Research highlights from permafrost research: Rock glacier mapping in the HKH region with Google Earth

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Research highlights from permafrost research: Rock glacier mapping in the HKH region with Google Earth M.-O. Schmid, P. Baral, S. Gruber, S. Shahi, T. Shrestha, D. Stumm, and P. Wester International Centre for Integrated Mountain Development Kathmandu, Nepal

Permafrost Pilot Study: Literature review Permafrost distribution assessment (rock glaciers) Scoping Meeting (May 2014) è Plan larger project (2015) Gruber, 2012

Hindu Kush Himalaya (HKH) 8 countries More than 4.5 million km 2 More than 50% of the area is above 3500m a.s.l. Contains the largest area of permafrost outside the Arctic Mountain permafrost in the region is poorly understood Lack of ground measured data for model calibration or validation Knowledge Gap

How to solve this knowledge gap? Traditional: Field measurements Modeling Difficult access / huge area Lack of input data Remote sensing for permafrost? à Rock glacier mapping with Google Earth

Aims and Objectives Developing method to assess permafrost distribution based on rock glacier mapping in Google Earth. Present regional patterns in the permafrost distribution and its linkages to mean annual air temperature, precipitation and topography. Create an adequate data substitute for model validation and other applications with regards to the absence of ground measured data in the investigation area.

Methodology Background: Rock glaciers are indicator of local permafrost occurrence Absence of rock glaciers no permafrost Rock glacier distribution has been used to derive permafrost distribution Our method: Rock glacier mapping with satellite images from Google Earth 4000 randomly distributed samples in the HKH region Every sample is mapped twice by two independent researchers

Rock glacier mapping 4000 randomly distributed sample polygons

Rock glacier mapping

Rock glacier mapping

Rock glacier mapping Map and attributing each rock glacier

Rock glacier mapping - Overlapping areas - Lower limit

Rock glacier mapping: results Schmid et al. 2014, TDC

Rock glacier mapping: results 3554 Lowest in Afghanistan 5735 Highest on TP Mean minimum elevation of rock glaciers per sample Schmid et al. 2014, TDC

Preliminary results Comparison to an existing global permafrost model: Gruber (2012) Blue: permafrost in nearly all conditions (cold, deep) Yellow: permafrost only in very favorable conditions (warm, shallow)

Mapped RG in relation to PZI Schmid et al. 2014, TDC

Rock glacier mapping Negative: Subjective? Permafrost Rockglacier Positive: Huge spatial coverage Transparent & reproducible science Very cost efficient Method with limitations, but good potential!

Conclusions Mapping of rock glaciers in Google Earth can be used as scientific research tool Huge variety of rock glaciers in the HKH region Minimum elevation of rock glaciers (and permafrost) varies between 3500 and 5500m a.s.l. Our study is in very good agreement with the latest global permafrost distribution model

Outcomes Scoping Meeting Widespread permafrost occurrence in HKH region Changes in permafrost can impact: Hydrology Vegetation, ecosystems Hazards Livelihoods à complex and interlinked Role of summer monsoon and dry seasons Study sites: mountain areas across various climate regimes Cross-regional learning, collaboration Scientific capacity building

Future plans 2015 Develop long-term strategy March IGS permafrost session and side meeting Plan larger project and secure funding Plan collaboration and build partnerships

Vision for future project Component 1 Assessing and understanding permafrost 2 Impact of permafrost thaw 3 Scientific capacity building Focus Monitoring programme Process studies Distribution Inter-linkages with snow, glaciers, glacial lakes Hydrology Ecosystems Hazards Livelihoods Collaboration of regional institutes with leading institutes/experts in field Courses and scholarships (MSc, PhD, postdoc) 4 Knowledge hub Permafrost database, data sharing Network of regional permafrost experts Conferences, meetings Communication to public

Thank you Ideas and questions? Thank you