The NCEP Climate Forecast System Reanalysis
| Autor: | Wanqiu Wang, Rongqian Yang, Hann-Ming Henry Juang, Stephen J. Lord, Richard W. Reynolds, Robert Kistler, John S. Woollen, Mingyue Chen, Arun Kumar, Yong Han, Yong Chen, Muthuvel Chelliah, Yu-Tai Hou, Shrinivas Moorthi, Pingping Xie, Quanhua Liu, Mitch Goldberg, Paul van Delst, Glenn Rutledge, Hua-Lu Pan, Craig S. Long, Lidia Cucurull, Sudhir Nadiga, Wayne Higgins, Cheng-Zhi Zou, Jun Wang, Suranjana Saha, Joe Sela, Daryl T. Kleist, David Behringer, Mark Iredell, Jae-Kyung E. Schemm, Michael Ek, Helin Wei, Roger Lin, Shuntai Zhou, Yan Xue, Jiande Wang, Diane Stokes, Robert Grumbine, Hui-ya Chuang, Xingren Wu, George Gayno, Russ Treadon, Haixia Liu, Boyin Huang, Dennis Keyser, Huug van den Dool, John Derber, Jesse Meng, Patrick Tripp, Wesley Ebisuzaki |
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| Rok vydání: | 2010 |
| Předmět: |
Atmospheric Science
Meteorological reanalysis geography geography.geographical_feature_category 010504 meteorology & atmospheric sciences Meteorology Equator 0207 environmental engineering 02 engineering and technology 01 natural sciences Atmosphere 13. Climate action Climatology Climate Forecast System Sea ice Environmental science Satellite 020701 environmental engineering 0105 earth and related environmental sciences |
| Zdroj: | Bulletin of the American Meteorological Society. 91:1015-1058 |
| ISSN: | 1520-0477 0003-0007 |
| Popis: | The NCEP Climate Forecast System Reanalysis (CFSR) was completed for the 31-yr period from 1979 to 2009, in January 2010. The CFSR was designed and executed as a global, high-resolution coupled atmosphere–ocean–land surface–sea ice system to provide the best estimate of the state of these coupled domains over this period. The current CFSR will be extended as an operational, real-time product into the future. New features of the CFSR include 1) coupling of the atmosphere and ocean during the generation of the 6-h guess field, 2) an interactive sea ice model, and 3) assimilation of satellite radiances by the Gridpoint Statistical Interpolation (GSI) scheme over the entire period. The CFSR global atmosphere resolution is ~38 km (T382) with 64 levels extending from the surface to 0.26 hPa. The global ocean's latitudinal spacing is 0.25° at the equator, extending to a global 0.5° beyond the tropics, with 40 levels to a depth of 4737 m. The global land surface model has four soil levels and the global sea ice m... |
| Databáze: | OpenAIRE |
| Externí odkaz: |
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