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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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