Climate sensitivity study with energy balance models

In this thesis, the sensitivity of the Earth's climate is studied by modeling past climatic variations with two-dimensional seasonal energy balance model. This thesis consists of two parts. The first part is a study of the interaction between the seasonal cycle and the small ice cap instability...

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Main Author: Huang, Jin
Other Authors: Bowman, Kenneth P.
Format: Text
Language:English
Published: 1991
Subjects:
Online Access:http://hdl.handle.net/2142/21016
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spelling ftunivillidea:oai:www.ideals.illinois.edu:2142/21016 2024-10-13T14:08:00+00:00 Climate sensitivity study with energy balance models Huang, Jin Bowman, Kenneth P. 1991 http://hdl.handle.net/2142/21016 eng eng AAI9210843 (UMI)AAI9210843 http://hdl.handle.net/2142/21016 Copyright 1991 Huang, Jin Physical Oceanography Paleoecology Physics Atmospheric Science text 1991 ftunivillidea 2024-10-01T12:57:43Z In this thesis, the sensitivity of the Earth's climate is studied by modeling past climatic variations with two-dimensional seasonal energy balance model. This thesis consists of two parts. The first part is a study of the interaction between the seasonal cycle and the small ice cap instability, which is a possible mechanism for the initiation of glaciation in the northern hemisphere and southern hemisphere. Results from a two-dimensional energy balance model with a realistic land-ocean distribution show that the small ice cap instability exists in the southern hemisphere, but not in the northern hemisphere. A series of experiments with a one-dimensional energy balance model with idealized geography is used to study the roles of the seasonal cycle and the land-ocean distribution. The results indicate that the seasonal cycle and land-ocean distribution can influence the strength of the albedo feedback, which is responsible for the small ice cap instability, through two factors: the temperature gradient and the amplitude of the seasonal cycle. The second part of this thesis is a study of the CO$\sb2$-climate feedback and its possible role in the 41 kyr sea surface temperature oscillation during the Matuyama chron (2.4 to 0.7 Myr BP). The CO$\sb2$-climate feedback is parameterized as an internal longwave radiation-polar temperature feedback in the energy balance model. Other physical processes are treated as boundary conditions. It is found that the CO$\sb2$-climate feedback can increase climate sensitivity to orbital parameters, especially to the obliquity changes, which have a 41 kyr cycle. The model results indicate that the CO$\sb2$-climate feedback is one of possible mechanisms for the dominant 41 kyr climate change during the Matuyama. (Abstract shortened with permission of author.) Made available in DSpace on 2011-05-07T12:55:52Z (GMT). No. of bitstreams: 2 license.txt: 4922 bytes, checksum: 910b249b4beec47e7ab768910c8f966f (MD5) 9210843.pdf: 4684861 bytes, checksum: 82e9af1e63c79ac052e09e5b7070d6b8 ... Text Ice cap University of Illinois at Urbana-Champaign: IDEALS (Illinois Digital Environment for Access to Learning and Scholarship)
institution Open Polar
collection University of Illinois at Urbana-Champaign: IDEALS (Illinois Digital Environment for Access to Learning and Scholarship)
op_collection_id ftunivillidea
language English
topic Physical Oceanography
Paleoecology
Physics
Atmospheric Science
spellingShingle Physical Oceanography
Paleoecology
Physics
Atmospheric Science
Huang, Jin
Climate sensitivity study with energy balance models
topic_facet Physical Oceanography
Paleoecology
Physics
Atmospheric Science
description In this thesis, the sensitivity of the Earth's climate is studied by modeling past climatic variations with two-dimensional seasonal energy balance model. This thesis consists of two parts. The first part is a study of the interaction between the seasonal cycle and the small ice cap instability, which is a possible mechanism for the initiation of glaciation in the northern hemisphere and southern hemisphere. Results from a two-dimensional energy balance model with a realistic land-ocean distribution show that the small ice cap instability exists in the southern hemisphere, but not in the northern hemisphere. A series of experiments with a one-dimensional energy balance model with idealized geography is used to study the roles of the seasonal cycle and the land-ocean distribution. The results indicate that the seasonal cycle and land-ocean distribution can influence the strength of the albedo feedback, which is responsible for the small ice cap instability, through two factors: the temperature gradient and the amplitude of the seasonal cycle. The second part of this thesis is a study of the CO$\sb2$-climate feedback and its possible role in the 41 kyr sea surface temperature oscillation during the Matuyama chron (2.4 to 0.7 Myr BP). The CO$\sb2$-climate feedback is parameterized as an internal longwave radiation-polar temperature feedback in the energy balance model. Other physical processes are treated as boundary conditions. It is found that the CO$\sb2$-climate feedback can increase climate sensitivity to orbital parameters, especially to the obliquity changes, which have a 41 kyr cycle. The model results indicate that the CO$\sb2$-climate feedback is one of possible mechanisms for the dominant 41 kyr climate change during the Matuyama. (Abstract shortened with permission of author.) Made available in DSpace on 2011-05-07T12:55:52Z (GMT). No. of bitstreams: 2 license.txt: 4922 bytes, checksum: 910b249b4beec47e7ab768910c8f966f (MD5) 9210843.pdf: 4684861 bytes, checksum: 82e9af1e63c79ac052e09e5b7070d6b8 ...
author2 Bowman, Kenneth P.
format Text
author Huang, Jin
author_facet Huang, Jin
author_sort Huang, Jin
title Climate sensitivity study with energy balance models
title_short Climate sensitivity study with energy balance models
title_full Climate sensitivity study with energy balance models
title_fullStr Climate sensitivity study with energy balance models
title_full_unstemmed Climate sensitivity study with energy balance models
title_sort climate sensitivity study with energy balance models
publishDate 1991
url http://hdl.handle.net/2142/21016
genre Ice cap
genre_facet Ice cap
op_relation AAI9210843
(UMI)AAI9210843
http://hdl.handle.net/2142/21016
op_rights Copyright 1991 Huang, Jin
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