A decade-long (2010–2020) period with precipitation deficits in central–south Chile (30–41∘ S), the so-called megadrought (MD), has led to streamflow depletions of larger amplitude than expected from precipitation anomalies, indicating an intensification in drought propagation. We analysed the catchment characteristics and runoff mechanisms modulating such intensification by using the CAMELS-CL dataset and simulations from the HBV hydrological model. We compared annual precipitation–runoff (P–R) relationships before and during the MD across 106 basins with varying snow-/rainfall regimes and identified those catchments where drought propagation was intensified. Our results show that catchments' hydrological memory – modulated by snow and gro...
In the Mediterranean Andes region (MA; 30°-37°S), the main rivers are largely fed by melting snowpac...
We present a field-data rich modelling analysis to reconstruct the climatic forcing, glacier respons...
In the Mediterranean Andes region '(MA; 30 degrees-37 degrees S), the main rivers are largely fed by...
A decade-long (2010–2020) period with precipitation deficits in central–south Chile (30–41∘ S), the ...
Central Chile (30-40°S) has experienced a rainfall decline since the early 80s. Such long-term dryin...
During the period 2010–2015, the semi-arid Central Andes in Argentina (CAA) experienced one of the m...
Study region: The natural river basins of Chile. Study focus: Drought effects on terrestrial ecosyst...
Streamflow in south-central Chile (SCC, ~€37-42° S) is vital for agriculture, forestry production, h...
Since 2010 an uninterrupted sequence of dry years, with annual rainfall deficits ranging from 25 to ...
Since 2010, Chile has experienced one of the most severe droughts over the last century, the so-call...
The current Chilean megadrought has led to acute water shortages in central Chile since 2010. Glacie...
Since 2010, Chile has experienced one of the most severe droughts over the last century, the so-call...
During the period 2010-2015, the semi-arid Central Andes in Argentina (CAA) experienced one of the m...
The current Chilean megadrought has led to acute water shortages in central Chile since 2010. Glacie...
Precipitation deficit is traditionally considered as the main driver of drought events, however the ...
In the Mediterranean Andes region (MA; 30°-37°S), the main rivers are largely fed by melting snowpac...
We present a field-data rich modelling analysis to reconstruct the climatic forcing, glacier respons...
In the Mediterranean Andes region '(MA; 30 degrees-37 degrees S), the main rivers are largely fed by...
A decade-long (2010–2020) period with precipitation deficits in central–south Chile (30–41∘ S), the ...
Central Chile (30-40°S) has experienced a rainfall decline since the early 80s. Such long-term dryin...
During the period 2010–2015, the semi-arid Central Andes in Argentina (CAA) experienced one of the m...
Study region: The natural river basins of Chile. Study focus: Drought effects on terrestrial ecosyst...
Streamflow in south-central Chile (SCC, ~€37-42° S) is vital for agriculture, forestry production, h...
Since 2010 an uninterrupted sequence of dry years, with annual rainfall deficits ranging from 25 to ...
Since 2010, Chile has experienced one of the most severe droughts over the last century, the so-call...
The current Chilean megadrought has led to acute water shortages in central Chile since 2010. Glacie...
Since 2010, Chile has experienced one of the most severe droughts over the last century, the so-call...
During the period 2010-2015, the semi-arid Central Andes in Argentina (CAA) experienced one of the m...
The current Chilean megadrought has led to acute water shortages in central Chile since 2010. Glacie...
Precipitation deficit is traditionally considered as the main driver of drought events, however the ...
In the Mediterranean Andes region (MA; 30°-37°S), the main rivers are largely fed by melting snowpac...
We present a field-data rich modelling analysis to reconstruct the climatic forcing, glacier respons...
In the Mediterranean Andes region '(MA; 30 degrees-37 degrees S), the main rivers are largely fed by...