Document Type
Article
Publication Title
Antarctic Journal of the United States
Publisher
National Science Foundation
Rights and Access Note
This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. In addition, no permission is required from the rights-holder(s) for educational uses. For other uses, you need to obtain permission from the rights-holder(s).
Publication Date
1983
First Page
112
Issue Number
5
Volume Number
18
Abstract/ 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.
Repository Citation
Mayewski, Paul Andrew, "Ice Mass Fluctuations in NorthernVictoria Land" (1983). Earth Science Faculty Scholarship. 215.
https://digitalcommons.library.umaine.edu/ers_facpub/215
Citation/Publisher Attribution
Mayewski, P.A. (1983). Ice mass fluctuations in Northern Victoria Land, Antarctic Journal of the United States, 18(5): 112
Publisher Statement
44 USC 19 § 1911 Free use of Government publications. Depository libraries shall make Government publications available for the free use of the general public.
Version
publisher's version of the published document
Included in
Climate Commons, Geomorphology Commons, Glaciology Commons, Hydrology Commons