Results 21 to 30 of about 161,944 (383)
Journal of Glaciology, 2018 Haxilegen Glacier No.51 (43.731°N, 84.391°E; CN5Y741C0051) is located in the Kuytun river basin, Erenharbirga range, eastern Tien Shan. This study presents the annual mass balance of Haxilegen Glacier No.51 for 7 hydrological years and uses a temperature-
HUI ZHANG +4 more
doaj +2 more sources
A Nonlinear Statistical Model for Extracting a Climatic Signal From Glacier Mass Balance Measurements [PDF]
Journal of Geophysical Research: Earth Surface, 2018 Understanding changes in glacier mass balances is essential for investigating climate changes. However, glacier‐wide mass balances determined from geodetic observations do not provide a relevant climatic signal as they depend on the dynamic response of ...
C. Vincent +14 more
semanticscholar +2 more sources
Estimation and Analysis of Glacier Mass Balance in the Southeastern Tibetan Plateau Using TanDEM-X Bi-Static InSAR during 2000–2014 [PDF]
AtmosphereIn recent decades, glaciers in the southeastern Tibetan Plateau (SETP) have been rapidly melting and showing a large scale of glacier mass loss. Due to the lack of large-scale, high-resolution, and high-precision observations, knowledge on the spatial ...
Yafei Sun +4 more
doaj +2 more sources
Mass balances of Yala and Rikha Samba glaciers, Nepal, from 2000 to 2017 [PDF]
Earth System Science Data, 2021 The glacier mass balance is an important variable to describe the climate system and is used for various applications like water resource management or runoff modelling.
D. Stumm +5 more
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Monitoring the annual geodetic mass balance of Bordu and Sary-Tor glaciers using UAV data
Annals of Glaciology, 2023 The geodetic mass balance of a glacier corresponds to glacier-wide volume changes, converted to mass changes using density assumptions. It is typically calculated by differencing multi-temporal digital elevation models.
Lander Van Tricht +5 more
doaj +1 more source
The Cryosphere, 2023 . Spatio-temporal reconstruction of winter glacier mass balance is important for assessing long-term impacts of climate change. However, high-altitude regions significantly lack reliable observations, which is limiting the calibration of glaciological ...
M. Guidicelli +3 more
semanticscholar +1 more source
International Journal of Applied Earth Observations and Geoinformation, 2021 Bistatic SAR interferometry is an essential technique of observing glacier height changes and geodetic mass balance. Eastern Nyainqentanglha distributes the majority parts of monsoonal temperate glaciers and presented the quickest glacier mass loss rate ...
Gang Li +4 more
doaj +1 more source
Geodetic Mass Balance of Haxilegen Glacier No. 51, Eastern Tien Shan, from 1964 to 2018
Remote Sensing, 2022 The eastern Tien Shan hosts substantial mid-latitude glaciers, but in situ glacier mass balance records are extremely sparse. Haxilegen Glacier No.
Chunhai Xu +4 more
doaj +1 more source
Journal of Glaciology, 2022 High Mountain Asia (HMA) glaciers are critical water reserves for montane regions, which are readily influenced by climate change. The glacier mass balance during 2000–2021 over HMA was estimated by comparing the elevations from ICESat-2 and the NASADEM.
Yubin Fan +5 more
semanticscholar +1 more source
Reconstructing the mass balance of Brewster Glacier, New Zealand, using MODIS-derived glacier-wide albedo [PDF]
The Cryosphere, 2016 In New Zealand, direct measurements of mass balance are sparse due to the inaccessibility of glaciers in the Southern Alps and the logistical difficulties associated with maintaining a mass balance record.
P. Sirguey +5 more
doaj +1 more source