<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">469052678</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20180323132834.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">170328e19920601xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/BF01025621</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/BF01025621</subfield>
  </datafield>
  <datafield tag="100" ind1="1" ind2=" ">
   <subfield code="a">Bryson</subfield>
   <subfield code="D">R.</subfield>
   <subfield code="u">Center for Climatic Research, Institute for Environmental Studies, University of Wisconsin, 53706, Madison, Wisconsin, USA</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="245" ind1="1" ind2="2">
   <subfield code="a">A macrophysical model of the holocene intertropical convergence and jetstream positions and rainfall for the Saharan region</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[R. Bryson]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">Summary: Using a macrophysical model, it has been found possible to model the Late Pleistocene and Holocene history of glacial volume and mean temperature as a function of solar radiation seasonality and modulation of the solar radiation by volcanic aerosols (Bryson, 1988). From this model it has been possible to model the Indian monsoon with fair agreement with the field data (Bryson, 1989). The present paper represents an extension of this effort to the modeling of the position of the Intertropical Convergence in North Africa and the latitude of the atmospheric polar jetstream in the same longitudes. From these two latitudes it is possible to simulate the seasonal rainfall history of the Saharan region. The preliminary results suggest that maximum intrusion of summer rains into North Africa should have occurred between 11,000 and 5000 BP, with a lesser intrusion between 30,000 and 28,000 BP. Winter rains, though not abundant, should have been present in the central sahara until 12,000 BP then diminishing to negligible by 8000 BP, according to the model. On the Mediterranean coast of North Africa, the winter rains should have been about 100% greater than the present until about 18,000 BP, diminishing to near the present value by about 8000 BP. Radiocarbon dated occupation sites appear to be most abundant at about the indicated times of greatest rainfall in sub-Saharan Africa, as does the frequency of high lake levels. A collateral purpose of this paper is to test the utility of the present inter-monthly changes in the parameterization of inter-century changes.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Springer-Verlag, 1992</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Meteorology and Atmospheric Physics</subfield>
   <subfield code="d">Springer-Verlag</subfield>
   <subfield code="g">47/2-4(1992-06-01), 247-258</subfield>
   <subfield code="x">0177-7971</subfield>
   <subfield code="q">47:2-4&lt;247</subfield>
   <subfield code="1">1992</subfield>
   <subfield code="2">47</subfield>
   <subfield code="o">703</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/BF01025621</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/BF01025621</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">Bryson</subfield>
   <subfield code="D">R.</subfield>
   <subfield code="u">Center for Climatic Research, Institute for Environmental Studies, University of Wisconsin, 53706, Madison, Wisconsin, USA</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">Meteorology and Atmospheric Physics</subfield>
   <subfield code="d">Springer-Verlag</subfield>
   <subfield code="g">47/2-4(1992-06-01), 247-258</subfield>
   <subfield code="x">0177-7971</subfield>
   <subfield code="q">47:2-4&lt;247</subfield>
   <subfield code="1">1992</subfield>
   <subfield code="2">47</subfield>
   <subfield code="o">703</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>
