TY - JOUR
T1 - Minimizing uncertainties in climate projections and water budget reveals the vulnerability of freshwater to climate change
AU - Adeyeri, Oluwafemi E.
AU - Zhou, Wen
AU - Ndehedehe, Christopher E.
AU - Wang, Xuan
AU - Ishola, Kazeem A.
AU - Laux, Patrick
N1 - © 2023 The Author(s)
PY - 2024/1/19
Y1 - 2024/1/19
N2 - Global water scarcity threatens agriculture, food security, and human sustainability. Hence, understanding changes in terrestrial water storage (WS) is crucial. By utilizing climate models, reanalysis, and satellite data, we demonstrate the effectiveness of the multivariate bias correction technique in facilitating precise WS representation while ensuring robust water budget closure. Historical data indicate seasonal changes, where forested basins exhibit a WS surplus in the December -January -February season, with a reversal in the JuneJuly -August -September season. Non -forested basins display varied patterns influenced by geographical location and land use type. Future projections indicate increased June -July -August -September deficits in most Southern Hemisphere basins under the middle -road (SSP 245) scenario and wetter December -JanuaryFebruary conditions under the regional rivalry (SSP 370) scenario. Weather and climate systems governing WS vary by season and basin, resulting in inconsistent moisture intake into basins. These findings underscore the intricate interplay between moisture transport, land characteristics, and the resulting WS, highlighting the need to understand these complex interactions for effective regional water resource management strategies in changing climates.
AB - Global water scarcity threatens agriculture, food security, and human sustainability. Hence, understanding changes in terrestrial water storage (WS) is crucial. By utilizing climate models, reanalysis, and satellite data, we demonstrate the effectiveness of the multivariate bias correction technique in facilitating precise WS representation while ensuring robust water budget closure. Historical data indicate seasonal changes, where forested basins exhibit a WS surplus in the December -January -February season, with a reversal in the JuneJuly -August -September season. Non -forested basins display varied patterns influenced by geographical location and land use type. Future projections indicate increased June -July -August -September deficits in most Southern Hemisphere basins under the middle -road (SSP 245) scenario and wetter December -JanuaryFebruary conditions under the regional rivalry (SSP 370) scenario. Weather and climate systems governing WS vary by season and basin, resulting in inconsistent moisture intake into basins. These findings underscore the intricate interplay between moisture transport, land characteristics, and the resulting WS, highlighting the need to understand these complex interactions for effective regional water resource management strategies in changing climates.
KW - Bias correction
KW - Storage
KW - Evapotranspiration
KW - Generation
KW - Dependence
KW - Rainfall
KW - Moisture
KW - Africa
UR - https://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=anu_research_portal_plus2&SrcAuth=WosAPI&KeyUT=WOS:001170502200001&DestLinkType=FullRecord&DestApp=WOS_CPL
U2 - 10.1016/j.oneear.2023.12.013
DO - 10.1016/j.oneear.2023.12.013
M3 - Article
SN - 2590-3330
VL - 7
JO - One Earth
JF - One Earth
IS - 1
ER -