Siri Jodha Khalsa: Collaborative effort to assess role glaciers & seasonal snow hydrology High Asia

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Glacial Flooding & Disaster Risk Management Knowledge Exchange and Field Training July 11-24, 2013 in Huaraz, Peru HighMountains.org/workshop/peru-2013

Establishing a Collaborative Effort to Assess the Role of Glaciers and Seasonal Snow Cover in the Hydrology of the Mountains of High Asia R. Armstrong, M. Williams, A. Barrett, M. J. Brodzik, F. Fetterer, Siri Jodha S. Khalsa, A. Racoviteanu, A. Rasmussen, B. Raup, A. Wilson, U. Horodyskyj Objectives The Contribution to High Asia Runoff from Ice and Snow (CHARIS) project is systematically assessing the role of glacier ice melt and seasonal snow melt in the freshwater resources of High Asia. This assessment is crucial for accurate forecasting of availability and vulnerability of water resources in this region. In collaboration with Asian partner organizations, we are deriving critical regional-­‐ scale information for planning downstream irrigation, hydropower generation and general consumption. Realistic forecasts of water resources in these regions are not possible until we better understand the current hydrologic regime. Methods We are applying a suite of satellite remote sensing, reanalysis and ground-­‐based data as input to snow and ice melt models. Gridded maps of snow and glacier area/elevation are input to a temperature-­‐index melt model. Runoff from snow-­‐ covered grid cells is the product of cell area and melt depth from the melt model. Glacier melt is estimated similarly, once snow has disappeared from glacierized grid cells. The melt model is driven by daily mean temperature from reanalysis data. Analysis and Validation We are comparing seasonal melt volume time series generated from temperature-­‐ index models with measured river discharge volumes and comparing the regional scale results with local sub-­‐basin studies based on energy balance modeling approaches. We are also evaluating the accuracy of the melt model results using innovative isotopic and geochemical tracers to identify and quantify the sources of water (ice melt, snow melt, rainfall and ground water) flowing into selected rivers representing the major hydro-­‐climates of the study area. With our Asian partners, we are assessing the performance of the various melt models. Results of this study can be applied to future efforts to evaluate the socio-­‐economic impacts of water uses and their vulnerability to changes in flow magnitude and timing. CHARIS People & Partners Project personnel are located principally at the University of Colorado: - Richard Armstrong, Principal Investigator, Senior Research Scientist and Fellow of CIRES. Leads the project with a perspective gained from more than 30 years in snow and ice research, including extensive glacier mass balance studies.


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