Journal Information

Online ISSN: 1525-7541
Print ISSN:    1525-755X
Frequency:    Bimonthly .

Volume 9, Issue 6 (December 2008)

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

Janet Hardy, Robert Davis, and Yeohoon Koh

Cold Regions Research and Engineering Laboratory, Engineer Research and Development Center, U.S. Army Corps of Engineers, Hanover, New Hampshire

Don Cline

NOAA/NWS/National Operational Hydrologic Remote Sensing Center, Chanhassen, Minnesota

Kelly Elder

USDA Forest Service, Fort Collins, Colorado

Richard Armstrong and Hans-Peter Marshall

University of Colorado, Boulder, Colorado

Thomas Painter

University of Utah, Salt Lake City, Utah

Gilles Castres Saint-Martin, Roger DeRoo, and Kamal Sarabandi

University of Michigan, Ann Arbor, Michigan

Tobias Graf and Toshio Koike

University of Tokyo, Tokyo, Japan

Kyle McDonald

NASA Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California





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 μm) and a scanning thermal radiometer (8–12 μm) 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.

Keywords: Field experiments, Snow, Land surface, In situ observations, Remote sensing

Received: January 12, 2007; Accepted: March 19, 2008

Corresponding author address: Janet P. Hardy, CRREL, Engineer Research and Development Center, U.S. Army Corps of Engineers, 72 Lyme Road, Hanover, NH 03755. Email:

This article included in the The Cold Land Processes Experiment (CLPX) special collection.

Cited by

John W. Pomeroy, Danny Marks, Tim Link, Chad Ellis, Janet Hardy, Aled Rowlands, Raoul Granger. (2009) The impact of coniferous forest temperature on incoming longwave radiation to melting snow. Hydrological Processes 23:17, 2513-2525
Online publication date: 15-Aug-2009.
CrossRef
D. Marks, A. Winstral, G. Flerchinger, M. Reba, J. Pomeroy, T. Link, K. Elder. (2008) Comparing Simulated and Measured Sensible and Latent Heat Fluxes over Snow under a Pine Canopy to Improve an Energy Balance Snowmelt Model. Journal of Hydrometeorology 9:6, 1506-1522
Online publication date: 1-Dec-2008.
Abstract . Full Text . PDF (1100 KB)