<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>Martin P. Hoerling</dc:contributor>
  <dc:contributor>Christopher C. Funk</dc:contributor>
  <dc:contributor>Ileana Blade</dc:contributor>
  <dc:contributor>Randall M. Dole</dc:contributor>
  <dc:contributor>Dave Allured</dc:contributor>
  <dc:contributor>Xiaowei Quan</dc:contributor>
  <dc:contributor>Jon K. Eischeid</dc:contributor>
  <dc:creator>Brant Liebmann</dc:creator>
  <dc:date>2014</dc:date>
  <dc:description>&lt;p&gt;Observations and sea surface temperature (SST)-forced ECHAM5 simulations are examined to study the seasonal cycle of eastern Africa rainfall and its SST sensitivity during 1979&amp;ndash;2012, focusing on interannual variability and trends. The eastern Horn is drier than the rest of equatorial Africa, with two distinct wet seasons, and whereas the October&amp;ndash;December wet season has become wetter, the March&amp;ndash;May season has become drier.&lt;/p&gt;
&lt;p&gt;The climatological rainfall in simulations driven by observed SSTs captures this bimodal regime. The simulated trends also qualitatively reproduce the opposite-sign changes in the two rainy seasons, suggesting that SST forcing has played an important role in the observed changes. The consistency between the sign of 1979&amp;ndash;2012 trends and interannual SST&amp;ndash;precipitation correlations is exploited to identify the most likely locations of SST forcing of precipitation trends in the model, and conceivably also in nature. Results indicate that the observed March&amp;ndash;May drying since 1979 is due to sensitivity to an increased zonal gradient in SST between Indonesia and the central Pacific. In contrast, the October&amp;ndash;December precipitation increase is mostly due to western Indian Ocean warming.&lt;/p&gt;
&lt;p class="last"&gt;The recent upward trend in the October&amp;ndash;December wet season is rather weak, however, and its statistical significance is compromised by strong year-to-year fluctuations. October&amp;ndash;December eastern Horn rain variability is strongly associated with El Ni&amp;ntilde;o&amp;ndash;Southern Oscillation and Indian Ocean dipole phenomena on interannual scales, in both model and observations. The interannual October&amp;ndash;December correlation between the ensemble-average and observed Horn rainfall 0.87. By comparison, interannual March&amp;ndash;May Horn precipitation is only weakly constrained by SST anomalies.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.1175/JCLI-D-13-00714.1</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>American Meteorological Society</dc:publisher>
  <dc:title>Understanding recent eastern Horn of Africa rainfall variability and change</dc:title>
  <dc:type>article</dc:type>
</oai_dc:dc>