Dynamic response of glaciers of the Tibetan Plateau to climate change
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1 Christoph Schneider 1/23 Christoph Schneider Yao, Tandong Manfred Buchroithner Tobias Bolch Kang, Shichang Dieter Scherer Yang, Wei Fabien Maussion Eva Huintjes Tobias Sauter Anwesha Bhattacharya Tino Pieczonka Dynamic Response of Glaciers of the Tibetan Plateau to Climate Change
2 Glacier response to climate forcing (in the case of a polythermal glacier) Christoph Schneider 2/23 snow & firn layer cold -based ice warm-based ice permafrost runoff glacier runoff
3 Glacier response to climate forcing (in the case of a polythermal glacier) Christoph Schneider 3/23 snow & firn layer cold -based ice warm-based ice permafrost runoff glacier runoff
4 Why do we look at glaciers on the Tibetan Plateau? _ fresh water storage _ (seasonal) runoff from glaciers _ glaciers as sensitive instruments reflecting climate variability and climate change on different temporal scales: - direct atmospheric forcing of mass balance components (seasonal to annual signal) - indirect, integrative response of glacier volume and geometry (annual to decadal signal) - nonlinear behaviour through tipping points in the glacial system (polythermal glacier!) _ sensitivity analysis of glacier systems allowing for inverse modelling of atmospheric forcing and its variability Christoph Schneider 4/23
5 Study area Zhadang Glacier Nyainqentanglha Range Christoph Schneider 5/23
6 Field work glacier mass balance net work Christoph Schneider 6/23 snow & firn layer mass balance stake network cold -based ice warm-based ice see POSTER: Huintjes et al.: Glaciological field work glacier runoff permafrost runoff
7 Field work glacier mass balance Christoph Schneider 7/23 see POSTER: Huintjes et al.: Glaciological field work
8 Field work glacier hydrology - conductivity & runoff Christoph Schneider 8/23 snow & firn layer cold -based ice warm-based ice see POSTER: Huintjes et al.: Glaciological field work glacier runoff permafrost runoff Runoff
9 Christoph Schneider 9/23 Field work glacier hydrology - conductivity & runoff see POSTER: Huintjes et al.: Glaciological field work
10 Field work terrestrial photogrammetry (glacier remote sensing) Christoph Schneider 10/23 terrestrial time snow & firn layer lapse camera system cold -based ice see POSTER: Huintjes et al.: Glaciological field work warm-based ice glacier runoff permafrost runoff
11 Field work glacier remote sensing Christoph Schneider 11/23 see POSTER: Huintjes et al.: Glaciological field work
12 Glacier remote sensing analysis Christoph Schneider 12/23 see POSTER: Bolch et al.: Glacier inventory. (Bolch et a. 2010, The Cryosphere)
13 Field work energy and mass balance measurement Christoph Schneider 13/23 energy balance snow & firn layer stations cold -based ice see POSTER: Maussion et al.: Atmospheric data retrieval warm-based ice glacier runoff permafrost runoff see POSTER: Huintjes et al.: Glacier field work
14 Field work glacier atmospheric boundary layer Christoph Schneider 14/23 see POSTER: Huintjes et al.: Glacier field work
15 Field work glacier atmospheric boundary layer Christoph Schneider 15/23 see POSTER: Huintjes et al.: Glacier field work
16 Christoph Schneider 16/23 Glacier mass balance modelling - spatially distributed temperature-index-modelling see POSTER: Huintjes et al.: Glacier mass balance
17 Glacier surface energy balance modelling Christoph Schneider 17/23 see POSTER: Huintjes et al.: Glacier mass balance data processing: Wei, Yang
18 Glacier snow cover modelling Christoph Schneider 18/23 see POSTER: Bhattacharya et al.: Snow cover model
19 Glacier snow cover modelling Christoph Schneider 19/23 see POSTER: Bhattacharya et al.: Snow cover model
20 Christoph Schneider 20/23 Meso-scale atmospheric modelling (WRF) see POSTER: Maussion et al.: Atmospheric modelling (WRF)
21 Christoph Schneider 21/23 Meso-scale atmospheric modelling (WRF) see POSTER: Maussion et al.: Atmospheric modelling (WRF)
22 Meso-scale atmospheric modelling (WRF) Christoph Schneider 22/23 see POSTER: Maussion et al.: Atmospheric modelling (WRF)
23 The next steps to go _ integral modelling of glacier mass balance - from atmosphere - to snow & ice - to runoff _ rigorous testing of all components against observations _ long-term model runs: from seasons to decades - calibration/validation against remote sensing observations _ sensitivity analysis: using long-term glacier mass balance variations for an inverse assessment of large-scale atmospheric forcing _ glacier-climate model projections - forcing models with climate projections for the 21 st century _ spatial and temporal pattern of climate forcing and glacier response on the TiP Christoph Schneider 23/23
24 Spatial pattern of lake areas on the TiP Christoph Schneider 24/23 Gottschalk (2010), unpublished master thesis, RWTH Aachen Univ.
25 Spatial pattern of lake areas on the TiP Christoph Schneider 25/23 Gottschalk (2010), unpublished master thesis, RWTH Aachen Univ.
26 The next steps to go _ integral modelling of glacier mass balance - from atmosphere - to snow & ice - to runoff _ rigorous testing of all components against observations _ long-term model runs: from seasons to decades - calibration/validation against remote sensing observations _ sensitivity analysis: using long-term glacier mass balance variations for an inverse assessment of large-scale atmospheric forcing _ glacier-climate model projections - forcing models with climate projections for the 21 st century _ spatial and temporal pattern of climate forcing and glacier response on the TiP _ glacier systems and glacier response to varying influences along a profile across the TiP from Nam Co to Mount Kailash Christoph Schneider 26/23
27 The next steps to go profile across TiP TIPex - WET TIPex DynRG - TiP WET TIPex - WET Christoph Schneider 27/23
28 Christoph Schneider 28/23 Christoph Schneider Yao, Tandong Manfred Buchroithner Tobias Bolch Kang, Shichang Dieter Scherer Yang, Wei Fabien Maussion Eva Huintjes Tobias Sauter Anwesha Bhattacharya Tino Pieczonka Thank you very much for listening "Act without doing; work without effort. Think of the small as large and the few as many. Confront the difficult while it is still easy; accomplish the great task by a series of small acts." Lao-Tzu in Tao Te Ching (The Book of the Way) Dynamic Response of Glaciers of the Tibetan Plateau to Climate Change
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