Ice Mass Fluctuations in NorthernVictoria Land

[From the introduction] Rennick Glacier is one of the major ice drainages for the northern Victoria Land sector of East Antarctica. Unlike glaciers farther south along the Transantarctic Mountains, Rennick Glacier does not drain into the Ross Ice Shelf but flows directly into a seasonally ice-covere...

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Bibliographic Details
Main Author: Mayewski, Paul Andrew
Format: Text
Language:unknown
Published: DigitalCommons@UMaine 1983
Subjects:
Glaciogeology
Geochemistry
Glaciology
Cryology
Climate Change
Climate
Earth Sciences
Geomorphology
Hydrology
East Antarctica
Victoria Land
Ross Ice Shelf
Transantarctic Mountains
Rennick
Rennick Glacier
Antarc*
Antarctica
Ice Shelf
Online Access:https://digitalcommons.library.umaine.edu/ers_facpub/215
https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1220&context=ers_facpub
Description
Summary:[From the introduction] Rennick Glacier is one of the major ice drainages for the northern Victoria Land sector of East Antarctica. Unlike glaciers farther south along the Transantarctic Mountains, Rennick Glacier does not drain into the Ross Ice Shelf but flows directly into a seasonally ice-covered ocean. Therefore, current fluctuations of this glacier are unhampered by the dampening effects of the Ross Ice Shelf. The primary controls on the activity of this glacier and others in this region are mass balance and sea level.

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