Results 11 to 20 of about 302,803 (284)

An Improved Sea‐Ice Velocity Retrieval Algorithm Based on 89 GHz Brightness Temperature Satellite Data in the Fram Strait

open access: yesEarth and Space Science, 2022
Fram Strait is the passageway where most drifting sea ice exits the Arctic Ocean into the North Atlantic, and the sea‐ice velocity (SIV) is the most critical parameter for the variability of the sea ice area flux through Fram Strait.
Q. Shi, J. Su, G. Spreen, Q. Yang
doaj   +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

Seasonal variability in Antarctic ice shelf velocities forced by sea surface height variations [PDF]

open access: yesThe Cryosphere, 2023
Antarctica's ice shelves resist the flow of grounded ice towards the ocean through “buttressing” arising from their contact with ice rises, rumples, and lateral margins.
C. Mosbeux   +5 more
doaj   +1 more source

Physical Mechanism and Parameterization for Correcting Radar Wave Velocity in Yellow River Ice with Air Temperature and Ice Thickness

open access: yesRemote Sensing, 2023
Unfrozen free and non-free water between ice crystals in flat and hummock ice in the Yellow River exists as water films with varying contents based on ice temperature.
Zhijun Li   +5 more
doaj   +1 more source

An analytical model for wind-driven Arctic summer sea ice drift [PDF]

open access: yesThe Cryosphere, 2016
The authors present an analytical model for wind-driven free drift of sea ice that allows for an arbitrary mixture of ice and open water. The model includes an ice–ocean boundary layer with an Ekman spiral, forced by transfers of wind-input ...
H.-S. Park, A. L. Stewart
doaj   +1 more source

The response of a floating ice sheet to an accelerating line load [PDF]

open access: yes, 2003
The two-dimensional response of a thin, floating sheet of ice to a line load that accelerates from rest at $t = 0$ to a uniform velocity V for $t \geq T$ is determined through an integral-transform solution of the linearized equations of motion.
Hay, SI   +6 more
core   +4 more sources

Electronic Measurement of Ice Velocity [PDF]

open access: yesJournal of Glaciology, 1971
AbstractA light-weight solid-state electronic distance meter was used to measure short-term ice velocities during a two-day interval on the Coleman Glacier at Mt Baker, Washington, U.S.A. The velocities fluctuated rapidly from zero or almost zero to a large fraction of a meter per day.
A. E. Harrison, David Lee
openaire   +1 more source

ICE VELOCITY MEASUREMENT IN EAST ANTARCTICA FROM 1960s TO 1980s BASED ON ARGON AND LANDSAT IMAGERY [PDF]

open access: yesThe International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, 2017
Ice flow velocity is a vital parameter for estimating the ice mass balance of glaciers in Antarctica. Especially long time serial observation of the surface velocity is of great significance to assessing the relationship between Antarctic ice materials ...
R. Li   +27 more
doaj   +1 more source

Overestimation and adjustment of Antarctic ice flow velocity fields reconstructed from historical satellite imagery [PDF]

open access: yesThe Cryosphere, 2022
Antarctic ice velocity maps describe the ice flow dynamics of the ice sheet and are one of the primary components used to estimate the Antarctic mass balance and contribution to global sea level changes. In comparison to velocity maps derived from recent
R. Li   +15 more
doaj   +1 more source

Thermal controls on ice stream shear margins

open access: yesJournal of Glaciology, 2021
Ice stream discharge responds to a balance between gravity, basal friction and lateral drag. Appreciable viscous heating occurs in shear margins between ice streams and adjacent slow-moving ice ridges, altering the temperature-dependent viscosity ...
Pierce Hunter   +4 more
doaj   +1 more source

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