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Basin / Site Name
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Gyirong, Tibet Plateau, China
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Country; Province/State
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China
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Website
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Operational Management
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Chinese Academy of Sciences - Institute of Tibetan Plateau Research Data Center (TPDC)
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Basin / Site Location (Centroid Coordinates)
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Coordinate Format
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Latitude
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Longitude
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Degrees Minutes Seconds
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Decimal Degrees
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85.3292
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28.3933
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Purpose / Scientific Focus
Primary focus is cryospheric research due to the high density of glacial lakes, permafrost, and steep terrain. It is heavily studied for GLOFs (Glacial Lake Outburst Floods), debris flows, and landslide-dammed lakes.
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Location (Physiographic Region)
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Area (km2)
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Elevation (m; Mean, Maximum, Minimum)
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Description (Physical–Ecological–Climatic Characteristics)
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Drainage / River System
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Gyirong sits on the northern slopes of the Himalayas. Local high-altitude tributaries (such as the Lhende Khola / Lhende River) drain southward through deep gorges, crossing the border into Nepal where they feed into the Bhote Koshi / Trishuli River, and eventually into the major Narayani (Gandaki) River basin flowing into the Ganges.
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Site History or Historical Context
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Years of Data
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Glacierized Area (% and year(s) measured)
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9% - 13% (roughly 11.8% of the basin consists of clean ice, while about 1.7% consists of debris-covered glacier ice)
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Main Land Cover(s)
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Lithology / Soils
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J F M A M J J A S O N D A
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Mean Monthly and Annual Temperature (°C)
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10 to 13 C
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J F M A M J J A S O N D A
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Mean Total Monthly and Annual Precipitation (mm)
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800 mm - 1,200 mm (driven heavily by the summer monsoon)
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Snow Characteristics
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Additional Noteworthy Characteristics of Basin/Site
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Characterized by extreme relief—dropping rapidly from high-altitude Tibetan plateau environments down steep Himalayan gorges. This creates distinct vertical climate zones, heavy monsoon influences funneling up from the south, and significant glaciated terrain.
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