<?xml version="1.0" encoding="UTF-8"?>
<rss xmlns:dc="http://purl.org/dc/elements/1.1/" version="2.0">
  <channel>
    <title>DSpace Collection:</title>
    <link>https://repository.kopri.re.kr/handle/201206/12729</link>
    <description />
    <pubDate>Sun, 19 Apr 2026 16:17:53 GMT</pubDate>
    <dc:date>2026-04-19T16:17:53Z</dc:date>
    <item>
      <title>Differentiating between first-year and multiyear sea ice in the Arctic using microwave-retrieved ice emissivities</title>
      <link>https://repository.kopri.re.kr/handle/201206/13020</link>
      <description>Title: Differentiating between first-year and multiyear sea ice in the Arctic using microwave-retrieved ice emissivities
Authors: Lee, Sang-Moo; Sohn, Byung-Ju; Kim, Seong-Joong
Abstract: Polarized emissivities of the sea ice over the Arctic were retrieved at Advanced Microwave&#xD;
Scanning RadiometerEOS 10.65, 18.7, 23.8, and 36.5 GHz channel frequencies. Results indicate that&#xD;
retrieved emissivities are consistent with other emissivity estimates. However, errors in the retrieved&#xD;
emissivity for multiyear sea ice at 23.8 and 36.5 GHz can be large up to 8% and 20%, respectively, because of&#xD;
ignoring the freeboard ice scattering and the use of the same emission layer as in 6.925 GHz. It is shown that&#xD;
the emissivity slope for first-year ice between 10.65 and 18.7 GHz is opposite to that for multiyear sea ice,&#xD;
enabling a distinction between first-year ice and multiyear ice. Using these differences in spectral features&#xD;
with ice types, an emissivity difference (vertically polarized emissivity difference between 10.65 and 18.7 GHz)&#xD;
was devised to differentiate between first-year sea ice and multiyear sea ice. A comparison with the ice status&#xD;
information obtained from Cold Regions Research and Engineering Laboratory buoy measurements&#xD;
demonstrates that the method can separate first-year ice from multiyear ice, implying that this technique&#xD;
enables us to obtain instantaneous and pixel-level ice-type information from space-based passive&#xD;
microwave measurements.</description>
      <pubDate>Sat, 27 May 2017 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">https://repository.kopri.re.kr/handle/201206/13020</guid>
      <dc:date>2017-05-27T00:00:00Z</dc:date>
    </item>
    <item>
      <title>Evolutionary Time Machine: A case study of sediment core sample from Larsen-C ice shelf in the Antarctica</title>
      <link>https://repository.kopri.re.kr/handle/201206/13129</link>
      <description>Title: Evolutionary Time Machine: A case study of sediment core sample from Larsen-C ice shelf in the Antarctica
Authors: 윤환수</description>
      <pubDate>Thu, 04 Aug 2016 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">https://repository.kopri.re.kr/handle/201206/13129</guid>
      <dc:date>2016-08-04T00:00:00Z</dc:date>
    </item>
    <item>
      <title>Source identification and distribution reveals the potential of the geochemical Antarctic sea ice proxy IPSO25</title>
      <link>https://repository.kopri.re.kr/handle/201206/13014</link>
      <description>Title: Source identification and distribution reveals the potential of the geochemical Antarctic sea ice proxy IPSO25
Authors: Belt, S. T.; Smik, L.; Brown, A.; Kim, J. -H.; Rowland, S. J.; Allen, C. S.; Gal, J. -K.; Shin, K. -H.; Lee, Jae Il; Taylor, K. W. R.
Abstract: The presence of a di-unsaturated highly branched isoprenoid (HBI) lipid biomarker (diene II)&#xD;
in Southern Ocean sediments has previously been proposed as a proxy measure of&#xD;
palaeo Antarctic sea ice. Here we show that a source of diene II is the sympagic diatom&#xD;
Berkeleya adeliensis Medlin. Furthermore, the propensity for B. adeliensis to flourish in platelet&#xD;
ice is reflected by an offshore downward gradient in diene II concentration in 4100 surface&#xD;
sediments from Antarctic coastal and near-coastal environments. Since platelet ice&#xD;
formation is strongly associated with super-cooled freshwater inflow, we further hypothesize&#xD;
that sedimentary diene II provides a potentially sensitive proxy indicator of landfast sea&#xD;
ice influenced by meltwater discharge from nearby glaciers and ice shelves, and&#xD;
re-examination of some previous diene II downcore records supports this hypothesis.&#xD;
The term IPSO25―Ice Proxy for the Southern Ocean with 25 carbon atoms―is proposed as a&#xD;
proxy name for diene II.</description>
      <pubDate>Mon, 01 Aug 2016 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">https://repository.kopri.re.kr/handle/201206/13014</guid>
      <dc:date>2016-08-01T00:00:00Z</dc:date>
    </item>
    <item>
      <title>Monitoring of the Antarctic ice sheet temperature changes using satellite microwave sensing</title>
      <link>https://repository.kopri.re.kr/handle/201206/13101</link>
      <description>Title: Monitoring of the Antarctic ice sheet temperature changes using satellite microwave sensing
Authors: Sohn, Byung-Ju</description>
      <pubDate>Sun, 31 Jul 2016 00:00:00 GMT</pubDate>
      <guid isPermaLink="false">https://repository.kopri.re.kr/handle/201206/13101</guid>
      <dc:date>2016-07-31T00:00:00Z</dc:date>
    </item>
  </channel>
</rss>

