Articles | Volume 8, issue 2
https://doi.org/10.5194/esd-8-337-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue:
https://doi.org/10.5194/esd-8-337-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Prevailing climatic trends and runoff response from Hindukush–Karakoram–Himalaya, upper Indus Basin
Shabeh Hasson
CORRESPONDING AUTHOR
CEN, Centre for Earth System Research and Sustainability, University of Hamburg, Hamburg, Germany
Department of Space Sciences, Institute of Space Technology, Islamabad, Pakistan
Jürgen Böhner
CEN, Centre for Earth System Research and Sustainability, University of Hamburg, Hamburg, Germany
Valerio Lucarini
Department of Mathematics and Statistics, University of Reading, Reading, UK
Walker Institute for Climate System Research, University of Reading, Reading, UK
CEN, Centre for Earth System Research and Sustainability, University of Hamburg, Hamburg, Germany
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Short summary
A first comprehensive and systematic hydroclimatic trend analysis for the upper Indus Basin suggests warming and drying of spring and rising early melt-season discharge over 1995–2012 period. In contrast, cooling and falling or weakly rising discharge is found within summer monsoon period that coincides well with main glacier melt season. Such seasonally distinct changes, indicating dominance of snow but suppression of glacial melt regime, address hydroclimatic explanation of
Karakoram Anomaly.
A first comprehensive and systematic hydroclimatic trend analysis for the upper Indus Basin...
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