Intrinsic Thermodynamical Time-Scales of the Atmosphere-Ocean-Cryosphere Climate System
Quantitative reconstruction of climatic parameters from both oceanic and continental records shows several time scales of the successive glacial-interglacial episodes that have characterized the Earth's climate about the past million years. For example, after analyzing data from the 2,083 m ice...
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ftdtic:ADA530527 2023-05-15T13:38:25+02:00 Intrinsic Thermodynamical Time-Scales of the Atmosphere-Ocean-Cryosphere Climate System Chu, Peter C. NAVAL POSTGRADUATE SCHOOL MONTEREY CA DEPT OF OCEANOGRAPHY 1993 text/html http://www.dtic.mil/docs/citations/ADA530527 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA530527 en eng http://www.dtic.mil/docs/citations/ADA530527 Approved for public release; distribution is unlimited. DTIC Meteorology Thermodynamics *CLIMATE *THERMODYNAMIC PROPERTIES *EARTH ATMOSPHERE ANTARCTIC REGIONS OCEANS GLACIOLOGY EARTH(PLANET) *CRYOSPHERE CLIMATE SYSTEM Text 1993 ftdtic 2016-02-23T03:53:44Z Quantitative reconstruction of climatic parameters from both oceanic and continental records shows several time scales of the successive glacial-interglacial episodes that have characterized the Earth's climate about the past million years. For example, after analyzing data from the 2,083 m ice core recovered by the Soviet Antarctic Expeditions at Vostok (East Antarctic), Jouzel et al. (1982) found several peaks (25.3, 45.7, and 107.5 kyr) in the variation spectra of the Vostok isotope temperature, and related these peaks to the astronomical forcing, i.e., the obliquity of the Earth's axis (period at 41 kyr) and the precession of the equinox (periods at 23 and 19 kyr). Is the climatic variation purely caused by the external forcing? If so, the climate prediction would be relatively simple because it becomes the forecast of the Earth's orbit tilt and precession. In fact, the climate system is much more complicated. The climatic variation is caused by both external and internal sources. Presented at the Conference on Global Change, American Meteorological Society (4th), 433-438, 1993. Text Antarc* Antarctic ice core Defense Technical Information Center: DTIC Technical Reports database Antarctic |
institution |
Open Polar |
collection |
Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Meteorology Thermodynamics *CLIMATE *THERMODYNAMIC PROPERTIES *EARTH ATMOSPHERE ANTARCTIC REGIONS OCEANS GLACIOLOGY EARTH(PLANET) *CRYOSPHERE CLIMATE SYSTEM |
spellingShingle |
Meteorology Thermodynamics *CLIMATE *THERMODYNAMIC PROPERTIES *EARTH ATMOSPHERE ANTARCTIC REGIONS OCEANS GLACIOLOGY EARTH(PLANET) *CRYOSPHERE CLIMATE SYSTEM Chu, Peter C. Intrinsic Thermodynamical Time-Scales of the Atmosphere-Ocean-Cryosphere Climate System |
topic_facet |
Meteorology Thermodynamics *CLIMATE *THERMODYNAMIC PROPERTIES *EARTH ATMOSPHERE ANTARCTIC REGIONS OCEANS GLACIOLOGY EARTH(PLANET) *CRYOSPHERE CLIMATE SYSTEM |
description |
Quantitative reconstruction of climatic parameters from both oceanic and continental records shows several time scales of the successive glacial-interglacial episodes that have characterized the Earth's climate about the past million years. For example, after analyzing data from the 2,083 m ice core recovered by the Soviet Antarctic Expeditions at Vostok (East Antarctic), Jouzel et al. (1982) found several peaks (25.3, 45.7, and 107.5 kyr) in the variation spectra of the Vostok isotope temperature, and related these peaks to the astronomical forcing, i.e., the obliquity of the Earth's axis (period at 41 kyr) and the precession of the equinox (periods at 23 and 19 kyr). Is the climatic variation purely caused by the external forcing? If so, the climate prediction would be relatively simple because it becomes the forecast of the Earth's orbit tilt and precession. In fact, the climate system is much more complicated. The climatic variation is caused by both external and internal sources. Presented at the Conference on Global Change, American Meteorological Society (4th), 433-438, 1993. |
author2 |
NAVAL POSTGRADUATE SCHOOL MONTEREY CA DEPT OF OCEANOGRAPHY |
format |
Text |
author |
Chu, Peter C. |
author_facet |
Chu, Peter C. |
author_sort |
Chu, Peter C. |
title |
Intrinsic Thermodynamical Time-Scales of the Atmosphere-Ocean-Cryosphere Climate System |
title_short |
Intrinsic Thermodynamical Time-Scales of the Atmosphere-Ocean-Cryosphere Climate System |
title_full |
Intrinsic Thermodynamical Time-Scales of the Atmosphere-Ocean-Cryosphere Climate System |
title_fullStr |
Intrinsic Thermodynamical Time-Scales of the Atmosphere-Ocean-Cryosphere Climate System |
title_full_unstemmed |
Intrinsic Thermodynamical Time-Scales of the Atmosphere-Ocean-Cryosphere Climate System |
title_sort |
intrinsic thermodynamical time-scales of the atmosphere-ocean-cryosphere climate system |
publishDate |
1993 |
url |
http://www.dtic.mil/docs/citations/ADA530527 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA530527 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic ice core |
genre_facet |
Antarc* Antarctic ice core |
op_source |
DTIC |
op_relation |
http://www.dtic.mil/docs/citations/ADA530527 |
op_rights |
Approved for public release; distribution is unlimited. |
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1766105615237644288 |