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    Characterizing Sierra Nevada Snowpack Using Variable-Resolution CESM

    Source: Journal of Applied Meteorology and Climatology:;2015:;volume( 055 ):;issue: 001::page 173
    Author:
    Rhoades, Alan M.
    ,
    Huang, Xingying
    ,
    Ullrich, Paul A.
    ,
    Zarzycki, Colin M.
    DOI: 10.1175/JAMC-D-15-0156.1
    Publisher: American Meteorological Society
    Abstract: he location, timing, and intermittency of precipitation in California make the state integrally reliant on winter-season snowpack accumulation to maintain its economic and agricultural livelihood. Of particular concern is that winter-season snowpack has shown a net decline across the western United States over the past 50 years, resulting in major uncertainty in water-resource management heading into the next century. Cutting-edge tools are available to help navigate and preemptively plan for these uncertainties. This paper uses a next-generation modeling technique?variable-resolution global climate modeling within the Community Earth System Model (VR-CESM)?at horizontal resolutions of 0.125° (14 km) and 0.25° (28 km). VR-CESM provides the means to include dynamically large-scale atmosphere?ocean drivers, to limit model bias, and to provide more accurate representations of regional topography while doing so in a more computationally efficient manner than can be achieved with conventional general circulation models. This paper validates VR-CESM at climatological and seasonal time scales for Sierra Nevada snowpack metrics by comparing them with the ?Daymet,? ?Cal-Adapt,? NARR, NCEP, and North American Land Data Assimilation System (NLDAS) reanalysis datasets, the MODIS remote sensing dataset, the SNOTEL observational dataset, a standard-practice global climate model (CESM), and a regional climate model (WRF Model) dataset. Overall, given California?s complex terrain and intermittent precipitation and that both of the VR-CESM simulations were only constrained by prescribed sea surface temperatures and data on sea ice extent, a 0.68 centered Pearson product-moment correlation, a negative mean SWE bias of <7 mm, an interquartile range well within the values exhibited in the reanalysis datasets, and a mean December?February extent of snow cover that is within 7% of the expected MODIS value together make apparent the efficacy of the VR-CESM framework.
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      Characterizing Sierra Nevada Snowpack Using Variable-Resolution CESM

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    contributor authorRhoades, Alan M.
    contributor authorHuang, Xingying
    contributor authorUllrich, Paul A.
    contributor authorZarzycki, Colin M.
    date accessioned2017-06-09T16:50:58Z
    date available2017-06-09T16:50:58Z
    date copyright2016/01/01
    date issued2015
    identifier issn1558-8424
    identifier otherams-75240.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4217554
    description abstracthe location, timing, and intermittency of precipitation in California make the state integrally reliant on winter-season snowpack accumulation to maintain its economic and agricultural livelihood. Of particular concern is that winter-season snowpack has shown a net decline across the western United States over the past 50 years, resulting in major uncertainty in water-resource management heading into the next century. Cutting-edge tools are available to help navigate and preemptively plan for these uncertainties. This paper uses a next-generation modeling technique?variable-resolution global climate modeling within the Community Earth System Model (VR-CESM)?at horizontal resolutions of 0.125° (14 km) and 0.25° (28 km). VR-CESM provides the means to include dynamically large-scale atmosphere?ocean drivers, to limit model bias, and to provide more accurate representations of regional topography while doing so in a more computationally efficient manner than can be achieved with conventional general circulation models. This paper validates VR-CESM at climatological and seasonal time scales for Sierra Nevada snowpack metrics by comparing them with the ?Daymet,? ?Cal-Adapt,? NARR, NCEP, and North American Land Data Assimilation System (NLDAS) reanalysis datasets, the MODIS remote sensing dataset, the SNOTEL observational dataset, a standard-practice global climate model (CESM), and a regional climate model (WRF Model) dataset. Overall, given California?s complex terrain and intermittent precipitation and that both of the VR-CESM simulations were only constrained by prescribed sea surface temperatures and data on sea ice extent, a 0.68 centered Pearson product-moment correlation, a negative mean SWE bias of <7 mm, an interquartile range well within the values exhibited in the reanalysis datasets, and a mean December?February extent of snow cover that is within 7% of the expected MODIS value together make apparent the efficacy of the VR-CESM framework.
    publisherAmerican Meteorological Society
    titleCharacterizing Sierra Nevada Snowpack Using Variable-Resolution CESM
    typeJournal Paper
    journal volume55
    journal issue1
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/JAMC-D-15-0156.1
    journal fristpage173
    journal lastpage196
    treeJournal of Applied Meteorology and Climatology:;2015:;volume( 055 ):;issue: 001
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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