Results 21 to 30 of about 6,390,963 (305)

ANALYSIS OF OVERESTIMATION IN HISTORICAL ICE FLOW VELOCITY MAPS IN WESTERN PACIFIC OCEAN SECTOR, ANTARCTICA [PDF]

open access: yesThe International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, 2022
High accuracy reconstruction of historical ice flow velocity fields is crucial in mass balance research of the Antarctic Ice Sheet by utilizing the input-output approach.
S. Ge   +29 more
doaj   +1 more source

Outlet glacier flow response to surface melt: based on analysis of a high-resolution satellite data set

open access: yesJournal of Glaciology, 2023
The dynamics of the Greenland Ice Sheet are affected by surface meltwater reaching the base of the ice, altering ice contact with the bedrock. Lack of understanding of this evolution hampers the ability to predict the effects of increasing temperatures ...
Signe H. Larsen   +5 more
doaj   +1 more source

Ice velocity and thickness of the world’s glaciers

open access: yesNature Geoscience, 2022
The effect of climate change on water resources and sea-level rise is largely determined by the size of the ice reservoirs around the world and the ice thickness distribution, which remains uncertain.
R. Millan   +3 more
semanticscholar   +1 more source

COMPILING TECHNIQUES FOR EAST ANTARCTIC ICE VELOCITY MAPPING BASED ON HISTORICAL OPTICAL IMAGERY [PDF]

open access: yesThe International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, 2018
Ice flow velocity over long time series in East Antarctica plays a vital role in estimating and predicting the mass balance of Antarctic Ice Sheet and its contribution to global sea level rise.
X. Li   +17 more
doaj   +1 more source

Surface velocity and ice discharge of the ice cap on King George Island, Antarctica [PDF]

open access: yesAnnals of Glaciology, 2013
AbstractGlaciers on King George Island, Antarctica, have shown retreat and surface lowering in recent decades, concurrent with increasing air temperatures. A large portion of the glacier perimeter is ocean-terminating, suggesting possible large mass losses due to calving and submarine melting.
Osmanoğlu, B.   +3 more
openaire   +2 more sources

Dynamics of Dalk Glacier in East Antarctica Derived from Multisource Satellite Observations Since 2000

open access: yesRemote Sensing, 2020
Monitoring variability in outlet glaciers can improve the understanding of feedbacks associated with calving, ocean thermal forcing, and climate change.
Yiming Chen   +6 more
doaj   +1 more source

Spatio-Temporal Distribution of Supra-Glacial Ponds and Ice Cliffs on Verde Glacier, Chile

open access: yesFrontiers in Earth Science, 2021
Known for their important role in locally enhancing surface melt, supraglacial ponds and ice cliffs are common features on debris-covered glaciers. We use high resolution satellite imagery to describe pond-cliff systems and surface velocity on Verde ...
Thomas Loriaux, Lucas Ruiz
doaj   +1 more source

Processing methodology for the ITS_LIVE Sentinel-1 ice velocity product

open access: yesEarth System Science Data, 2021
. The NASA MEaSUREs Inter-mission Time Series of Land Ice Velocity and Elevation (ITS_LIVE) project seeks to accelerate understanding of critical glaciers and ice sheet processes by providing researchers with global, low-latency, comprehensive and state ...
Y. Lei, A. Gardner, P. Agram
semanticscholar   +1 more source

Surface-velocity field of the northern Larsen Ice Shelf, Antarctica [PDF]

open access: yesAnnals of Glaciology, 1994
Three satellite images of the northern Larsen Ice Shelf arc used to derive velocity fields for the periods 1975–86 and 1986 89. Substantial increases in the speed of the ice between these periods are detected to a high degree of confidence. Ice which entered the ice shelf between Fothergill Point and Cape Worsley and ice from Drygalski Glacier has ...
R. A. Bindschadler   +3 more
openaire   +1 more source

Surface undulations of Antarctic ice streams tightly controlled by bedrock topography [PDF]

open access: yesThe Cryosphere, 2013
Full Stokes flow-line models predict that fast-flowing ice streams transmit information about their bedrock topography most efficiently to the surface for basal undulations with length scales between 1 and 20 times the mean ice thickness.
J. De Rydt   +3 more
doaj   +1 more source

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