Data from: Increasing dependence of lowland populations on mountain water resources

Mountain areas provide disproportionally high runoff in many parts of the world, and here we quantify for the first time their importance for water resources and food production from the viewpoint of the lowland areas downstream. The dataset maps the degree to which lowland areas potentially depend...

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Main Authors: Viviroli, Daniel, Kummu, Matti, Meybeck, Michel, Kallio, Marko, Wada, Yoshihide
Format: Other/Unknown Material
Language:unknown
Published: Zenodo 2020
Subjects:
Online Access:https://doi.org/10.5061/dryad.ns1rn8pnt
id ftzenodo:oai:zenodo.org:3897479
record_format openpolar
spelling ftzenodo:oai:zenodo.org:3897479 2024-09-15T17:41:43+00:00 Data from: Increasing dependence of lowland populations on mountain water resources Viviroli, Daniel Kummu, Matti Meybeck, Michel Kallio, Marko Wada, Yoshihide 2020-06-16 https://doi.org/10.5061/dryad.ns1rn8pnt unknown Zenodo https://doi.org/10.1038/s41893-020-0559-9 https://zenodo.org/communities/dryad https://doi.org/10.5061/dryad.ns1rn8pnt oai:zenodo.org:3897479 info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode water resources Mountain areas lowland areas water towers Projections Anthropocene highland-lowland systems info:eu-repo/semantics/other 2020 ftzenodo https://doi.org/10.5061/dryad.ns1rn8pnt10.1038/s41893-020-0559-9 2024-07-26T16:29:56Z Mountain areas provide disproportionally high runoff in many parts of the world, and here we quantify for the first time their importance for water resources and food production from the viewpoint of the lowland areas downstream. The dataset maps the degree to which lowland areas potentially depend on runoff contributions from mountain areas (39% of land mass) between the 1960s and the 2040s. Water resources index W quantifies the potential dependence of the world's lowland areas on water resources originating in mountain areas upstream. The data cover the timeframe from the 1960s (1961–1970) to the 2040s (2041–2050) in decadal steps. Data for projections from the 2010s onwards are available for three scenario pathways (SSP1-RCP4.5, SSP2-RCP6.0, SSP3-RCP6.0) and show median results from 5 CMIP5 GCMs (GFDL-ESM2M, HadGEM2-ES, IPSL-CM5A-LR, MIROC-ESM-CHEM, NorESM1‑M). The files are GeoTIFF formatted and in a regular raster of 5'×5' (arc minutes in WGS 1984 coordinate system) The values of W can be classified using the following ranges: W ≤ -2 → Essential but vastly insufficient -2 < W < -1 → Essential but insufficient -1 ≤ W < 0 → Essential and sufficient W = 0 → No surplus from mountains 0 < W ≤ 1 → Supportive 1 < W < 2 → Minor W ≥ 2 → Negligible The values of W are rounded to four decimal places and limited to a range of -1110 to 9998. Values falling outside of that range are set to the nearest limit. he following flag values apply to W : -5555 indicates that there is no water balance surplus from the mountain area upstream, but a lowland water balance surplus; -6666 indicates that there is no water balance surplus from the mountain area upstream, and a lowland water balance deficit. Mountain areas and oceans are NODATA, large ice shields are omitted (Greenland: NODATA, Antarctica: not covered in extent). Other/Unknown Material Antarc* Antarctica Greenland Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic water resources
Mountain areas
lowland areas
water towers
Projections
Anthropocene
highland-lowland systems
spellingShingle water resources
Mountain areas
lowland areas
water towers
Projections
Anthropocene
highland-lowland systems
Viviroli, Daniel
Kummu, Matti
Meybeck, Michel
Kallio, Marko
Wada, Yoshihide
Data from: Increasing dependence of lowland populations on mountain water resources
topic_facet water resources
Mountain areas
lowland areas
water towers
Projections
Anthropocene
highland-lowland systems
description Mountain areas provide disproportionally high runoff in many parts of the world, and here we quantify for the first time their importance for water resources and food production from the viewpoint of the lowland areas downstream. The dataset maps the degree to which lowland areas potentially depend on runoff contributions from mountain areas (39% of land mass) between the 1960s and the 2040s. Water resources index W quantifies the potential dependence of the world's lowland areas on water resources originating in mountain areas upstream. The data cover the timeframe from the 1960s (1961–1970) to the 2040s (2041–2050) in decadal steps. Data for projections from the 2010s onwards are available for three scenario pathways (SSP1-RCP4.5, SSP2-RCP6.0, SSP3-RCP6.0) and show median results from 5 CMIP5 GCMs (GFDL-ESM2M, HadGEM2-ES, IPSL-CM5A-LR, MIROC-ESM-CHEM, NorESM1‑M). The files are GeoTIFF formatted and in a regular raster of 5'×5' (arc minutes in WGS 1984 coordinate system) The values of W can be classified using the following ranges: W ≤ -2 → Essential but vastly insufficient -2 < W < -1 → Essential but insufficient -1 ≤ W < 0 → Essential and sufficient W = 0 → No surplus from mountains 0 < W ≤ 1 → Supportive 1 < W < 2 → Minor W ≥ 2 → Negligible The values of W are rounded to four decimal places and limited to a range of -1110 to 9998. Values falling outside of that range are set to the nearest limit. he following flag values apply to W : -5555 indicates that there is no water balance surplus from the mountain area upstream, but a lowland water balance surplus; -6666 indicates that there is no water balance surplus from the mountain area upstream, and a lowland water balance deficit. Mountain areas and oceans are NODATA, large ice shields are omitted (Greenland: NODATA, Antarctica: not covered in extent).
format Other/Unknown Material
author Viviroli, Daniel
Kummu, Matti
Meybeck, Michel
Kallio, Marko
Wada, Yoshihide
author_facet Viviroli, Daniel
Kummu, Matti
Meybeck, Michel
Kallio, Marko
Wada, Yoshihide
author_sort Viviroli, Daniel
title Data from: Increasing dependence of lowland populations on mountain water resources
title_short Data from: Increasing dependence of lowland populations on mountain water resources
title_full Data from: Increasing dependence of lowland populations on mountain water resources
title_fullStr Data from: Increasing dependence of lowland populations on mountain water resources
title_full_unstemmed Data from: Increasing dependence of lowland populations on mountain water resources
title_sort data from: increasing dependence of lowland populations on mountain water resources
publisher Zenodo
publishDate 2020
url https://doi.org/10.5061/dryad.ns1rn8pnt
genre Antarc*
Antarctica
Greenland
genre_facet Antarc*
Antarctica
Greenland
op_relation https://doi.org/10.1038/s41893-020-0559-9
https://zenodo.org/communities/dryad
https://doi.org/10.5061/dryad.ns1rn8pnt
oai:zenodo.org:3897479
op_rights info:eu-repo/semantics/openAccess
Creative Commons Zero v1.0 Universal
https://creativecommons.org/publicdomain/zero/1.0/legalcode
op_doi https://doi.org/10.5061/dryad.ns1rn8pnt10.1038/s41893-020-0559-9
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