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        <identifier>oai:www.ideals.illinois.edu:2142/21016</identifier>
        <datestamp>2023-07-10</datestamp>
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        <thesis xmlns="http://www.ndltd.org/standards/metadata/etdms/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/" xsi:schemaLocation="http://www.ndltd.org/standards/metadata/etdms/1.1/ http://www.ndltd.org/standards/metadata/etdms/1.1/etdms11.xsd http://purl.org/dc/elements/1.1/ http://www.ndltd.org/standards/metadata/etdms/1.1/etdmsdc.xsd">
          <dc:contributor>Bowman, Kenneth P.</dc:contributor>
          <dc:creator>Huang, Jin</dc:creator>
          <dc:date>2011-05-07T12:55:52Z</dc:date>
          <dc:date>2011-05-07T12:55:52Z</dc:date>
          <dc:date>10000-01-01</dc:date>
          <dc:date>1991</dc:date>
          <dc: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.</dc:description>
          <dc:description>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.)</dc:description>
          <dc:description>Made available in DSpace on 2011-05-07T12:55:52Z (GMT). No. of bitstreams: 2
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  Previous issue date: 1991</dc:description>
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Item is restricted indefinitely.</dc:description>
          <dc:description>Restriction data tranferred 2014-07-01T11:21:40-05:00
Original Data
Group with Access UIUC Users [automated]
Release Date: none
Reason: ETDs are only available to UIUC Users without author permission</dc:description>
          <dc:description>ETDs are only available to UIUC Users without author permission</dc:description>
          <dc:description>U of I Only</dc:description>
          <dc:identifier>AAI9210843</dc:identifier>
          <dc:identifier>(UMI)AAI9210843</dc:identifier>
          <dc:identifier>http://hdl.handle.net/2142/21016</dc:identifier>
          <dc:language>eng</dc:language>
          <dc:rights>Copyright 1991 Huang, Jin</dc:rights>
          <dc:subject>Physical Oceanography</dc:subject>
          <dc:subject>Paleoecology</dc:subject>
          <dc:subject>Physics, Atmospheric Science</dc:subject>
          <dc:title>Climate sensitivity study with energy balance models</dc:title>
          <dc:type>text</dc:type>
          <degree>
            <department>Atmospheric Science</department>
            <discipline>Atmospheric Science</discipline>
            <grantor>University of Illinois at Urbana-Champaign</grantor>
            <level>Dissertation</level>
            <name>Ph.D.</name>
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