Meltwater runoff in the catchment area containing Chhota Shigri glacier (Western Himalaya) is simulated for the period 1951–2099. The applied mass-balance model is forced by downscaled products from four regional climate models with different horizontal resolution. For the future climate scenarios we use high resolution time series of 5 km grid spacing, generated using the newly developed Intermediate Complexity Atmospheric Research Model. The meteorological input is downscaled to 300 m horizontal resolution. The use of an ice flow model provides annually updated glacier area for the mass-balance calculations. The mass-balance model calculates daily snow accumulation, melt, runoff, as well as the individual runoff components (glacial melt, ...
An improved understanding of fresh water stored in the Himalaya is crucial for water resource manage...
River flow from glacierized areas in the Himalaya is influenced both by intra-annual variations in p...
The understanding of the runoff generation processes is reviewed and simulation of daily streamflow ...
Glacier mass balance and runoff are simulated from 1955 to 2014 for the catchment (46% glacier cover...
Glacier-wide mass balances and runoffs are reconstructed over 1969-2016 for Chhota Shigri Glacier ca...
Under different climate change scenarios, the current study was planned to simulate runoff due to sn...
In contrast to widespread glacier retreat evidenced globally, glaciers in the Karakoram region have ...
The analysis of climate change impact on the hydrology of high altitude glacierized catchments in th...
The history of glacier length fluctuations serves as a reliable indicator of the past climate. In th...
ABSTRACT: The Himalayas and glaciers are huge storage and very important source of fresh water. On t...
The heavily debris-covered Inylchek glaciers in the central Tian Shan are the largest glacier system...
The impact of warmer climate on melt and evaporation was studied for tainted, snowfed and glacierfed...
The heavily debris-covered Inylchek glaciers in the central Tian Shan are the largest glacier system...
Glaciers are of key importance to freshwater supplies in the Himalayan region. Their growth or decli...
The heavily debris-covered Inylchek glaciers in the central Tian Shan are the largest glacier system...
An improved understanding of fresh water stored in the Himalaya is crucial for water resource manage...
River flow from glacierized areas in the Himalaya is influenced both by intra-annual variations in p...
The understanding of the runoff generation processes is reviewed and simulation of daily streamflow ...
Glacier mass balance and runoff are simulated from 1955 to 2014 for the catchment (46% glacier cover...
Glacier-wide mass balances and runoffs are reconstructed over 1969-2016 for Chhota Shigri Glacier ca...
Under different climate change scenarios, the current study was planned to simulate runoff due to sn...
In contrast to widespread glacier retreat evidenced globally, glaciers in the Karakoram region have ...
The analysis of climate change impact on the hydrology of high altitude glacierized catchments in th...
The history of glacier length fluctuations serves as a reliable indicator of the past climate. In th...
ABSTRACT: The Himalayas and glaciers are huge storage and very important source of fresh water. On t...
The heavily debris-covered Inylchek glaciers in the central Tian Shan are the largest glacier system...
The impact of warmer climate on melt and evaporation was studied for tainted, snowfed and glacierfed...
The heavily debris-covered Inylchek glaciers in the central Tian Shan are the largest glacier system...
Glaciers are of key importance to freshwater supplies in the Himalayan region. Their growth or decli...
The heavily debris-covered Inylchek glaciers in the central Tian Shan are the largest glacier system...
An improved understanding of fresh water stored in the Himalaya is crucial for water resource manage...
River flow from glacierized areas in the Himalaya is influenced both by intra-annual variations in p...
The understanding of the runoff generation processes is reviewed and simulation of daily streamflow ...