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    <link>https://repository.kopri.re.kr/handle/201206/5207</link>
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    <pubDate>Sun, 26 Apr 2026 12:35:44 GMT</pubDate>
    <dc:date>2026-04-26T12:35:44Z</dc:date>
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      <title>Development of damage monitoring system for health monitoring to permafrost in polar regions</title>
      <link>https://repository.kopri.re.kr/handle/201206/13189</link>
      <description>Title: Development of damage monitoring system for health monitoring to permafrost in polar regions
Authors: Lee, Bang Yong</description>
      <pubDate>Thu, 01 Nov 2018 00:00:00 GMT</pubDate>
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      <dc:date>2018-11-01T00:00:00Z</dc:date>
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    <item>
      <title>Development of Shallow-Depth Soil Temperature Estimation Model Based on Thermal Response in Permafrost Area</title>
      <link>https://repository.kopri.re.kr/handle/201206/9527</link>
      <description>Title: Development of Shallow-Depth Soil Temperature Estimation Model Based on Thermal Response in Permafrost Area
Authors: Park, Keunbo; Kim, Dongwook; Lee, Bang Yong; Yang, Heekwon
Abstract: A soil temperature estimation model for increasing depth in a permafrost area in Alaska near the Bering Sea is proposed based on a thermal response concept. Thermal response is a measure of the internal physical heat transfer of soil due to transferred heat into the soil. Soil temperature data at different depths from late spring to the early autumn period at multiple permafrost sites were collected using automatic sensor measurements. From the analysis results, a model was established based on the relationship between the normalized cumulative soil temperatures (CRCST*i,m and CST*ud,m) of two different depths. CST*ud,m is the parameter of the soil temperature measurement at a depth of 5 cm, and CRCST*i,m is the parameter of the soil temperature measured at deeper depths of i cm (i = 10, 15, 20, and 30). Additionally, the fitting parameters of the mathematical models of the CRCST*i,m？CST*ud,m relationship were determined. The measured soil temperature depth profiles at a different site were compared with their predicted soil temperatures using the developed model for the model validation purpose. Consequently, the predicted soil temperatures at different soil depths using the soil temperature measurement of the uppermost depth (5 cm) were in good agreement with the measured results.</description>
      <pubDate>Mon, 01 Oct 2018 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">https://repository.kopri.re.kr/handle/201206/9527</guid>
      <dc:date>2018-10-01T00:00:00Z</dc:date>
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      <title>Development of damage monitoring system and evaluation of health monitoring</title>
      <link>https://repository.kopri.re.kr/handle/201206/12020</link>
      <description>Title: Development of damage monitoring system and evaluation of health monitoring
Authors: Lee, Bang Yong</description>
      <pubDate>Fri, 01 Dec 2017 00:00:00 GMT</pubDate>
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      <dc:date>2017-12-01T00:00:00Z</dc:date>
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      <title>Development of damage monitoring system and evaluation of health monitoring</title>
      <link>https://repository.kopri.re.kr/handle/201206/12021</link>
      <description>Title: Development of damage monitoring system and evaluation of health monitoring
Authors: Lee, Bang Yong</description>
      <pubDate>Sun, 01 Jan 2017 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">https://repository.kopri.re.kr/handle/201206/12021</guid>
      <dc:date>2017-01-01T00:00:00Z</dc:date>
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