<?xml version="1.0" encoding="UTF-8"?>
<collection xmlns="http://www.loc.gov/MARC21/slim">
 <record>
  <leader>     caa a22        4500</leader>
  <controlfield tag="001">605472459</controlfield>
  <controlfield tag="003">CHVBK</controlfield>
  <controlfield tag="005">20210128100338.0</controlfield>
  <controlfield tag="007">cr unu---uuuuu</controlfield>
  <controlfield tag="008">210128e20151201xx      s     000 0 eng  </controlfield>
  <datafield tag="024" ind1="7" ind2="0">
   <subfield code="a">10.1007/s00382-015-2537-x</subfield>
   <subfield code="2">doi</subfield>
  </datafield>
  <datafield tag="035" ind1=" " ind2=" ">
   <subfield code="a">(NATIONALLICENCE)springer-10.1007/s00382-015-2537-x</subfield>
  </datafield>
  <datafield tag="245" ind1="0" ind2="0">
   <subfield code="a">Evaluation of large-scale meteorological patterns associated with temperature extremes in the NARCCAP regional climate model simulations</subfield>
   <subfield code="h">[Elektronische Daten]</subfield>
   <subfield code="c">[Paul Loikith, Duane Waliser, Huikyo Lee, J. Neelin, Benjamin Lintner, Seth McGinnis, Linda Mearns, Jinwon Kim]</subfield>
  </datafield>
  <datafield tag="520" ind1="3" ind2=" ">
   <subfield code="a">Large-scale meteorological patterns (LSMPs) associated with temperature extremes are evaluated in a suite of regional climate model (RCM) simulations contributing to the North American Regional Climate Change Assessment Program. LSMPs are characterized through composites of surface air temperature, sea level pressure, and 500hPa geopotential height anomalies concurrent with extreme temperature days. Six of the seventeen RCM simulations are driven by boundary conditions from reanalysis while the other eleven are driven by one of four global climate models (GCMs). Four illustrative case studies are analyzed in detail. Model fidelity in LSMP spatial representation is high for cold winter extremes near Chicago. Winter warm extremes are captured by most RCMs in northern California, with some notable exceptions. Model fidelity is lower for cool summer days near Houston and extreme summer heat events in the Ohio Valley. Physical interpretation of these patterns and identification of well-simulated cases, such as for Chicago, boosts confidence in the ability of these models to simulate days in the tails of the temperature distribution. Results appear consistent with the expectation that the ability of an RCM to reproduce a realistically shaped frequency distribution for temperature, especially at the tails, is related to its fidelity in simulating LMSPs. Each ensemble member is ranked for its ability to reproduce LSMPs associated with observed warm and cold extremes, identifying systematically high performing RCMs and the GCMs that provide superior boundary forcing. The methodology developed here provides a framework for identifying regions where further process-based evaluation would improve the understanding of simulation error and help guide future model improvement and downscaling efforts.</subfield>
  </datafield>
  <datafield tag="540" ind1=" " ind2=" ">
   <subfield code="a">Springer-Verlag Berlin Heidelberg, 2015</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Temperature extremes</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Regional climate modeling</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Large-scale meteorological patterns</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">North America</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="690" ind1=" " ind2="7">
   <subfield code="a">Model evaluation</subfield>
   <subfield code="2">nationallicence</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Loikith</subfield>
   <subfield code="D">Paul</subfield>
   <subfield code="u">Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Dr., 91101, Pasadena, CA, USA</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Waliser</subfield>
   <subfield code="D">Duane</subfield>
   <subfield code="u">Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Dr., 91101, Pasadena, CA, USA</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Lee</subfield>
   <subfield code="D">Huikyo</subfield>
   <subfield code="u">Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Dr., 91101, Pasadena, CA, USA</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Neelin</subfield>
   <subfield code="D">J.</subfield>
   <subfield code="u">Department of Atmospheric and Oceanic Science, University of California, Los Angeles, CA, USA</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Lintner</subfield>
   <subfield code="D">Benjamin</subfield>
   <subfield code="u">Department of Environmental Sciences, Rutgers, The State University of New Jersey, New Brunswick, NJ, USA</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">McGinnis</subfield>
   <subfield code="D">Seth</subfield>
   <subfield code="u">Institute for Mathematical Applications to the Geosciences, National Center for Atmospheric Research, Boulder, CO, USA</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Mearns</subfield>
   <subfield code="D">Linda</subfield>
   <subfield code="u">Institute for Mathematical Applications to the Geosciences, National Center for Atmospheric Research, Boulder, CO, USA</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="700" ind1="1" ind2=" ">
   <subfield code="a">Kim</subfield>
   <subfield code="D">Jinwon</subfield>
   <subfield code="u">Joint Institute for Regional Earth System Science and Engineering, University of California Los Angeles, Los Angeles, CA, USA</subfield>
   <subfield code="4">aut</subfield>
  </datafield>
  <datafield tag="773" ind1="0" ind2=" ">
   <subfield code="t">Climate Dynamics</subfield>
   <subfield code="d">Springer Berlin Heidelberg</subfield>
   <subfield code="g">45/11-12(2015-12-01), 3257-3274</subfield>
   <subfield code="x">0930-7575</subfield>
   <subfield code="q">45:11-12&lt;3257</subfield>
   <subfield code="1">2015</subfield>
   <subfield code="2">45</subfield>
   <subfield code="o">382</subfield>
  </datafield>
  <datafield tag="856" ind1="4" ind2="0">
   <subfield code="u">https://doi.org/10.1007/s00382-015-2537-x</subfield>
   <subfield code="q">text/html</subfield>
   <subfield code="z">Onlinezugriff via DOI</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="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="908" ind1=" " ind2=" ">
   <subfield code="D">1</subfield>
   <subfield code="a">research-article</subfield>
   <subfield code="2">jats</subfield>
  </datafield>
  <datafield tag="949" ind1=" " ind2=" ">
   <subfield code="B">NATIONALLICENCE</subfield>
   <subfield code="F">NATIONALLICENCE</subfield>
   <subfield code="b">NL-springer</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/s00382-015-2537-x</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">Loikith</subfield>
   <subfield code="D">Paul</subfield>
   <subfield code="u">Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Dr., 91101, Pasadena, CA, USA</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">Waliser</subfield>
   <subfield code="D">Duane</subfield>
   <subfield code="u">Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Dr., 91101, Pasadena, CA, USA</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">Huikyo</subfield>
   <subfield code="u">Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Dr., 91101, Pasadena, CA, USA</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">Neelin</subfield>
   <subfield code="D">J.</subfield>
   <subfield code="u">Department of Atmospheric and Oceanic Science, University of California, Los Angeles, CA, USA</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">Lintner</subfield>
   <subfield code="D">Benjamin</subfield>
   <subfield code="u">Department of Environmental Sciences, Rutgers, The State University of New Jersey, New Brunswick, NJ, USA</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">McGinnis</subfield>
   <subfield code="D">Seth</subfield>
   <subfield code="u">Institute for Mathematical Applications to the Geosciences, National Center for Atmospheric Research, Boulder, CO, USA</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">Mearns</subfield>
   <subfield code="D">Linda</subfield>
   <subfield code="u">Institute for Mathematical Applications to the Geosciences, National Center for Atmospheric Research, Boulder, CO, USA</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">Kim</subfield>
   <subfield code="D">Jinwon</subfield>
   <subfield code="u">Joint Institute for Regional Earth System Science and Engineering, University of California Los Angeles, Los Angeles, CA, 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">Climate Dynamics</subfield>
   <subfield code="d">Springer Berlin Heidelberg</subfield>
   <subfield code="g">45/11-12(2015-12-01), 3257-3274</subfield>
   <subfield code="x">0930-7575</subfield>
   <subfield code="q">45:11-12&lt;3257</subfield>
   <subfield code="1">2015</subfield>
   <subfield code="2">45</subfield>
   <subfield code="o">382</subfield>
  </datafield>
 </record>
</collection>
