<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">469025883</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180323132729.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">170328e19920801xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/BF00185102</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/BF00185102</subfield>
  </datafield>
  <datafield tag="100" ind1="1" ind2=" ">
   <subfield code="a">Nesje</subfield>
   <subfield code="D">Atle</subfield>
   <subfield code="u">Department of Geography, University of Bergen, Breiviken 2, N-5035, Bergen-Sandviken, Norway</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="245" ind1="1" ind2="0">
   <subfield code="a">Topographical effects on the equilibrium-line altitude on glaciers</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Atle Nesje]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">The most common approaches used to calculate the equilibrium-line altitude (ELA) on former glaciers are: a) the maximum elevation of lateral moraines (MELM), b) the median elevation of glaciers (MEG), c) the toe-to-headwall altitude ratio (THAR), and d) the ratio of the accumulation area to the total area (AAR), of which the AAR method is considered to be the most accurate. A theoretical evaluation of the AAR approach, using changing slope angles and valley morphology on idealized glaciers at two different positions, shows that glaciers advancing into flat areas underestimate the ELA depression, while glaciers moving into areas of increasing slope angle, overestimate the ELA difference. Therefore, topographical and morphological effects on calculated ELA depressions on glaciers must be carefully evaluated.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Kluwer Academic Publishers, 1992</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">GeoJournal</subfield>
   <subfield code="d">Kluwer Academic Publishers</subfield>
   <subfield code="g">27/4(1992-08-01), 383-391</subfield>
   <subfield code="x">0343-2521</subfield>
   <subfield code="q">27:4&lt;383</subfield>
   <subfield code="1">1992</subfield>
   <subfield code="2">27</subfield>
   <subfield code="o">10708</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/BF00185102</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/BF00185102</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">100</subfield>
   <subfield code="E">1-</subfield>
   <subfield code="a">Nesje</subfield>
   <subfield code="D">Atle</subfield>
   <subfield code="u">Department of Geography, University of Bergen, Breiviken 2, N-5035, Bergen-Sandviken, Norway</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">GeoJournal</subfield>
   <subfield code="d">Kluwer Academic Publishers</subfield>
   <subfield code="g">27/4(1992-08-01), 383-391</subfield>
   <subfield code="x">0343-2521</subfield>
   <subfield code="q">27:4&lt;383</subfield>
   <subfield code="1">1992</subfield>
   <subfield code="2">27</subfield>
   <subfield code="o">10708</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>
