Implementation of Noah land surface model advances in the National Centers for Environmental Prediction operational mesoscale Eta model

  • M. B. Ek
    Environmental Modeling Center, National Centers for Environmental Prediction Suitland Maryland USA
  • K. E. Mitchell
    Environmental Modeling Center, National Centers for Environmental Prediction Suitland Maryland USA
  • Y. Lin
    Environmental Modeling Center, National Centers for Environmental Prediction Suitland Maryland USA
  • E. Rogers
    Environmental Modeling Center, National Centers for Environmental Prediction Suitland Maryland USA
  • P. Grunmann
    Environmental Modeling Center, National Centers for Environmental Prediction Suitland Maryland USA
  • V. Koren
    Office of Hydrologic Development, National Weather Service Silver Spring Maryland USA
  • G. Gayno
    Air Force Weather Agency Offutt Air Force Base Nebraska USA
  • J. D. Tarpley
    Office of Research and Applications National Environmental Satellite Data and Information Service Suitland Maryland USA

書誌事項

公開日
2003-11-27
権利情報
  • http://onlinelibrary.wiley.com/termsAndConditions#vor
DOI
  • 10.1029/2002jd003296
公開者
American Geophysical Union (AGU)

この論文をさがす

説明

<jats:p>We present the impact tests that preceded the most recent operational upgrades to the land surface model used in the National Centers for Environmental Prediction (NCEP) mesoscale Eta model, whose operational domain includes North America. These improvements consist of changes to the “Noah” land surface model (LSM) physics, most notable in the area of cold season processes. Results indicate improved performance in forecasting low‐level temperature and humidity, with improvements to (or without affecting) the overall performance of the Eta model quantitative precipitation scores and upper air verification statistics. Remaining issues that directly affect the Noah LSM performance in the Eta model include physical parameterizations of radiation and clouds, which affect the amount of available energy at the surface, and stable boundary layer and surface layer processes, which affect surface turbulent heat fluxes and ultimately the surface energy budget.</jats:p>

収録刊行物

被引用文献 (48)*注記

もっと見る

問題の指摘

ページトップへ