Results 11 to 20 of about 63,897 (256)

An estimate of global glacier volume [PDF]

open access: yesThe Cryosphere, 2012
Abstract. I asses the feasibility of multi-variate scaling relationships to estimate glacier volume from glacier inventory data. I calibrate scaling laws against volume observations of optimized towards the purpose of estimating the total global ice volume. This is applied individually to each record in the Randolph Glacier Inventory which is the first
openaire   +3 more sources

The physical basis of glacier volume‐area scaling [PDF]

open access: yesJournal of Geophysical Research: Solid Earth, 1997
Ice volumes are known for only a few of the roughly 160,000 glaciers worldwide but are important components of many climate and sea level studies which require water flux estimates. A scaling analysis of the mass and momentum conservation equations shows that glacier volumes can be related by a power law to more easily observed glacier surface areas ...
David B. Bahr   +2 more
openaire   +1 more source

Melt regimes, internal stratigraphy, and flow dynamics of three glaciers in the Alaska Range [PDF]

open access: yes, 2012
We used ground-penetrating radar (GPR), GPS and glaciochemistry to evaluate melt regimes and ice depths, important variables for mass-balance and ice-volume studies, of Upper Yentna Glacier, Upper Kahiltna Glacier and the Mount Hunter ice divide, Alaska.
Arcone, Steven   +7 more
core   +2 more sources

Volume-area scaling for debris-covered glaciers [PDF]

open access: yesJournal of Glaciology, 2020
AbstractA volume-area scaling relation is commonly used to estimate glacier volume or its future changes on a global scale. The presence of an insulating supraglacial debris cover alters the mass-balance profile of a glacier, potentially modifying the scaling relation.
openaire   +2 more sources

Glacier volume estimation as an ill-posed inversion [PDF]

open access: yesJournal of Glaciology, 2014
AbstractEstimating a glacier’s volume by inferring properties at depth (e.g. bed topography or basal slip) from properties observed at the surface (e.g. area and slope) creates a calculation instability that grows exponentially with the size of the glacier.
David B. Bahr   +2 more
openaire   +1 more source

Volume, formation and sedimentation of future glacier lakes in Switzerland [PDF]

open access: yes, 2022
ISSN:2196 ...
Steffen, Tim   +4 more
openaire   +3 more sources

Radioglaciological studies on Hurd Peninsula glaciers, Livingston Island, Antarctica [PDF]

open access: yes, 2009
We present the results of several radio-echo sounding surveys carried out on Johnsons and Hurd Glaciers, Livingston Island, Antarctica, between the 1999/2000 and 2004/05 austral summer campaigns, which included both radar profiling and common-midpoint ...
Ahlstrom, L.P.   +6 more
core   +2 more sources

Volume–area scaling vs flowline modelling in glacier volume projections [PDF]

open access: yesAnnals of Glaciology, 2007
AbstractVolume–area scaling provides a practical alternative to ice-flow modelling to account for glacier size changes when modelling the future evolution of glaciers; however, uncertainties remain as to the validity of this approach under non-steady conditions.
Valentina Radić   +2 more
openaire   +1 more source

Modelling glacier-bed overdeepenings and possible future lakes for the glaciers in the Himalaya—Karakoram region [PDF]

open access: yes, 2016
Surface digital elevation models (DEMs) and slope-related estimates of glacier thickness enable modelling of glacier-bed topographies over large ice-covered areas.
Allen, S.   +5 more
core   +2 more sources

On the estimation of ice volume of alpine glaciers

open access: yesIce and Snow, 2015
Volume (V) − area (S) scaling approach (V = kSp, where V and S are obtained from direct measurements) is widely used for ice storage assessments in glacier-mountain systems. Accuracy of this approach was tested using surface area and volume dataset for 121 glaciers of different morphological type and sizes in Altay Mountains.
Yu. Ya. Macheret   +3 more
openaire   +3 more sources

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