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Titlebook: Radiation and Water in the Climate System; Remote Measurements Ehrhard Raschke Conference proceedings 1996 Springer-Verlag Berlin Heidelber

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Introduction to Numerical Weather Prediction Data Assimilationle information. A description of the current observing system can be found in McGrath (1993); around 105 elementary pieces of information are currently used over 24 hours by the operational data assimilation system.
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Conference proceedings 1996ssue within environmental and climate research. More reliable ways should be found to model them in their complex interplay with cascades of processes in that system, and their impact on all our resources on earth. Such modelling needs also validation with accurate and complete observations which in
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1431-7125 burning issue within environmental and climate research. More reliable ways should be found to model them in their complex interplay with cascades of processes in that system, and their impact on all our resources on earth. Such modelling needs also validation with accurate and complete observation
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Observational Requirements for Modeling of Global and Regional Climate Changelibrium doubled CO. calculations with atmosphere-only GCMs, and 8 are simulating transient greenhouse gas increase scenarios with coupled ocean-atmosphere models for the 1995 IPCC scientific assessment.
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Observational Requirements for Modeling of Global and Regional Climate Changeaerosol concentrations is perhaps the most important single problem in the earth sciences today. General circulation models (GCMs) are the tools of choice for making such projections. Simulating climate change with GCMs has become a worldwide activity; 12 modeling groups thus far have performed equi
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Introduction to Numerical Weather Prediction Data Assimilationle information. A description of the current observing system can be found in McGrath (1993); around 105 elementary pieces of information are currently used over 24 hours by the operational data assimilation system.
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