Cold Regions Hydrology High-Resolution Observatory for Snow and Cold Land Processes

被引:144
作者
Rott, Helmut [1 ,2 ]
Yueh, Simon H. [3 ]
Cline, Donald W. [4 ]
Duguay, Claude [5 ]
Essery, Richard [6 ]
Haas, Christian [7 ,8 ]
Heliere, Florence [9 ]
Kern, Michael [9 ]
Macelloni, Giovanni [10 ]
Malnes, Eirik [11 ]
Nagler, Thomas [2 ]
Pulliainen, Jouni [12 ]
Rebhan, Helge [9 ]
Thompson, Alan [9 ]
机构
[1] Univ Innsbruck, Inst Meteorol & Geophys, A-6020 Innsbruck, Austria
[2] ENVEO IT, A-6020 Innsbruck, Austria
[3] CALTECH, Jet Prop Lab, Pasadena, CA 91125 USA
[4] NOAA NOHRSC, Chanhassen, MN 55317 USA
[5] Univ Waterloo, Waterloo, ON N2L 3G1, Canada
[6] Univ Edinburgh, Sch Geosci, Edinburgh EH8 9XP, Midlothian, Scotland
[7] Univ Alberta, Edmonton, AB T6G 2E1, Canada
[8] Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany
[9] ESA ESTEC, NL-2201 AZ Noordwijk, Netherlands
[10] IFAC CNR, I-50127 Florence, Italy
[11] NORUT IT, N-9291 Tromso, Norway
[12] Finnish Meteorol Inst, Helsinki 00560, Finland
基金
美国国家航空航天局;
关键词
Climate research; earth observation satellite; glaciers; snow cover; synthetic aperture radar; water resources; BACKSCATTERING COEFFICIENT; MASS-BALANCE; SCATTERING; SAR; VARIABILITY; SIMULATIONS; EXTENT; PHASE;
D O I
10.1109/JPROC.2009.2038947
中图分类号
TM [电工技术]; TN [电子技术、通信技术];
学科分类号
0808 ; 0809 ;
摘要
Snow is a critical component of the global water cycle and climate system, and a major source of water supply in many parts of the world. There is a lack of spatially distributed information on the accumulation of snow on land surfaces, glaciers, lake ice, and sea ice. Satellite missions for systematic and global snow observations will be essential to improve the representation of the cryosphere in climate models and to advance the knowledge and prediction of the water cycle variability and changes that depend on snow and ice resources. This paper describes the scientific drivers and technical approach of the proposed Cold Regions Hydrology High-Resolution Observatory (CoReH2O) satellite mission for snow and cold land processes. The sensor is a synthetic aperture radar operating at 17.2 and 9.6 GHz, VV and VH polarizations. The dual-frequency and dual-polarization design enables the decomposition of the scattering signal for retrieving snow mass and other physical properties of snow and ice.
引用
收藏
页码:752 / 765
页数:14
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