Results 21 to 30 of about 20,223 (134)
Diverging Trends in Rain‐On‐Snow Over High Mountain Asia
Rain‐on‐snow (ROS) over snow‐dominated regions such as High Mountain Asia (HMA) modulates snowmelt and runoff and is key contributor in influencing water availability and hazards (e.g., floods and landslides). We studied the trends in ROS in HMA over the
Fadji Z. Maina, Sujay V. Kumar
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Multi-decadal monsoon characteristics and glacier response in High Mountain Asia
Glacier health across High Mountain Asia (HMA) is highly heterogeneous and strongly governed by regional climate, which is variably influenced by monsoon dynamics and the westerlies.
T E Shaw+11 more
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Climate regime of Asian glaciers revealed by GAMDAM glacier inventory [PDF]
Among meteorological elements, precipitation has a large spatial variability and less observation, particularly in high-mountain Asia, although precipitation in mountains is an important parameter for hydrological circulation.
A. Sakai+5 more
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Remote Detection of Surge-Related Glacier Terminus Change across High Mountain Asia
High Mountain Asia (HMA) hosts the largest glacier concentration outside of polar regions. It is also distinct glaciologically as it forms one of two major surge clusters globally, and many glaciers there contradict the globally observed glacier ...
Amelia B. Vale+3 more
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Brief communication: Updated GAMDAM glacier inventory over high-mountain Asia [PDF]
The original Glacier Area Mapping for Discharge from the Asian Mountains (GAMDAM) glacier inventory was the first methodologically consistent dataset for high-mountain Asia.
A. Sakai
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Spatial differences of ice volume across High Mountain Asia
Advanced knowledge of glacier ice volume is vital for water resource assessment. Previous studies have focused on the estimation of ice volume, but the quantitative understanding of the spatial variability of ice volume across High Mountain regions is ...
Rong-Jun Wang+8 more
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Supraglacial debris thickness and supply rate in High-Mountain Asia
Supraglacial debris in High-Mountain Asia is extensively thin and its supply rate from local topography increases with the temperature and slope of debris-supply slopes, according to analyses of remote sensing data from over 4600 glaciers.
Michael McCarthy+5 more
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INVERSING GLACIER ALBEDO IN HIGH MOUNTAIN ASIA BASED ON SENTINEL-3 SATELLITE DATA [PDF]
Surface albedo, defined as the ratio of the upward to downward solar irradiance, is an important climate parameter in the surface energy budget. Among them, glacier albedo is the link between glaciers and the hydration process of climate and cold zones ...
Y. Tian, Y. Tian, Z. Liu, Z. Liu
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Ice Cliff Dynamics of Debris-Covered Trakarding Glacier in the Rolwaling Region, Nepal Himalaya
Ice cliffs can act as “hot spots” for melt on debris-covered glaciers and promote local glacier mass loss. Repeat high-resolution remote-sensing data are therefore required to monitor the role of ice cliff dynamics in glacier mass loss.
Yota Sato+10 more
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Mapping patterns of supraglacial debris thickness and understanding their controls are important for quantifying the energy balance and melt of debris-covered glaciers and building process understanding into predictive models.
Karla Boxall+3 more
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