The Ocean Level and Models Simulating Its Oscillations

General modes for simulating changes in mean sea level are expressed for different time frames that involve short- and long-term transgressive - regressive periods. Our investigations of variations in the global hydrologic cycle indicate that they are important factors in the long term fluctuations...

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Main Authors: Kliege, R. K., Dobrovolsky, S. G.
Format: Article in Journal/Newspaper
Language:English
Published: Journal of Coastal Research 1988
Subjects:
Online Access:https://journals.flvc.org/jcr/article/view/77738
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spelling ftfloridaojojs:oai:journals.flvc.org:article/77738 2023-05-15T16:40:37+02:00 The Ocean Level and Models Simulating Its Oscillations Kliege, R. K. Dobrovolsky, S. G. 1988-05-01 application/pdf https://journals.flvc.org/jcr/article/view/77738 eng eng Journal of Coastal Research https://journals.flvc.org/jcr/article/view/77738/75189 https://journals.flvc.org/jcr/article/view/77738 Journal of Coastal Research; Vol 4 No 2 (1988): Journal of Coastal Research 0749-0208 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion Peer-reviewed Article 1988 ftfloridaojojs 2020-11-14T19:09:55Z General modes for simulating changes in mean sea level are expressed for different time frames that involve short- and long-term transgressive - regressive periods. Our investigations of variations in the global hydrologic cycle indicate that they are important factors in the long term fluctuations of the world ocean level. It is suggested that anthropogenic factors are contributing to a world-wide increase in temperature that may in turn destabilize the western Anarctica ice sheet. A surge and melting of this vast ice mass might cause a rise in the world ocean level on the order of 5 to 7 meters. Article in Journal/Newspaper Ice Sheet Florida Online Journals (FloridaOJ)
institution Open Polar
collection Florida Online Journals (FloridaOJ)
op_collection_id ftfloridaojojs
language English
description General modes for simulating changes in mean sea level are expressed for different time frames that involve short- and long-term transgressive - regressive periods. Our investigations of variations in the global hydrologic cycle indicate that they are important factors in the long term fluctuations of the world ocean level. It is suggested that anthropogenic factors are contributing to a world-wide increase in temperature that may in turn destabilize the western Anarctica ice sheet. A surge and melting of this vast ice mass might cause a rise in the world ocean level on the order of 5 to 7 meters.
format Article in Journal/Newspaper
author Kliege, R. K.
Dobrovolsky, S. G.
spellingShingle Kliege, R. K.
Dobrovolsky, S. G.
The Ocean Level and Models Simulating Its Oscillations
author_facet Kliege, R. K.
Dobrovolsky, S. G.
author_sort Kliege, R. K.
title The Ocean Level and Models Simulating Its Oscillations
title_short The Ocean Level and Models Simulating Its Oscillations
title_full The Ocean Level and Models Simulating Its Oscillations
title_fullStr The Ocean Level and Models Simulating Its Oscillations
title_full_unstemmed The Ocean Level and Models Simulating Its Oscillations
title_sort ocean level and models simulating its oscillations
publisher Journal of Coastal Research
publishDate 1988
url https://journals.flvc.org/jcr/article/view/77738
genre Ice Sheet
genre_facet Ice Sheet
op_source Journal of Coastal Research; Vol 4 No 2 (1988): Journal of Coastal Research
0749-0208
op_relation https://journals.flvc.org/jcr/article/view/77738/75189
https://journals.flvc.org/jcr/article/view/77738
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