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cRYOSPHERE iNITIATIVE

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SCIENCE APPLICATIONS

Comprehensive baseline information

Explore cryosphere related science applications.

Snow
Monitoring & Assessment of Snow Cover in the HKH

The snow cover data is presented for 92 sub-basins from the 10 major river basins of the HKH. Users can view basin/sub-basin wise statistics of the snow cover for different elevation zones, slopes and aspects The snow cover maps can be displayed for a particular date or a specified time period using a time-slider tool.

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himap
Glacier Dynamics in Bhutan Himalaya

Glaciers are repositories of information for climate change studies as they are sensitive to changes in temperature, precipitation, and at-surface solar radiation.

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Glacier Dynamics in Nepal Himalaya

Glaciers are repositories of information for climate change studies as they are sensitive to changes in temperature, precipitation, and at-surface solar radiation.

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Status of Glaciers in the HKH Region

The comprehensive baseline information on the glaciers of the entire HKH region have been organised by major basins and sub-basins

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Datasets

Glacier dataset

Various dataset is available as inventory of glacial lakes in the Himalaya. The data is prepared using topographic maps and satellite images.

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Pilot study towards assessing environmental and societal impacts of permafrost thaw in the Hindu Kush Himalayas

In the Hindu Kush Himalayan (HKH) region, many people live near permafrost or in areas potentially affected by changes in permafrost (Figure 1). Permafrost is ground material (rock or soil) at or below 0°C for two or more years. The near-surface layer above it thaws during the warm season and is termed the “active layer”. Permafrost thaw as a consequence of climate change will have societal, economical, and biological impacts in this area.

Permafrost is ground material (rock or soil), frequently mixed with ground ice, at or below 0°C for two or more years. The near-surface layer above it thaws during the warm season and is termed the “active layer”. The existence and characteristics of permafrost depend on the climatic setting, topography, surface cover and subsurface material. Permafrost is not visible at the surface making it challenging to map its occurrence and extent. Hence,a change in it can lead to unexpected impacts.

Permafrost thaw influences a broad range of systems including hydrology, landscape evolution, vegetation, sediments load in rivers, debris flows and rock fall, and water chemistry. As a consequence, it can strongly affect regional livelihoods and economies. Due to the tight coupling of atmosphere and subsurface temperature, widespread permafrost thaw during the coming decades can be regarded as virtually certain in the HKH region.

Permafrost stabilizes rock slopes, moraines and debris covered slopes, by adding cohesion and by preventing the build-up of hydrostatic pressure. Therefore, melting permafrost can have manifold consequences. For example permafrost under high altitude pastures can retain water in the near surface and make it available to vegetation during summer when the top layer of the permafrost thaws. When permafrost disappears, the water can drain freely, and the ground becomes drier and subsequently vegetation changes.

Especially glacial lakes or hydropower dams in the vicinity of mountains with permafrost will see an increase in rockfall hazards, which may lead to outburst floods with grave downstream consequences. In addition, moraines consist of loose sediments of various sizes, which are often held together by permafrost. When permafrost in moraines and debris slopes thaws, the sediments become available for transport, erode easily and are deposited in lower reaches of rivers. This can happen as a slow and steady process, or as a catastrophic event in combination with extreme precipitation, which can form debris flows with high forces possibly destructing downstream infrastructure such as houses, bridges and roads.

To maximize benefit for the HKH region, a two-part pilot study will be conducted to: (a) assess the quality of the modelled permafrost distribution, and (b) consolidate the current state of knowledge based on literature review. Based on this, targeted follow-up studies with priority topics can be planned in key regions.
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Figure 1: Permafrost and glacier in the extended HKH region (based on Gruber, 2012). 

Visit http://www.geo.uzh.ch/microsite/cryodata/pf_global/ to obtain the 1km permafrost map for Google Earth or as a web mapping service.

Geographical Coverage

Whole HKH region, including ICIMOD member countries: Afghanistan, Bangladesh, Bhutan, China, India, Myanmar, Nepal, and Pakistan

Objectives

  • Clarify the state of the art: (a) Literature review of permafrost studies in the HKH region, and (b) Synthesis of permafrost literature from other regions worldwide and interpretation of its relevance to the HKH region.
  • Overview of possible impacts of changes in permafrost on HKH population based on literature review.
  • Simple systematic assessment of permafrost occurrence in the HKH region.
  • Systematic collection of permafrost and temperature data and metadata for future processing.

Strategies and Approaches

Study methods include literature review in collaboration with partners, systematic analysis of freely available remote sensing imagery to assess the modelled permafrost distribution, and collection and documentation of permafrost and air temperature data and its metadata. Based on this and a workshop, recommendations will be developed for future projects.

Current Partners

Contact: Dorothea Stumm,  Senior Glaciologist and Permafrost Project Coordinator

Science Talk

Permafrost

Permafrost is frozen ground that remains at or below 0° Celsius for two or more years. In high-altitude regions, permafrost can underlie much of the landscape. Many people in the Hindu Kush Himalayas live near permafrost or in areas potentially affected by changes in permafrost.

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