This study provides for the-first-time a water availability analysis at drainage and basin-scale in Peru. Using new gridded datasets of precipitation and temperature, along with six global actual evapotranspiration estimations from remote sensing products, the vulnerability of water resources due to climate change is evaluated. This is addressed under a bottom-up approach and probabilistic Budyko framework that enables us to measure the associated uncertainty. First, to select an adequate estimation of long-term actual evapotranspiration, we compared at basin-scale the remote sensing products with long-term actual evapotranspiration inferred from a waterbalance (precipitation minus discharge) and deterministic Budyko (aridity and evaporati...
In this article, we propose an investigation of the modifications of the hydrological response of tw...
Future changes in multidecadal mean water availability, represented as the difference between precip...
Partitioning of precipitation (P) into actual evapotranspiration (ET) and runoff affects a proxy for...
Quantifying the dependence of future water availability on changing climate is critical for water re...
Peruvian Pacific drainage catchments only benefit from 2% of the total national available freshwater...
Located at a complex topographic, climatic, and hydrologic crossroads, southern Peru is a semi-arid ...
The livelihoods of people in the Andes are expected to be affected by climate change due to their de...
The livelihoods of people in the Andes are expected to be affected by climate change due to their de...
Quantification of the surface water offer is crucial for its management. In Peru, the low spatial de...
Study region Santa River basin, Peru. Study focus In the Andes of Peru, climate change and so...
Projections of future water shortages in the world’s glaciated mountain ranges have grown increasing...
Quantification of the surface water offer is crucial for its management. In Peru, the low spatial de...
In a context of water scarcity in Peruvian Pacific catchments as a crucial issue for Peru, added to ...
Understanding vulnerability has become one of the most important themes of research into climate cha...
Estimating water resources is important for adequate water management in the future, but suitable da...
In this article, we propose an investigation of the modifications of the hydrological response of tw...
Future changes in multidecadal mean water availability, represented as the difference between precip...
Partitioning of precipitation (P) into actual evapotranspiration (ET) and runoff affects a proxy for...
Quantifying the dependence of future water availability on changing climate is critical for water re...
Peruvian Pacific drainage catchments only benefit from 2% of the total national available freshwater...
Located at a complex topographic, climatic, and hydrologic crossroads, southern Peru is a semi-arid ...
The livelihoods of people in the Andes are expected to be affected by climate change due to their de...
The livelihoods of people in the Andes are expected to be affected by climate change due to their de...
Quantification of the surface water offer is crucial for its management. In Peru, the low spatial de...
Study region Santa River basin, Peru. Study focus In the Andes of Peru, climate change and so...
Projections of future water shortages in the world’s glaciated mountain ranges have grown increasing...
Quantification of the surface water offer is crucial for its management. In Peru, the low spatial de...
In a context of water scarcity in Peruvian Pacific catchments as a crucial issue for Peru, added to ...
Understanding vulnerability has become one of the most important themes of research into climate cha...
Estimating water resources is important for adequate water management in the future, but suitable da...
In this article, we propose an investigation of the modifications of the hydrological response of tw...
Future changes in multidecadal mean water availability, represented as the difference between precip...
Partitioning of precipitation (P) into actual evapotranspiration (ET) and runoff affects a proxy for...