Current and future global distribution of potential biomes under climate change scenarios

Probability and uncertainty maps showing the potential current and future natural vegetation on a global scale under three different climate change scenarios (RCP 2.6, RCP 4.5 and RCP 8.5) predicted using ensemble machine learning. Current (2022 - 2023) conditions are calculated on historical long t...

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Main Authors: Bonannella, Carmelo, Hengl, Tomislav, Leal Parente, Leandro, de Bruin, Sytze
Format: Other/Unknown Material
Language:unknown
Published: OpenGeoHub Foundation 2023
Subjects:
rcp
Online Access:https://research.wur.nl/en/datasets/current-and-future-global-distribution-of-potential-biomes-under-
https://doi.org/10.5281/zenodo.7822868
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spelling ftunivwagenin:oai:library.wur.nl:wurpubs/614917 2024-02-04T09:53:52+01:00 Current and future global distribution of potential biomes under climate change scenarios Bonannella, Carmelo Hengl, Tomislav Leal Parente, Leandro de Bruin, Sytze 2023 text/html https://research.wur.nl/en/datasets/current-and-future-global-distribution-of-potential-biomes-under- https://doi.org/10.5281/zenodo.7822868 unknown OpenGeoHub Foundation https://edepot.wur.nl/631226 https://research.wur.nl/en/datasets/current-and-future-global-distribution-of-potential-biomes-under- doi:10.5281/zenodo.7822868 info:eu-repo/semantics/openAccess Wageningen University & Research biomes climate change scenario ensemble machine learning global rcp info:eu-repo/semantics/other info:eu-repo/semantics/publishedVersion 2023 ftunivwagenin https://doi.org/10.5281/zenodo.7822868 2024-01-10T23:13:20Z Probability and uncertainty maps showing the potential current and future natural vegetation on a global scale under three different climate change scenarios (RCP 2.6, RCP 4.5 and RCP 8.5) predicted using ensemble machine learning. Current (2022 - 2023) conditions are calculated on historical long term averages (1979 - 2013), while future projections cover two different epochs: 2040 - 2060 and 2061 - 2080. Files are named according to the following naming convention, e.g.: biomes_graminoid.and.forb.tundra.rcp85_p_1km_a_20610101_20801231_go_epsg.4326_v20230410 with the following fields: generic theme: biomes, variable name: graminoid.and.forb.tundra.rcp85, variable type, e.g. probability ("p"), hard class ("c"), model deviation ("md") spatial resolution: 1km, depth reference, e.g. below ("b"), above ("a") ground or at surface ("s"), begin time (YYYYMMDD): 20610101, end time: 20801231, bounding box, e.g. global land without Antarctica ("go"), EPSG code: epsg.4326, version code, e.g. creation date: v20230410. We provide probability and hard class layers using a revised classification system of the BIOME 6000 project explained in the work of Hengl et al. (2018). The 20 classes from this classification system have then been aggregated in 6 biome classes following the IUCN Global Ecosystem Typology classification system. For probability layers, the uncertainty (model deviation: md) is calculated as the standard deviation of the predicted values of the base learners of the ensemble model. The higher the standard deviation the more uncertain the model is regarding the right value to assign to the pixel. For hard class layers the uncertainty is calculated using the margin of victory (Calderón-Loor et al., 2021) defined as the difference between the first and the second highest class probability value in a given pixel. High values would be measures of low uncertainty, while low values would indicate a high uncertainty. It is highly recommended to use the md layers to properly interpret the results of the map. Styling ... Other/Unknown Material Antarc* Antarctica Wageningen UR (University & Research Centre): Digital Library Calderón ENVELOPE(-57.967,-57.967,-63.300,-63.300)
institution Open Polar
collection Wageningen UR (University & Research Centre): Digital Library
op_collection_id ftunivwagenin
language unknown
topic biomes
climate change scenario
ensemble machine learning
global
rcp
spellingShingle biomes
climate change scenario
ensemble machine learning
global
rcp
Bonannella, Carmelo
Hengl, Tomislav
Leal Parente, Leandro
de Bruin, Sytze
Current and future global distribution of potential biomes under climate change scenarios
topic_facet biomes
climate change scenario
ensemble machine learning
global
rcp
description Probability and uncertainty maps showing the potential current and future natural vegetation on a global scale under three different climate change scenarios (RCP 2.6, RCP 4.5 and RCP 8.5) predicted using ensemble machine learning. Current (2022 - 2023) conditions are calculated on historical long term averages (1979 - 2013), while future projections cover two different epochs: 2040 - 2060 and 2061 - 2080. Files are named according to the following naming convention, e.g.: biomes_graminoid.and.forb.tundra.rcp85_p_1km_a_20610101_20801231_go_epsg.4326_v20230410 with the following fields: generic theme: biomes, variable name: graminoid.and.forb.tundra.rcp85, variable type, e.g. probability ("p"), hard class ("c"), model deviation ("md") spatial resolution: 1km, depth reference, e.g. below ("b"), above ("a") ground or at surface ("s"), begin time (YYYYMMDD): 20610101, end time: 20801231, bounding box, e.g. global land without Antarctica ("go"), EPSG code: epsg.4326, version code, e.g. creation date: v20230410. We provide probability and hard class layers using a revised classification system of the BIOME 6000 project explained in the work of Hengl et al. (2018). The 20 classes from this classification system have then been aggregated in 6 biome classes following the IUCN Global Ecosystem Typology classification system. For probability layers, the uncertainty (model deviation: md) is calculated as the standard deviation of the predicted values of the base learners of the ensemble model. The higher the standard deviation the more uncertain the model is regarding the right value to assign to the pixel. For hard class layers the uncertainty is calculated using the margin of victory (Calderón-Loor et al., 2021) defined as the difference between the first and the second highest class probability value in a given pixel. High values would be measures of low uncertainty, while low values would indicate a high uncertainty. It is highly recommended to use the md layers to properly interpret the results of the map. Styling ...
format Other/Unknown Material
author Bonannella, Carmelo
Hengl, Tomislav
Leal Parente, Leandro
de Bruin, Sytze
author_facet Bonannella, Carmelo
Hengl, Tomislav
Leal Parente, Leandro
de Bruin, Sytze
author_sort Bonannella, Carmelo
title Current and future global distribution of potential biomes under climate change scenarios
title_short Current and future global distribution of potential biomes under climate change scenarios
title_full Current and future global distribution of potential biomes under climate change scenarios
title_fullStr Current and future global distribution of potential biomes under climate change scenarios
title_full_unstemmed Current and future global distribution of potential biomes under climate change scenarios
title_sort current and future global distribution of potential biomes under climate change scenarios
publisher OpenGeoHub Foundation
publishDate 2023
url https://research.wur.nl/en/datasets/current-and-future-global-distribution-of-potential-biomes-under-
https://doi.org/10.5281/zenodo.7822868
long_lat ENVELOPE(-57.967,-57.967,-63.300,-63.300)
geographic Calderón
geographic_facet Calderón
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation https://edepot.wur.nl/631226
https://research.wur.nl/en/datasets/current-and-future-global-distribution-of-potential-biomes-under-
doi:10.5281/zenodo.7822868
op_rights info:eu-repo/semantics/openAccess
Wageningen University & Research
op_doi https://doi.org/10.5281/zenodo.7822868
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