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    NASA Cold Land Processes Experiment (CLPX 2002/03): Local Scale Observation Site

    Source: Journal of Hydrometeorology:;2008:;Volume( 009 ):;issue: 006::page 1434
    Author:
    Hardy, Janet
    ,
    Davis, Robert
    ,
    Koh, Yeohoon
    ,
    Cline, Don
    ,
    Elder, Kelly
    ,
    Armstrong, Richard
    ,
    Marshall, Hans-Peter
    ,
    Painter, Thomas
    ,
    Saint-Martin, Gilles Castres
    ,
    DeRoo, Roger
    ,
    Sarabandi, Kamal
    ,
    Graf, Tobias
    ,
    Koike, Toshio
    ,
    McDonald, Kyle
    DOI: 10.1175/2008JHM875.1
    Publisher: American Meteorological Society
    Abstract: The local scale observation site (LSOS) is the smallest study site (0.8 ha) of the 2002/03 Cold Land Processes Experiment (CLPX) and is located within the Fraser mesocell study area. It was the most intensively measured site of the CLPX, and measurements here had the greatest temporal component of all CLPX sites. Measurements made at the LSOS were designed to produce a comprehensive assessment of the snow, soil, and vegetation characteristics viewed by the ground-based remote sensing instruments. The objective of the ground-based microwave remote sensing was to collect time series of active and passive microwave spectral signatures over snow, soil, and forest, which is coincident with the intensive physical characterization of these features. Ground-based remote sensing instruments included frequency modulated continuous wave (FMCW) radars operating over multiple microwave bandwidths; the Ground-Based Microwave Radiometer (GBMR-7) operating at channels 18.7, 23.8, 36.5, and 89 GHz; and in 2003, an L-, C-, X- and Ku-band scatterometer radar system. Snow and soil measurements included standard snow physical properties, snow wetness, snow depth transects, and soil moisture. The stem and canopy temperature and xylem sap flux of several trees were monitored continuously. Five micrometeorological towers monitored ambient conditions and provided forcing datasets for 1D snow and soil models. Arrays of pyranometers (0.3?3 ?m) and a scanning thermal radiometer (8?12 ?m) characterized the variability of radiative receipt in the forests. A field spectroradiometer measured the hyperspectral hemispherical-directional reflectance of the snow surface. These measurements, together with the ground-based remote sensing, provide the framework for evaluating and improving microwave radiative transfer models and coupling them to land surface models. The dataset is archived at the National Snow and Ice Data Center (NSIDC) in Boulder, Colorado.
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      NASA Cold Land Processes Experiment (CLPX 2002/03): Local Scale Observation Site

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4208828
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    • Journal of Hydrometeorology

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    contributor authorHardy, Janet
    contributor authorDavis, Robert
    contributor authorKoh, Yeohoon
    contributor authorCline, Don
    contributor authorElder, Kelly
    contributor authorArmstrong, Richard
    contributor authorMarshall, Hans-Peter
    contributor authorPainter, Thomas
    contributor authorSaint-Martin, Gilles Castres
    contributor authorDeRoo, Roger
    contributor authorSarabandi, Kamal
    contributor authorGraf, Tobias
    contributor authorKoike, Toshio
    contributor authorMcDonald, Kyle
    date accessioned2017-06-09T16:24:45Z
    date available2017-06-09T16:24:45Z
    date copyright2008/12/01
    date issued2008
    identifier issn1525-755X
    identifier otherams-67387.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208828
    description abstractThe local scale observation site (LSOS) is the smallest study site (0.8 ha) of the 2002/03 Cold Land Processes Experiment (CLPX) and is located within the Fraser mesocell study area. It was the most intensively measured site of the CLPX, and measurements here had the greatest temporal component of all CLPX sites. Measurements made at the LSOS were designed to produce a comprehensive assessment of the snow, soil, and vegetation characteristics viewed by the ground-based remote sensing instruments. The objective of the ground-based microwave remote sensing was to collect time series of active and passive microwave spectral signatures over snow, soil, and forest, which is coincident with the intensive physical characterization of these features. Ground-based remote sensing instruments included frequency modulated continuous wave (FMCW) radars operating over multiple microwave bandwidths; the Ground-Based Microwave Radiometer (GBMR-7) operating at channels 18.7, 23.8, 36.5, and 89 GHz; and in 2003, an L-, C-, X- and Ku-band scatterometer radar system. Snow and soil measurements included standard snow physical properties, snow wetness, snow depth transects, and soil moisture. The stem and canopy temperature and xylem sap flux of several trees were monitored continuously. Five micrometeorological towers monitored ambient conditions and provided forcing datasets for 1D snow and soil models. Arrays of pyranometers (0.3?3 ?m) and a scanning thermal radiometer (8?12 ?m) characterized the variability of radiative receipt in the forests. A field spectroradiometer measured the hyperspectral hemispherical-directional reflectance of the snow surface. These measurements, together with the ground-based remote sensing, provide the framework for evaluating and improving microwave radiative transfer models and coupling them to land surface models. The dataset is archived at the National Snow and Ice Data Center (NSIDC) in Boulder, Colorado.
    publisherAmerican Meteorological Society
    titleNASA Cold Land Processes Experiment (CLPX 2002/03): Local Scale Observation Site
    typeJournal Paper
    journal volume9
    journal issue6
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/2008JHM875.1
    journal fristpage1434
    journal lastpage1442
    treeJournal of Hydrometeorology:;2008:;Volume( 009 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian