<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     naa a22        4500</leader>
  <controlfield tag="001">510753698</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180411083114.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">180411e20130901xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/s13131-013-0355-8</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/s13131-013-0355-8</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="4">
   <subfield code="a">The influence of thermohaline fronts on chlorophyll a concentrations during spring and summer in the southeastern Yellow Sea</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Pung-Guk Jang, Tong Lee, Jung-Hoon Kang, Kyoungsoon Shin]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">A spatial and temporal variation in physiochemical parameters in the southeastern Yellow Sea (YS) is investigated in the spring and summer of 2009 to 2011. Nutrient show a strong negative relationship with chlorophyll a (Chl a) concentration in spring, and the subsurface chlorophyll a maxima (SCM) layer was associated with the nitracline in summer. In summer, the SCM was usually found within or above the pycnocline and at the depths of shoals from the open sea to the coastal sea due to tidal and/or topographical fronts in the southernmost study area. High Chl a concentrations were found in the central southern YS, where the YS cold water layer expanded under the pycnocline and encountered water masses during spring and summer. After a typhoonin the summer of 2011, Chl a concentration increased, especially in the central southern YS, where cold waters occurred below the pycnocline. The results suggest that the development of thermohaline fronts may play an important role in the growth and accumulation of phytoplankton biomass in the upper layer of the southeastern YS during spring and summer.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">The Chinese Society of Oceanography and Springer-Verlag Berlin Heidelberg, 2013</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Yellow Sea ColdWater</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">nutrient</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">chorophyll a</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">thermohaline front</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Jang</subfield>
   <subfield code="D">Pung-Guk</subfield>
   <subfield code="u">Korea Institute of Ocean Science and Technology/South Sea Institute, 656-830, Geoje, Republic of Korea</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Lee</subfield>
   <subfield code="D">Tong</subfield>
   <subfield code="u">Department of Oceanography, College of Natural Sciences, Pusan National University, 609-735, Busan, Republic of Korea</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Kang</subfield>
   <subfield code="D">Jung-Hoon</subfield>
   <subfield code="u">Korea Institute of Ocean Science and Technology/South Sea Institute, 656-830, Geoje, Republic of Korea</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Shin</subfield>
   <subfield code="D">Kyoungsoon</subfield>
   <subfield code="u">Korea Institute of Ocean Science and Technology/South Sea Institute, 656-830, Geoje, Republic of Korea</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Acta Oceanologica Sinica</subfield>
   <subfield code="d">Springer Berlin Heidelberg</subfield>
   <subfield code="g">32/9(2013-09-01), 82-90</subfield>
   <subfield code="x">0253-505X</subfield>
   <subfield code="q">32:9&lt;82</subfield>
   <subfield code="1">2013</subfield>
   <subfield code="2">32</subfield>
   <subfield code="o">13131</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/s13131-013-0355-8</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="908" ind1=" " ind2=" ">
   <subfield code="D">1</subfield>
   <subfield code="a">research-article</subfield>
   <subfield code="2">jats</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">856</subfield>
   <subfield code="E">40</subfield>
   <subfield code="u">https://doi.org/10.1007/s13131-013-0355-8</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Jang</subfield>
   <subfield code="D">Pung-Guk</subfield>
   <subfield code="u">Korea Institute of Ocean Science and Technology/South Sea Institute, 656-830, Geoje, Republic of Korea</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Lee</subfield>
   <subfield code="D">Tong</subfield>
   <subfield code="u">Department of Oceanography, College of Natural Sciences, Pusan National University, 609-735, Busan, Republic of Korea</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Kang</subfield>
   <subfield code="D">Jung-Hoon</subfield>
   <subfield code="u">Korea Institute of Ocean Science and Technology/South Sea Institute, 656-830, Geoje, Republic of Korea</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">700</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Shin</subfield>
   <subfield code="D">Kyoungsoon</subfield>
   <subfield code="u">Korea Institute of Ocean Science and Technology/South Sea Institute, 656-830, Geoje, Republic of Korea</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="950" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="P">773</subfield>
   <subfield code="E">0-</subfield>
   <subfield code="t">Acta Oceanologica Sinica</subfield>
   <subfield code="d">Springer Berlin Heidelberg</subfield>
   <subfield code="g">32/9(2013-09-01), 82-90</subfield>
   <subfield code="x">0253-505X</subfield>
   <subfield code="q">32:9&lt;82</subfield>
   <subfield code="1">2013</subfield>
   <subfield code="2">32</subfield>
   <subfield code="o">13131</subfield>
  </datafield>
  <datafield tag="900" ind1=" " ind2="7">
   <subfield code="a">Metadata rights reserved</subfield>
   <subfield code="b">Springer special CC-BY-NC licence</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="898" ind1=" " ind2=" ">
   <subfield code="a">BK010053</subfield>
   <subfield code="b">XK010053</subfield>
   <subfield code="c">XK010000</subfield>
  </datafield>
  <datafield tag="949" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="F">NATIONALLICENCE</subfield>
   <subfield code="b">NL-springer</subfield>
  </datafield>
 </record>
</collection>
