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    Evaluation of the Snow Simulations from the Community Land Model, Version 4 (CLM4)

    Source: Journal of Hydrometeorology:;2015:;Volume( 017 ):;issue: 001::page 153
    Author:
    Toure, Ally M.
    ,
    Rodell, Matthew
    ,
    Yang, Zong-Liang
    ,
    Beaudoing, Hiroko
    ,
    Kim, Edward
    ,
    Zhang, Yongfei
    ,
    Kwon, Yonghwan
    DOI: 10.1175/JHM-D-14-0165.1
    Publisher: American Meteorological Society
    Abstract: his paper evaluates the simulation of snow by the Community Land Model, version 4 (CLM4), the land model component of the Community Earth System Model, version 1.0.4 (CESM1.0.4). CLM4 was run in an offline mode forced with the corrected land-only replay of the Modern-Era Retrospective Analysis for Research and Applications (MERRA-Land) and the output was evaluated for the period from January 2001 to January 2011 over the Northern Hemisphere poleward of 30°N. Simulated snow-cover fraction (SCF), snow depth, and snow water equivalent (SWE) were compared against a set of observations including the Moderate Resolution Imaging Spectroradiometer (MODIS) SCF, the Interactive Multisensor Snow and Ice Mapping System (IMS) snow cover, the Canadian Meteorological Centre (CMC) daily snow analysis products, snow depth from the National Weather Service Cooperative Observer (COOP) program, and Snowpack Telemetry (SNOTEL) SWE observations. CLM4 SCF was converted into snow-cover extent (SCE) to compare with MODIS SCE. It showed good agreement, with a correlation coefficient of 0.91 and an average bias of ?1.54 ? 102 km2. Overall, CLM4 agreed well with IMS snow cover, with the percentage of correctly modeled snow?no snow being 94%. CLM4 snow depth and SWE agreed reasonably well with the CMC product, with the average bias (RMSE) of snow depth and SWE being 0.044 m (0.19 m) and ?0.010 m (0.04 m), respectively. CLM4 underestimated SNOTEL SWE and COOP snow depth. This study demonstrates the need to improve the CLM4 snow estimates and constitutes a benchmark against which improvement of the model through data assimilation can be measured.
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      Evaluation of the Snow Simulations from the Community Land Model, Version 4 (CLM4)

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    • Journal of Hydrometeorology

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    contributor authorToure, Ally M.
    contributor authorRodell, Matthew
    contributor authorYang, Zong-Liang
    contributor authorBeaudoing, Hiroko
    contributor authorKim, Edward
    contributor authorZhang, Yongfei
    contributor authorKwon, Yonghwan
    date accessioned2017-06-09T17:16:12Z
    date available2017-06-09T17:16:12Z
    date copyright2016/01/01
    date issued2015
    identifier issn1525-755X
    identifier otherams-82162.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4225246
    description abstracthis paper evaluates the simulation of snow by the Community Land Model, version 4 (CLM4), the land model component of the Community Earth System Model, version 1.0.4 (CESM1.0.4). CLM4 was run in an offline mode forced with the corrected land-only replay of the Modern-Era Retrospective Analysis for Research and Applications (MERRA-Land) and the output was evaluated for the period from January 2001 to January 2011 over the Northern Hemisphere poleward of 30°N. Simulated snow-cover fraction (SCF), snow depth, and snow water equivalent (SWE) were compared against a set of observations including the Moderate Resolution Imaging Spectroradiometer (MODIS) SCF, the Interactive Multisensor Snow and Ice Mapping System (IMS) snow cover, the Canadian Meteorological Centre (CMC) daily snow analysis products, snow depth from the National Weather Service Cooperative Observer (COOP) program, and Snowpack Telemetry (SNOTEL) SWE observations. CLM4 SCF was converted into snow-cover extent (SCE) to compare with MODIS SCE. It showed good agreement, with a correlation coefficient of 0.91 and an average bias of ?1.54 ? 102 km2. Overall, CLM4 agreed well with IMS snow cover, with the percentage of correctly modeled snow?no snow being 94%. CLM4 snow depth and SWE agreed reasonably well with the CMC product, with the average bias (RMSE) of snow depth and SWE being 0.044 m (0.19 m) and ?0.010 m (0.04 m), respectively. CLM4 underestimated SNOTEL SWE and COOP snow depth. This study demonstrates the need to improve the CLM4 snow estimates and constitutes a benchmark against which improvement of the model through data assimilation can be measured.
    publisherAmerican Meteorological Society
    titleEvaluation of the Snow Simulations from the Community Land Model, Version 4 (CLM4)
    typeJournal Paper
    journal volume17
    journal issue1
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/JHM-D-14-0165.1
    journal fristpage153
    journal lastpage170
    treeJournal of Hydrometeorology:;2015:;Volume( 017 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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