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Daily snow cover estimation from Advanced Very High Resolution Radiometer Polar Pathfinder data over Northern Hemisphere land surfaces during 1982-2004

Author
HONGXU ZHAO1 ; FERNANDES, Richard1
[1] Earth Sciences Sector, Canada Centre for Remote Sensing, Natural Resources Canada, Ottawa, Canada
Source

Journal of geophysical research. 2009, Vol 114, Num D5 ; D05113.1-D05113.14 ; ref : 3/4 p

ISSN
0148-0227
Scientific domain
Astronomy earth cosmic environment; Geology; Geophysics; Climatology, meteorology; Oceanography
Publisher
American Geophysical Union, Washington, DC
Publication country
United States
Document type
Article
Language
English
Keyword (fr)
Algorithme Carte Ciel serein Climat Courant Couverture neige Elément traceur Fonte neige Hémisphère Nord In situ Long terme Monde NOAA Neige Nébulosité Performance Printemps Profondeur Radiomètre Résolution spatiale Satellite Source Surface sol Très haute résolution Canada Eurasie Amérique du Nord
Keyword (en)
algorithms maps Clear sky climate currents Snow cover pathfinder elements Snow melt Northern Hemisphere in situ Long term global NOAA snow Cloudiness performances Spring(season) depth Radiometer spatial resolution satellites springs Ground surface very high resolution Canada Eurasia North America
Keyword (es)
Algoritmo Mapa Cielo sereno Clima Cubierta nieve Deshielo Hemisferio norte Largo plazo Mundo Nieve Nebulosidad Primavera Profundidad Radiómetro Satélite Fuente Superficie suelo Canada Eurasia America del norte
Classification
Pascal
001 Exact sciences and technology / 001E Earth, ocean, space / 001E01 Earth sciences

Discipline
Earth sciences
Origin
Inist-CNRS
Database
PASCAL
INIST identifier
21419711

Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS

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