYYYYDDDHHMM.img or vYYYYDDDHHMM.img, where YYYY is the four-digit year, DDD is the three digit day of the year (001 to 365, or 366 on leap years), HH is the hour (00 to 23) and MM is the minute (00 to 59). (The second is assumed to be 0.)

The currents rasters must use the same coordinate system, cell size, extent, and number of rows and columns as the three rasters used to initialize the simulation. The MGET tools Project Raster To Template and Find ArcGIS Rasters and Project to Template can help automate this procedure. MGET’s various Load Currents tools use them internally to convert the original currents rasters to the geographic characteristics of your simulation rasters.

The images must use a constant time increment. There must be no gaps in the series of time slices for periods for which you want to run a simulation. For example, if want to conduct a simulation for the month of September 2015 and you have a daily currents product, you must provide images for all 30 days of September 2015. There must not be any missing days.

You must also modify Simulation.ini file at the root of the Simulation Directory to set four variables:

  • currentsloaded – set this to True
  • currentsproduct – set this to some arbitrary string describing your product; it does not matter what it is
  • currentsdatetype – you probably want to set this to Center, indicating that the date/time of the file indicates the center of the time window that the image applies to
  • maxsecondsbetweencurrentsimages – set this to the number of seconds between each image, e.g. 86400 for daily images

Step 3: Run the simulation

After loading currents for a range of dates you want to simulate, you can run the simulation. This step will disperse the larvae using the ocean currents and track where they settle. This step takes a long time to run, ranging from a few minutes for a simulation spanning a few days for a few patches, to hours or even a few days for a 30-day simulation for dozens or hundreds of patches.

The tool has many parameters. To obtain good results, you must choose values carefully. Let’s walk through them in detail.

Main parameters

Here’s how the tool looks with you first open it:

Simulation directory

The directory you created with the Create Larval Dispersal Simulation tool and then loaded with ocean currents.

Results directory

An existing directory to receive the results. You must create it before running the tool. The tool will create a bunch of outputs within it. The outputs will be overwritten if they already exist. The documentation for this parameter describes the outputs in detail. I discuss them more below.

I suggest you make this directory a peer of the simulation directory. Alternatively you can put it inside the simulation directory, but be careful: if you run the Create Larval Dispersal Simulation tool again (e.g. by accidentally rerunning your geoprocessing model) it will delete and recreate the simulation directory and your results will be lost. If you plan to run simulations using multiple parameters–e.g. different start dates, durations, settlement parameters–you should name the directory in a way that lets you remember those values. However, if you forget to do this, the tool creates a text file within the results directory that lists the parameter values for that run.

Start date

The start date for your simulation. If desired, you may also include a time; if you don’t, midnight (00:00:00) will be used. (Given the resolution of the currents data, specifying the time is not likely to be important.)


The number of days to simulate. The first time you run your simulation, I highly recommend you use a short duration such as 2-5 days and limit the simulation to just a few patches (using the Patches that disperse larvae parameter described below). This will let you check whether there are any basic problems, such as the Time Step being too large or too small (see below), or some cells missing ocean currents values. You can also quickly check the results to see if the tool is doing what you thought it would do.

Next, increase the duration to the full amount you’d like to simulate. Usually this is the pelagic larval duration (PLD) value for the species you are modeling. If you are testing multiple PLD values, use the shortest one. Again, do this for just a few patches and check that the output looks reasonable. This will demonstrate that the tool can run for a few patches without failing due to insufficient memory (see below for more about that). It will also give you an idea how long the full simulation takes, per patch, so you can plan when to run the full simulation (e.g. overnight, while you’re away from work).

Finally, when you’re ready for the complete simulation, use the full duration with all of the patches. This will usually take several hours or more.

Time step

Number of hours the simulator should advance its clock after recalculating larval movements and settlement. This is an important parameter that directly affects both the accuracy of the results and how long the tool will take to run. Although we provided a default of 1 hour, this may not be an appropriate value. Depending on your cell size and the maximum speed of your ocean currents, you might need a smaller value for the simulation to be numerically stable. Fortunately it is not difficult to determine an appropriate value, using the following procedure.

First run the tool using default time step of 1 hour. Use a short duration (2-5 days) and just one patch so it runs very quickly. Every time the tool runs it performs a numerical stability check. If you get this message:

Warning: The stability condition is 1.566760, which is greater than 2 ^ -1/2 =
0.707106. The simulation MAY NOT be numerically stable and the output results
MAY NOT be correct. To fix this problem, reduce the simulation time step to
0.037610 days or less.

it indicates that the time step is too long. When the cell size is small or the ocean currents are fast, a shorter time step is needed. Reduce the time step to the recommended value, or less. Note that the warning message reports the time step in daysbut the tool requires you input it hours. We are sorry for the inconvenience. To convert days to hours, multiply by 24.

Later, when the results are visualized, it will be inconvenient if the time step cannot be divided evenly into 24 hours. So don’t just convert the recommended value reported by the warning to hours and plug it into the tool. For example, in the example above, don’t use 0.90264 hours. Use something like 0.5 hours instead, so exactly 48 time steps occur per day.

Now run the tool again and verify that the warning goes away. Instead you should get this message:

The stability condition is 0.391690, which is less than or equal to 2 ^ -1/2 = 0.707106. The simulation
will be numerically stable.

Now run the tool again for the full simulation duration (e.g. 30 days). If you get the warning again, it means that during this period there was a faster current than you encountered during the initial shorter simulation. Reduce the time step further and rerun the full simulation again until the warning goes away.

If you see that the stability condition is very low, e.g. below 0.1, it indicates that the time step is shorter than it needs to be. This may happen for the default time step of 1 hour if you’re using relatively coarse resolution currents or your study area has relatively slow currents. There is no harm in simulating using a short time step. But the length of time the tool requires to run is directly proportional to the time step. If you increase the time step the tool will complete in a shorter time, which can be advantageous.

The amount of memory required to run the simulation does not depend on the time step. If you receive an OUT OF MEMORYerror while running the simulation, increasing the time step will generally not solve the problem (but increasing the Simulation summarization period might; see below).

Whenever you change the time step, after you settle on a final value always adjust the Simulation summarization period as well (see below).

Simulation summarization period

Period, expressed as the number of simulation time steps, at which the simulation results should be “summarized”. This parameter affects two important aspects of the simulation and directly influences the amount of memory required to execute the simulation, so it should be chosen carefully.

The first important aspect this parameter influences concerns the production of visualizations (Step 4) that summarize the results of the simulation. As the simulation runs, each time the summary period elapses the tool records an image of larval density at that point in the simulation, among other things. The first summarization occurs at the moment larvae are released but before any time has elapsed. The subsequent summarizations occur after the specified number of time steps elapse. For example, if the time step is 0.5 hours and the summarization period is 24, a summarization will occur every 12 hours. Using these records, the tool in Step 4 produces a time series of larval density rasters–one raster each time a summary occurs. The date and time of the summarization are stamped into the raster’s name. It is convenient, therefore, to choose a time step and summarization period that produces rasters at human-friendly summarization times, such as once per day, once per 6 hours, etc. In this respect, your choice of the summarization period is mainly an aesthetic choice: do you want many, frequent larval density rasters, or just a few, infrequent rasters?

The second important aspect this parameter influences concerns larval mortality, an optional process that you apply in Step 4 below. The summarization period determines the frequency at which mortality will be applied during that step.

Settlement parameters


Additional parameters


Common warning and error messages

The ocean currents images are missing data
Warning: The ocean currents images are missing data for some cells flagged as water by your water mask. This will affect the accuracy of the simulation. The simulator will assume the ocean currents have a velocity of zero in these cells. Larvae that enter these cells can only exit via diffusion. These cells may retain larvae in a manner that is not realistic.


Warning: The ocean currents images are missing data for some cells flagged as habitat patches. This will affect the accuracy of the simulation. The simulator will assume the ocean currents have a velocity of zero in these cells. Larvae can only exit these cells via diffusion. These cells may retain larvae in a a manner that is not realistic. The IDs of the affected patches are: <a list of patch IDs>

Fix this by recreating the simulation and then, when you run the Load Currents tool, use the Method for estimating missing currents parameter to fill in the missing values. See the discussion of that parameter in Step 3 above.

The stability condition is <some value>, which is greater than 2 ^ -1/2
Warning: The stability condition is 1.566760, which is greater than 2 ^ -1/2 =
0.707106. The simulation MAY NOT be numerically stable and the output results
MAY NOT be correct. To fix this problem, reduce the simulation time step to
0.037610 days or less.

Fix this by decreasing the Time step parameter. See above for further discussion.

During simulation of patch 137, a negative density was detected
Warning: During simulation of patch 137, a negative density was detected during
step 5 of the simulation. This indicates a numerical stability problem with the
MPDATA algorithm. You should reduce the simulation time step to a lower value
and try again. If this does not resolve the problem, please contact the MGET
development team for assistance.

This should only happen when the Time step is much too large. Fix this by decreasing the Time step parameter. See above for further discussion.

The start date / end date occurs too far before / after …
ValueError: The start date of the simulation (2010-09-20 00:00:00) occurs too far before the date of the first ocean currents image (2011-09-20 00:00:00) that is loaded in the larval dispersal simulation in directory C:\GOM_Connectivity\Simulation. To fix this problem, either move the start date forward or load some older ocean currents data into the simulation, so that the start date matches up with the currents data.


ValueError: The end date of the simulation (2011-11-19 00:00:00) occurs too far after the date of the last ocean currents image (2011-10-20 00:00:00) that is loaded in the larval dispersal simulation in directory C:\GOM_Connectivity\Simulation. To fix this problem, either move the start date backward, reduce the duration of the simulation, or load some more recent ocean currents data into the simulation, so that the end date matches up with the currents data.

The usual reason for these messages is that you that changed your dates or duration but forgot to load additional ocean currents into the simulation. The messages suggest solutions.

Step 4: Visualize the results



Schill SR, Raber GT, Roberts JJ, Treml EA, Brenner J, Halpin PN (2015) No Reef Is an Island: Integrating Coral Reef Connectivity Data into the Design of Regional-Scale Marine Protected Area Networks. PLoS ONE 10(12): e0144199.

Smolarkiewicz PK (1983) A simple positive definite advection scheme with small implicit diffusion. Monthly Weather Review 111:479–86.

Smolarkiewicz PK (2006) Multidimensional positive definite advection transport algorithm: an overview. International Journal for Numerical Methods in Fluids 50:1123–44.

Smolarkiewicz PK, Margolin LG (1998) MPDATA: a finite difference solver for geophysical flows. Journal of Computational Physics 140:459–80.

Treml E, Halpin P, Urban D, Pratson L (2008) Modeling population connectivity by ocean currents, a graph-theoretic approach for marine conservation. Landscape Ecology 23:19–36.

Treml EA, Roberts J, Chao Y, Halpin P, Possingham HP, Riginos C (2012) Reproductive output and duration of the pelagic larval stage determine seascape-wide connectivity of marine populations. Integrative and Comparative Biology 52(4): 525-537.

If you use MGET in your project, please cite our papers in your publications. Your citations help us continue to provide MGET as free software. Thanks for your support!

If you are unable to download any of the papers below, e.g. because they are blocked by a paywall that you cannot get through, please email and we will send you a copy.

The main MGET paper

Roberts JJ, Best BD, Dunn DC, Treml EA, Halpin PN (2010) Marine Geospatial Ecology Tools: An integrated framework for ecological geoprocessing with ArcGIS, Python, R, MATLAB, and C++. Environmental Modelling & Software 25: 1197-1207. doi: 10.1016/j.envsoft.2010.03.029

Publications describing tools that have been incorporated into MGET

Dunn DC, Boustany AM, Roberts JJ, Brazer E, Sanderson M, Gardner B, Halpin PN (2013) Empirical move-on rules to inform fishing strategies: a New England case study. Fish and Fisheries. doi:10.1111/faf.12019

Dunn DC, Boustany AM, Halpin PN (2011) Spatio-temporal management of fisheries to reduce by-catch and increase fishing selectivity. Fish and Fisheries 12: 110-119. doi: 10.1111/j.1467-2979.2010.00388.x

Dunn DC, Stewart K, Bjorkland RH, Haughton M, Singh-Renton S, Lewison R, Thorne L, Halpin PN (2009) A regional analysis of coastal and domestic fishing effort in the wider Caribbean. Fisheries Research 102: 60-68. doi: 10.1016/j.fishres.2009.10.010

Treml EA, Halpin PN, Urban DL, Pratson LF (2008) Modeling population connectivity by ocean currents, a graph-theoretic approach for marine conservation. Landscape Ecology 23: 19-36. doi: 10.1007/s10980-007-9138-y

Treml EA, Roberts J, Chao Y, Halpin PN, Possingham HP, Riginos C (2012). Reproductive output and duration of the pelagic larval stage determine seascape-wide connectivity of marine populations. Integrative and Comparative Biology: 52: 525-537. doi: 10.1093/icb/ics101

Invoking MGET tools programatically

MGET is, in essence, a library of functions. The functions are implemented in various programming languages, mainly Python, R, C++, and MATLAB, but are exposed uniformly via several widely-used interface technologies. Depending on your favored programming environment, you may invoke a given function:

  • From ArcGIS as a geoprocessing tool
  • From Python as a classmethod of a class
  • From many other languages as a method of a COM Automation class

In ArcGIS, MGET appears as a geoprocessing toolbox. The toolbox contains about 300 tools. The tools may be executed individually, wired together into graphical workflows using the ArcGIS ModelBuilder, executed programmatically from geoprocessing scripts, or executed from the ArcGIS Command Line window.

Accessing the MGET toolbox in the ArcToolbox window

After you have installed MGET (instructions here), you can access it from the ArcToolbox window in ArcMap or ArcCatalog. If the ArcToolbox window is not visible, click the ArcToolbox button to bring it up:

You should see the MGET toolbox listed among the others:

If the toolbox is not there but you know MGET is installed, you simply need to add it to the ArcToolbox window.

The MGET toolbox

The MGET toolbox groups its tools into a hierarchy according to their function.

If you have not installed MGET yet, you can browse the toolbox in the interactive diagram below to get a feel for what is included. Click the  icons to drill into the toolbox. Each  icon represents a tool. Click on it to view its documentation.

MGET ArcGIS Toolbox

The top-level toolsets are:

  • Connectivity Analysis – Tools for modeling connectivity between patches of marine habitat by simulating the hydrodynamic dispersal of larvae. This toolset may be expanded in the future to consider other approaches to modeling connectivity.
  • Conversion – Tools for batch-converting between data formats. These are similar to tools provided by ArcGIS but fill important gaps not addressed by ArcGIS, such as the ability to convert gridded data in HDF or netCDF format to ArcGIS-compatible rasters.
  • Data Management – Miscellaneous tools useful for certain data management tasks. Many of these were written in the early years of ArcGIS 9.x to provide basic batch processing capabilities not present in ArcGIS itself. Now that modern versions of ArcGIS include batch processing, many of these tools may be obsolete. Some remain useful in certain scenarios.
  • Data Products – Tools for acquiring and working with various data products that are popular in the marine spatial ecology community. Use these to quickly download oceanographic products in ArcGIS-compatible formats, obtain values of oceanographic products at points in space and time, identify fronts and eddies in satellite images, and so on. These tools are individually tailored to specific products and provide access to them with a minimum of fuss.
  • Fishery Analysis – Tools designed specifically for analyzing fisheries data. While the rest of MGET includes many tools that may be applied to fisheries data, this toolset contains those that are uniquely applicable it.
  • Oceanographic Analysis – Tools for performing oceanographic analysis on generic input data. At present, there is only one toolset within here, containing tools for identifying fronts in ArcGIS rasters or binary files. Most of MGET’s oceanographic analysis tools actually appear in the Data Products toolset because they are tailored to work with specific products (e.g. a tool that detects fronts in NOAA NODC’s 4km AVHRR Pathfinder SST data).
  • Spatial and Temporal Analysis – General-purpose tools for spatial and temporal analysis.
  • Statistics – Tools that perform statistical analysis or modeling. Some of MGET’s most popular tools appear here, such as those for predictive modeling, often used in modeling and mapping the distribution of species. Many of these tools interface ArcGIS with the R statistics program.

Getting started with geoprocessing in ArcGIS

If you have not worked with geoprocessing tools in ArcGIS before, we strongly suggest you get some basic experience running Arc’s built-in tools and using the ModelBuilder workflow system before trying MGET. To get started, we suggest browsing the materials at ESRI’s Geoprocessing Resource Center.

Once you are able to execute tools and build models with the ModelBuilder, proceed to the cookbook below for examples of how to apply MGET’s tools in common scenarios for which MGET was designed.

A cookbook of common MGET scenarios

We are developing a cookbook showing step-by-step examples for common scenarios but at this time (June 2013) it is not ready. In the mean time, please see our downloadable habitat model example for a step-by-step example of one of the most popular applications of MGET. This example covers a number of the topics we plan to cover in the cookbook, although there are many topics that are not covered. If you have any questions please contact us.

Here’s an outline of what we’re planning to cover in the cookbook:

  • Obtaining data in GIS-compatible formats:
    • Downloading popular products supported by MGET in raster format
    • Converting HDF, netCDF, and other formats to rasters
    • Interpolating (a.k.a. sampling) values of rasters and gridded products
    • Querying OBIS and other DiGIR servers for point observations of species
    • Obtaining climate index values for a table of dated records
  • Analyzing and visualizing oceanographic data:
    • Animating time-series data in ArcMap
    • Creating climatologies
    • Creating line features representing current or wind vectors
    • Finding fronts in SST images
    • Finding eddies in SSH images
  • Building predictive species distribution models:
    • Preparing input data for analysis
    • Exploring the data and detecting possible problems
    • Fitting (a.k.a. training) a predictive model
    • Evaluating the model’s performance
    • Predicting rasters for the response variable
  • Analyzing fisheries data:
    • Detecting temporal periodicity in fishing events
    • Detecting spatiotemporal autocorrelation in fishing events
    • Modeling fishing effort using the Fishing Effort Envelope Tool (FEET)
  • Simulating marine hydrodynamic connectivity:
    • Building habitat rasters and initializing a simulation
    • Downloading ocean currents into the simulation
    • Running the simulation
    • Animating the output density rasters
    • Analyzing the output connectivity network
  • Performing exploratory statistical analysis and accessing R from ArcGIS:
    • Creating scatterplots
    • Creating Cleveland dot plots
    • Creating density histograms
    • Executing arbitrary R scripts from ArcGIS
  • Conducting other spatial and temporal analyses:
    • Mapping species diversity from point observations of species
    • Detecting temporal periodicity in a table of dated records
    • Calculating the moon phase for a table of dated records
    • Creating fishnets (polygon grids) that spatially summarize point data
    • Finding the feature nearest to each point
    • Interpolating values for no data cells of a raster

In the mean time, you can review a few examples on our old website. Please do not hesitate to contact us if you have any questions.

Marine Geospatial Ecology Tools is Free/Open Source software which depends on Microsoft Windows and Python.

If you use MGET in your project, please cite our papers in your publications. Your citations help us continue to provide MGET as free software. Thanks for your support!

MGET 0.8a75, released 8 April 2021

PlatformPythonCompatible WithDownload
Microsoft Windows, 32-bit or 64-bit2.4 x86ArcGIS Desktop 9.2MGET-0.8a75.win32-py2.4.exe
2.5 x86ArcGIS Desktop 9.1, 9.3, 9.3.1MGET-0.8a75.win32-py2.5.exe
2.6 x86ArcGIS Desktop 10.0MGET-0.8a75.win32-py2.6.exe
2.7 x86ArcGIS Desktop 10.1-10.8MGET-0.8a75.win32-py2.7.exe

What about ArcGIS 64-bit Background Geoprocessing, ArcGIS Pro, and Python 3.x?

Currently, MGET is only available for 32-bit Python, which means it will only work with ArcGIS Desktop (the 32-bit ArcMap and ArcCatalog applications). Although it is 32-bit, it will work on both the 32-bit and 64-bit versions of the Windows operating system. It is not currently available for any 64-bit version of Python, any version of Python 3, or operating systems other than Windows.

We anticipate that we will eventually release a version of MGET for 64-bit Python 3.x that will be compatible with ArcGIS Pro. However, the work required for this is nontrivial, and at present we do not have a source of funding to directly support it. Progress is slow and we do not have an ETA at this time. (If you know of funding that would support this, please contact us!) Now that ArcGIS Pro is the future of ArcGIS, we do not anticipate releasing MGET for 64-bit Python 2.7, meaning that MGET will likely not ever work with ArcGIS 64-bit Background Geoprocessing. If you have questions, please feel free to contact us.

Copyright and License

Except where otherwise noted, Marine Geospatial Ecology Tools is Copyright © 2008 by Jason J. Roberts. MGET is free software; you can redistribute it and/or modify it under the terms of the GNU General Public License as published by the Free Software Foundation; either version 2 of the License, or (at your option) any later version. MGET is distributed in the hope that it will be useful, but WITHOUT ANY WARRANTY; without even the implied warranty of MERCHANTABILITY or FITNESS FOR A PARTICULAR PURPOSE. See the GNU General Public License (available in the file LICENSE.txt) for more details.

Installation Requirements

Minimum requirements:

  • Microsoft Windows XP SP2 or a later version of Windows, including Server releases and 64-bit editions
  • 32-bit Python 2.4, 2.5, 2.6, or 2.7
  • Python for Windows Extensions (the Python pywin32 package)

Optional requirements for full functionality:

Installation Instructions

These instructions assume you have installed ArcGIS Desktop and the ArcGIS setup program installed Python (it does so by default). If you are a Python expert and plan to use MGET without ArcGIS, you can ignore the steps relating to ArcGIS. For help with installation, please email

Step 1: Log on to your computer as an administrator

Although you must be logged on as an administrator to install MGET, you do not need to be an administrator to run the tools once they are installed.Installation Instructions

Step 2: Close all ArcGIS applications

Close all instances of ArcCatalog, ArcMap, ArcGlobe, etc.

Step 3: If you have ArcGIS 10.1 and earlier, install the latest ArcGIS service pack (optional)

You can skip this step if you do not have ArcGIS, or if you have ArcGIS 10.2 or later. If you do have ArcGIS 10.1 or earlier, installing the service pack will improve the reliability and performance of the MGET tools that require ArcGIS.

  • Click Start, All Programs, ArcGIS, ArcGIS Administrator (if you have ArcGIS 10.0 and later) or Desktop Administrator (if you have ArcGIS 9.3.1 and earlier).
  • In the pane on the right side, note the service pack number that appears right after the words “ArcGIS Service Pack:”
  • Close the Administrator.
  • Open ESRI’s Patches and Service Packs web page.
  • Find the most recent Service Pack for your version of ArcGIS. If the most recent service pack is newer than the one you have installed (or you don’t have one installed), download and install it.

Step 4: Install the pywin32 Python package.

MGET requires that the pywin32 Python package be installed for your version of Python. Pywin32 is also known as the Python Extensions for Windows. You must install the version of pywin32 that matches the version of Python that you will be using for MGET. Typically this is the version of Python that ArcGIS installed for you.

If you have ArcGIS 10.1 or later, this is Python 2.7. To download pywin32 for Python 2.7:

If you have ArcGIS 10.0 or earlier, you have Python 2.6 or earlier. You must download this from a different location:

  • Scroll down to the table of file names. Download and install the file that contains “win32″ and that matches your version of Python. For example, if you have ArcGIS 10.0 with Python 2.6 and are downloading Build 217, choose pywin32-217.win32-py2.6.exe. (Note: for Arc 10.1 and later, we recommend getting pywin32 from github, as described above.)

Step 5: If you have MGET installed already, uninstall it

  • Start the Windows Control Panel.
  • Bring up the list of installed programs:
    • Windows XP and Server 2003: Click Add or Remove Programs
    • Windows Vista and Server 2008: Switch to Classic View and click Programs and Features
    • Windows 7, Server 2008 R2, and later: View by small icons and click Programs and Features
  • Uninstall the program named “Python X.Y GeoEco-Z” or “Python X.Y Marine Geospatial Ecology Tools Z”, where X.Y is your Python version number and Z is an MGET version number (e.g. 0.7).

Step 6: Install MGET

Install the MGET setup program you downloaded above. The installation program is very simple. Unless you have multiple copies of Python installed on your machine (which is rare) the setup program has no options. You can just click Next until it completes:

Step 7: Install optional software

Many MGET tools will be immediately functional after you install MGET. But some tools rely on other software applications and libraries. To ease the burden of getting started, MGET requires none of these to be on your machine when you install it. All MGET tools check their software dependencies when you invoke them, and report error messages and brief installation instructions if required software is not installed.

If you prefer to get started right away, you can rely on these error messages to prompt you for additional software installations when they are needed. If you prefer not to see these error messages, you can preemptively install all of the additional software now.

  • ArcGIS Spatial Analyst extension – this is required by a number of MGET tools, but often only when you use certain parameters, such as the map algebra expression on the various conversion tools that produce ArcGIS rasters. If your ArcGIS license includes this extension but you did not install it, you can re-run the ArcGIS setup program to add it to your installation. Please see the ArcGIS documentation or consult an ArcGIS expert for more information.
  • R statistics program, version 2.5.0 or later – this is required by MGET tools that perform statistical calculations.
  • MATLAB, version 2007b, or the free MATLAB Component Runtime (MCR) version 7.7 – this is required by MGET tools that perform certain numerical calculations. Either one will work, but you must have the exact version specified here. Newer or older versions will not work. If you do not have MATLAB 2007b already installed, we recommend you download the MATLAB Component Runtime from the link above. The tools affected by this requirement include:
    • The Coral Reef Larval Connectivity tools
    • The Cleanup Options of the tools that execute the Cayula-Cornillon front-detection algorithm
    • The tools that execute the Okubo-Weiss eddy-detection algorithm
  • NOAA CoastWatch Utilities, version 3.2 or later – these are required if you want to use any of the MGET tools that process CoastWatch data. In the CoastWatch Utilities setup, be sure to you enable the Command line tools option.

Step 8: Add MGET to your default ArcToolbox window

The MGET setup program does this automatically for the user that installed MGET. But other users must add the toolbox manually. This is usually necessary on classroom computers and similar machines that are accessed by multiple users.

To manually add the toolbox for your user account:

  • Close all ArcGIS applications (ArcMap, ArcCatalog, ArcGlobe, etc.).
  • Start ArcCatalog.
  • If the ArcToolbox window is not visible, click the ArcToolbox button to bring it up:
  • If you don’t see Marine Geospatial Ecology Tools listed in the ArcToolbox window, right click on ArcToolbox and select Add Toolbox:
  • Navigate to C:\Program Files\GeoEco\ArcGISToolbox and add the toolbox you see there:
  • You should now see MGET in the ArcToolbox window:
  • Close ArcCatalog.

From now on, MGET will appear in the ArcToolbox window of ArcCatalog and all new ArcMap documents (.mxd files).

For existing ArcMap documents, you must add the toolbox manually within ArcMap for that document: Start ArcMap, open the document, and follow steps 4-6 above. This is necessary because each ArcMap document maintains a customized ArcToolbox list. The list is initialized to a copy of ArcCatalog’s list whenever a new map is created, but exists independently from that point forward.

Marine Geospatial Ecology Tools

What is it?

Marine Geospatial Ecology Tools (MGET) is a free, open-source geoprocessing toolbox that can help you solve a wide variety of marine research, conservation, and spatial planning problems. MGET plugs into ArcGIS and can perform tasks such as:

  • Accessing oceanographic data from ArcGIS
  • Identifying ecologically-relevant oceanographic features in remote sensing imagery
  • Building predictive species distribution models
  • Modeling habitat connectivity by simulating hydrodynamic dispersal of larvae
  • Detecting spatiotemporal patterns in fisheries and other time series data

Learn more!

Programming Tutorial

Invoking MGET tools programatically MGET is, in essence, a library of functions. The functions are implemented in various programming languages, mainly Python, R, C++, and MATLAB, but are exposed uniformly via several widely-used interface technologies. Depending on your favored programming environment, you may invoke a given function: From ArcGIS as a geoprocessing tool From Python…

Continue Reading Programming Tutorial

ArcGIS Tutorial

In ArcGIS, MGET appears as a geoprocessing toolbox. The toolbox contains about 300 tools. The tools may be executed individually, wired together into graphical workflows using the ArcGIS ModelBuilder, executed programmatically from geoprocessing scripts, or executed from the ArcGIS Command Line window. Accessing the MGET toolbox in the ArcToolbox window After you have installed MGET…

Continue Reading ArcGIS Tutorial

Predictive Modeling Workflow

In MGET 0.8a42, we introduced a simplified workflow for predictive modeling, shown here for generalized linear models (GLMs). The new workflow is the same for all model types (GLM, GAM, etc.) and consists of three steps: Fit the model to training data in a table. This works the same as before. The model formula specifies…

Continue Reading Predictive Modeling Workflow

In December, following the Society for Marine Mammalogy’s 20th Biennial Conference on Marine Mammals in Otago, New Zealand, we conducted 1-day workshops at the University of Otago and University of Auckland. Thanks to all who attended! A special thanks to the workshop organizers, Judy Rodda and Rochelle Constantine. At the workshops, we presented introductory lectures on MGET,… Read More

At the 2012 Esri International User Conference, Esri honored the Duke Marine Geospatial Ecology Lab (MGEL) with a Special Achievement in GIS Award, in recognition of MGEL’s contributions to marine science and its “outstanding work with GIS technology”. MGEL Director Pat Halpin and members Ben Best and Jason Roberts attended the conference and received the award on behalf of the… Read More

We were recently notified by Dr. James Sheppard, Chair of the Spatial Ecology and Telemetry Working Group (SETWG) of The Wildlife Society (TWS), that the SETWG has recognized the MGET development team with an award for providing “a spatial function, tool or service that has significantly enhanced the field of wildlife conservation and management”. More details of the award… Read More