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pro vyhledávání: '"G. Deblonde"'
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Akademický článek
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Publikováno v:
Journal of Hydrometeorology. 8:1225-1242
A Canadian Land Data Assimilation System (CaLDAS) for the analysis of land surface prognostic variables is designed and implemented at the Meteorological Service of Canada for the initialization of numerical weather prediction and climate models. The
Publikováno v:
Monthly Weather Review. 135:152-172
Currently, satellite radiances in the Canadian Meteorological Centre operational data assimilation system are only assimilated in clear skies. A two-step method, developed at the European Centre for Medium-Range Weather Forecasts, is considered to as
Publikováno v:
Bulletin of the American Meteorological Society. 81:2213-2221
The American Meteorological Society held its Tenth Conference on Satellite Meteorology and Oceanography in conjunction with the 80th Annual Meeting in Long Beach, California. For the second consecutive conference, a format that consisted of primarily
Autor:
G. DeBlonde, W. R. Peltier
Publikováno v:
Journal of Climate. 6:709-727
Ice age scenarios for the last glacial interglacial cycle, based on observations of Boyle and Keigwin concerning the North Atlantic thermohaline circulation and of Barnola et al. concerning atmospheric CO[sub 2] variations derived from the Vostok ice
Autor:
G. Deblonde, J. Cihlar
Publikováno v:
Remote Sensing Reviews. 7:151-177
The relationships between the normalized difference vegetation index (NDVI) and surface environmental variables are studied across the Canadian landmass using data over a six year period (1982 to 1987). The NDVI images are 15 day composites over the
Publikováno v:
Global and Planetary Change. 6:37-55
The variations of Northern Hemisphere continental ice sheet extent (excepting on Greenland) are simulated over the last glacial-interglacial cycle of Late Pleistocene time using an ice sheet model (ISM) which is asynchronously coupled to a climate mo
Autor:
G. Deblonde, W. R. Peltier
Publikováno v:
Journal of Climate. 4:318-344
A new one-dimensional, zonally averaged high resolution spherical model of the accumulation and flow of continental ice sheets in response to variations in insolation forcing has been constructed. The model includes a detailed representation of the i
Autor:
W. R. Peltier, G Deblonde
Publikováno v:
Climate Dynamics. 5:103-110
A global two-dimensional one-level seasonal energy-balance model is asynchronously coupled to vertically integrated ice-flow models (which depend both on latitude and longitude) to study the response of the atmosphere-ocean-cryosphere-lithosphere sys