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    The NCEP Climate Forecast System Reanalysis

    Source: Bulletin of the American Meteorological Society:;2010:;volume( 091 ):;issue: 008::page 1015
    Author:
    Saha, Suranjana
    ,
    Moorthi, Shrinivas
    ,
    Pan, Hua-Lu
    ,
    Wu, Xingren
    ,
    Wang, Jiande
    ,
    Nadiga, Sudhir
    ,
    Tripp, Patrick
    ,
    Kistler, Robert
    ,
    Woollen, John
    ,
    Behringer, David
    ,
    Liu, Haixia
    ,
    Stokes, Diane
    ,
    Grumbine, Robert
    ,
    Gayno, George
    ,
    Wang, Jun
    ,
    Hou, Yu-Tai
    ,
    Chuang, Hui-Ya
    ,
    Juang, Hann-Ming H.
    ,
    Sela, Joe
    ,
    Iredell, Mark
    ,
    Treadon, Russ
    ,
    Kleist, Daryl
    ,
    Van Delst, Paul
    ,
    Keyser, Dennis
    ,
    Derber, John
    ,
    Ek, Michael
    ,
    Meng, Jesse
    ,
    Wei, Helin
    ,
    Yang, Rongqian
    ,
    Lord, Stephen
    ,
    Van Den Dool, Huug
    ,
    Kumar, Arun
    ,
    Wang, Wanqiu
    ,
    Long, Craig
    ,
    Chelliah, Muthuvel
    ,
    Xue, Yan
    ,
    Huang, Boyin
    ,
    Schemm, Jae-Kyung
    ,
    Ebisuzaki, Wesley
    ,
    Lin, Roger
    ,
    Xie, Pingping
    ,
    Chen, Mingyue
    ,
    Zhou, Shuntai
    ,
    Higgins, Wayne
    ,
    Zou, Cheng-Zhi
    ,
    Liu, Quanhua
    ,
    Chen, Yong
    ,
    Han, Yong
    ,
    Cucurull, Lidia
    ,
    Reynolds, Richard W.
    ,
    Rutledge, Glenn
    ,
    Goldberg, Mitch
    DOI: 10.1175/2010BAMS3001.1
    Publisher: American Meteorological Society
    Abstract: 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 model has three layers. The CFSR atmospheric model has observed variations in carbon dioxide (CO2) over the 1979?2009 period, together with changes in aerosols and other trace gases and solar variations. Most available in situ and satellite observations were included in the CFSR. Satellite observations were used in radiance form, rather than retrieved values, and were bias corrected with ?spin up? runs at full resolution, taking into account variable CO2 concentrations. This procedure enabled the smooth transitions of the climate record resulting from evolutionary changes in the satellite observing system. CFSR atmospheric, oceanic, and land surface output products are available at an hourly time resolution and a horizontal resolution of 0.5° latitude ? 0.5° longitude. The CFSR data will be distributed by the National Climatic Data Center (NCDC) and NCAR. This reanalysis will serve many purposes, including providing the basis for most of the NCEP Climate Prediction Center's operational climate products by defining the mean states of the atmosphere, ocean, land surface, and sea ice over the next 30-yr climate normal (1981?2010); providing initial conditions for historical forecasts that are required to calibrate operational NCEP climate forecasts (from week 2 to 9 months); and providing estimates and diagnoses of the Earth's climate state over the satellite data period for community climate research. Preliminary analysis of the CFSR output indicates a product that is far superior in most respects to the reanalysis of the mid-1990s. The previous NCEP?NCAR reanalyses have been among the most used NCEP products in history; there is every reason to believe the CFSR will supersede these older products both in scope and quality, because it is higher in time and space resolution, covers the atmosphere, ocean, sea ice, and land, and was executed in a coupled mode with a more modern data assimilation system and forecast model. A supplement to this article is available online: DOI: 10.1175/2010BAMS3001.2.S1
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      The NCEP Climate Forecast System Reanalysis

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4211594
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    • Bulletin of the American Meteorological Society

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    contributor authorSaha, Suranjana
    contributor authorMoorthi, Shrinivas
    contributor authorPan, Hua-Lu
    contributor authorWu, Xingren
    contributor authorWang, Jiande
    contributor authorNadiga, Sudhir
    contributor authorTripp, Patrick
    contributor authorKistler, Robert
    contributor authorWoollen, John
    contributor authorBehringer, David
    contributor authorLiu, Haixia
    contributor authorStokes, Diane
    contributor authorGrumbine, Robert
    contributor authorGayno, George
    contributor authorWang, Jun
    contributor authorHou, Yu-Tai
    contributor authorChuang, Hui-Ya
    contributor authorJuang, Hann-Ming H.
    contributor authorSela, Joe
    contributor authorIredell, Mark
    contributor authorTreadon, Russ
    contributor authorKleist, Daryl
    contributor authorVan Delst, Paul
    contributor authorKeyser, Dennis
    contributor authorDerber, John
    contributor authorEk, Michael
    contributor authorMeng, Jesse
    contributor authorWei, Helin
    contributor authorYang, Rongqian
    contributor authorLord, Stephen
    contributor authorVan Den Dool, Huug
    contributor authorKumar, Arun
    contributor authorWang, Wanqiu
    contributor authorLong, Craig
    contributor authorChelliah, Muthuvel
    contributor authorXue, Yan
    contributor authorHuang, Boyin
    contributor authorSchemm, Jae-Kyung
    contributor authorEbisuzaki, Wesley
    contributor authorLin, Roger
    contributor authorXie, Pingping
    contributor authorChen, Mingyue
    contributor authorZhou, Shuntai
    contributor authorHiggins, Wayne
    contributor authorZou, Cheng-Zhi
    contributor authorLiu, Quanhua
    contributor authorChen, Yong
    contributor authorHan, Yong
    contributor authorCucurull, Lidia
    contributor authorReynolds, Richard W.
    contributor authorRutledge, Glenn
    contributor authorGoldberg, Mitch
    date accessioned2017-06-09T16:33:09Z
    date available2017-06-09T16:33:09Z
    date copyright2010/08/01
    date issued2010
    identifier issn0003-0007
    identifier otherams-69877.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4211594
    description abstractThe 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 model has three layers. The CFSR atmospheric model has observed variations in carbon dioxide (CO2) over the 1979?2009 period, together with changes in aerosols and other trace gases and solar variations. Most available in situ and satellite observations were included in the CFSR. Satellite observations were used in radiance form, rather than retrieved values, and were bias corrected with ?spin up? runs at full resolution, taking into account variable CO2 concentrations. This procedure enabled the smooth transitions of the climate record resulting from evolutionary changes in the satellite observing system. CFSR atmospheric, oceanic, and land surface output products are available at an hourly time resolution and a horizontal resolution of 0.5° latitude ? 0.5° longitude. The CFSR data will be distributed by the National Climatic Data Center (NCDC) and NCAR. This reanalysis will serve many purposes, including providing the basis for most of the NCEP Climate Prediction Center's operational climate products by defining the mean states of the atmosphere, ocean, land surface, and sea ice over the next 30-yr climate normal (1981?2010); providing initial conditions for historical forecasts that are required to calibrate operational NCEP climate forecasts (from week 2 to 9 months); and providing estimates and diagnoses of the Earth's climate state over the satellite data period for community climate research. Preliminary analysis of the CFSR output indicates a product that is far superior in most respects to the reanalysis of the mid-1990s. The previous NCEP?NCAR reanalyses have been among the most used NCEP products in history; there is every reason to believe the CFSR will supersede these older products both in scope and quality, because it is higher in time and space resolution, covers the atmosphere, ocean, sea ice, and land, and was executed in a coupled mode with a more modern data assimilation system and forecast model. A supplement to this article is available online: DOI: 10.1175/2010BAMS3001.2.S1
    publisherAmerican Meteorological Society
    titleThe NCEP Climate Forecast System Reanalysis
    typeJournal Paper
    journal volume91
    journal issue8
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/2010BAMS3001.1
    journal fristpage1015
    journal lastpage1057
    treeBulletin of the American Meteorological Society:;2010:;volume( 091 ):;issue: 008
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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