Results 51 to 60 of about 6,390,963 (305)

Dynamic Monitoring of Debris-Covered Glacier Surface Velocity and Ice Thickness of Mt.Tomur, Tian Shan, China

open access: yesRemote Sensing, 2022
The Mt.Tomur glaciers, in the Tian Shan mountains of Western China, are usually debris-covered, and due to climate change, glacial hazards are becoming more frequent in this region.
Changbin Bai   +8 more
doaj   +1 more source

Calving rates at tidewater glaciers vary strongly with ocean temperature [PDF]

open access: yes, 2015
TerraSAR-X data were provided by DLR (project OCE1503), and funded by the Conoco Phillips-Lundin Northern Area Program through the CRIOS project (Calving Rates and Impact on Sea level). A.L. and S.B.
Luckman, Adrian   +14 more
core   +1 more source

Continent‐Wide, Interferometric SAR Phase, Mapping of Antarctic Ice Velocity

open access: yesGeophysical Research Letters, 2019
Surface ice velocity is a fundamental characteristic of glaciers and ice sheets that quantifies the transport of ice. Changes in ice dynamics have a major impact on ice sheet mass balance and its contribution to sea level rise.
J. Mouginot, E. Rignot, B. Scheuchl
semanticscholar   +1 more source

Surface velocity and ice thickness of the Müller ice cap, Axel Heiberg Island

open access: yes, 2021
Muller ice cap is situated on Axel Heiberg Island in Arctic Canada. It is characterised by a mountanious region separating the ice cap in the east from the outlet glaciers in the west. Research has taken place on the outlet glaciers of the ice cap since 1959, but only limited research has been conducted on the main ice cap, and no full depth ice cores ...
openaire   +2 more sources

Inverting ice surface elevation and velocity for bed topography and slipperiness beneath Thwaites Glacier [PDF]

open access: yesThe Cryosphere, 2021
There is significant uncertainty over how ice sheets and glaciers will respond to rising global temperatures. Limited knowledge of the topography and rheology of the ice–bed interface is a key cause of this uncertainty as models show that small changes in the bed can have a large influence on predicted rates of ice loss.
Helen Ockenden   +3 more
openaire   +3 more sources

ICE FLOW VELOCITY MAPPING OF EAST ANTARCTICA FROM 1963 TO 1989 [PDF]

open access: yesThe International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, 2019
Long-time serial observation of surface ice flow velocity in Antarctic is a crucial component in estimating the mass balance of Antarctic ice sheet. However, there is a lack of historical continental scale velocity maps of Antarctica before the 1990s ...
Y. Cheng   +19 more
doaj   +1 more source

Measuring temperature of the ice surface during its formation by using infrared instrumentation [PDF]

open access: yes, 2007
A non-destructive remote sensing technique was used to measure the surface temperature of a thin macroscopic water film flowing on a growing asymmetric ice accretion during its formation inside an icing research wind tunnel.
Kollar, László E.   +2 more
core   +1 more source

Constraining subglacial processes from surface velocity observations using surrogate-based Bayesian inference [PDF]

open access: yesJournal of Glaciology, 2020
Basal motion is the primary mechanism for ice flux in Greenland, yet a widely applicable model for predicting it remains elusive. This is due to the difficulty in both observing small-scale bed properties and predicting a time-varying water pressure on ...
D. Brinkerhoff   +2 more
semanticscholar   +1 more source

Slope estimation influences on ice thickness inversion models: a case study for Monte Tronador glaciers, North Patagonian Andes

open access: yesJournal of Glaciology, 2020
Glacier ice thickness is crucial to quantifying water resources in mountain regions, and is an essential input for ice-flow models. Using a surface velocity inversion method, we combine ice thickness measurements with detailed surface elevation and ...
Valentina Zorzut   +5 more
doaj   +1 more source

A Combined Approach for Filtering Ice Surface Velocity Fields Derived from Remote Sensing Methods [PDF]

open access: yesRemote Sensing, 2017
Various glaciological topics require observations of horizontal velocities over vast areas, e.g., detecting acceleration of glaciers, as well as for estimating basal parameters of ice sheets using inverse modelling approaches. The quality of the velocity is of high importance; hence, methods to remove noisy points in remote sensing derived data are ...
Christine Lüttig   +2 more
openaire   +2 more sources

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