Results 51 to 60 of about 43,336 (208)

Tributary Glacier Surges: An Exceptional Concentration at Panmah Glacier, Karakoram Himalaya [PDF]

open access: yes, 2007
Four tributaries of Panmah Glacier have surged in less than a decade, three in quick succession between 2001 and 2005. Since 1985, 13 surges have been recorded in the Karakoram Himalaya, more than in any comparable period since the 1850s.
Hewitt, Kenneth
core   +2 more sources

An imbalancing act: the delayed dynamic response of the Kaskawulsh Glacier to sustained mass loss

open access: yesJournal of Glaciology, 2021
The Kaskawulsh Glacier is an iconic outlet draining the icefields of the St. Elias Mountains in Yukon, Canada. We determine and attempt to interpret its catchment-wide mass budget since 2007. Using SPOT5/6/7 data we estimate a 2007–18 geodetic balance of
Erik M. Young   +3 more
doaj   +1 more source

Revisiting glacier mass-balance sensitivity to surface air temperature using a data-driven regionalization

open access: yesJournal of Glaciology, 2022
This study involves examination of glaciological mass-balance time series, glacier and climatic descriptors, the application of machine learning methods for glaciological clustering, and computation of mass-balance time series based upon the clustering ...
Alfonso Fernández   +1 more
doaj   +1 more source

Reconstruction of Annual Glacier Mass Balance from Remote Sensing-Derived Average Glacier-Wide Albedo

open access: yesRemote Sensing, 2022
Annual mass balance is an important reflection of glacier status that is also very sensitive to climate fluctuations. However, there is no effective and universal albedo-based method for the reconstruction of annual mass balance due to the scarcity of ...
Zhimin Zhang   +7 more
doaj   +1 more source

Mass Balance of “Vesper” Glacier, Washington, U.S.A. [PDF]

open access: yesJournal of Glaciology, 1981
AbstractDuring 1974–75 glaciologic and geologic studies were conducted on a small (0.17 km2) avalanche-nourished glacier in the North Cascade Range of Washington. The approximate equilibrium-line altitude (ELA) for this ice body, informally called “Vesper” glacier, lies at 1475 m, some 300 m below the regional ELA value.
David P. Dethier, Jan E. Frederick
openaire   +1 more source

Glaciological Mass balance of Znosko Glacier, King George Island

open access: yesAnais da Academia Brasileira de Ciências, 2023
The present article objective is to determine the net mass balance of the glacier Znosko for periods 2018-2019 and 2019-2020. It is situated on King George Island which belongs to the groups Shetland of the South, Antarctic Peninsula region. For this objective, during February 2018 a net of 19 stakes (which were controlled once during February 2019 and
WILSON SUAREZ   +5 more
openaire   +5 more sources

What do We Know the Snow Darkening Effect Over Himalayan Glaciers? [PDF]

open access: yes, 2011
The atmospheric absorbing aerosols such as dust, black carbon (BC), organic carbon (OC) are now well known warming factors in the atmosphere. However, when these aerosols deposit onto the snow surface, it causes darkening of snow and thereby absorbing ...
Colarco, P. R.   +8 more
core   +1 more source

Greenland surface mass-balance observations from the ice-sheet ablation area and local glaciers [PDF]

open access: yes, 2016
Glacier surface mass-balance measurements on Greenland started more than a century ago, but no compilation exists of the observations from the ablation area of the ice sheet and local glaciers.
Abermann, Jakob   +33 more
core   +3 more sources

Glacier Mass Balance Based on Two Digital Elevation Models and Ground Observation Records for the Baishui River Glacier No. 1 in Yulong Snow Mountain, Southeastern Qinghai–Tibet Plateau

open access: yesFrontiers in Earth Science, 2022
Glacier mass balance is a key idea in understanding the relationship between glaciers and climate. In this study, Landsat images, Shuttle Radar Topography Mission, and Advance Land Operation Satellite digital elevation models, and ground observation ...
Lihua Chen   +11 more
doaj   +1 more source

Home - About - Disclaimer - Privacy