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: Dataset
Language:English
Published: 2023
Subjects:
rcp
Online Access:https://zenodo.org/record/7520814
https://doi.org/10.5281/zenodo.7520814
id ftzenodo:oai:zenodo.org:7520814
record_format openpolar
spelling ftzenodo:oai:zenodo.org:7520814 2023-07-16T03:52:58+02:00 Current and future global distribution of potential biomes under climate change scenarios Bonannella, Carmelo Hengl, Tomislav Leal Parente, Leandro de Bruin, Sytze 2023-01-10 https://zenodo.org/record/7520814 https://doi.org/10.5281/zenodo.7520814 eng eng info:eu-repo/grantAgreement/EC/HE/101059548/ doi:10.5281/zenodo.7520813 https://zenodo.org/communities/oemc-project https://zenodo.org/record/7520814 https://doi.org/10.5281/zenodo.7520814 oai:zenodo.org:7520814 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode ensemble machine learning climate change scenario rcp biomes global info:eu-repo/semantics/other dataset 2023 ftzenodo https://doi.org/10.5281/zenodo.752081410.5281/zenodo.7520813 2023-06-27T23:02:30Z 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_v20230110 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: v20230110. 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 ... Dataset Antarc* Antarctica Zenodo Calderón ENVELOPE(-57.967,-57.967,-63.300,-63.300)
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic ensemble machine learning
climate change scenario
rcp
biomes
global
spellingShingle ensemble machine learning
climate change scenario
rcp
biomes
global
Bonannella, Carmelo
Hengl, Tomislav
Leal Parente, Leandro
de Bruin, Sytze
Current and future global distribution of potential biomes under climate change scenarios
topic_facet ensemble machine learning
climate change scenario
rcp
biomes
global
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_v20230110 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: v20230110. 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 Dataset
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
publishDate 2023
url https://zenodo.org/record/7520814
https://doi.org/10.5281/zenodo.7520814
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 info:eu-repo/grantAgreement/EC/HE/101059548/
doi:10.5281/zenodo.7520813
https://zenodo.org/communities/oemc-project
https://zenodo.org/record/7520814
https://doi.org/10.5281/zenodo.7520814
oai:zenodo.org:7520814
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.752081410.5281/zenodo.7520813
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