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contributor authorAndersson, Erik
contributor authorBauer, Peter
contributor authorBeljaars, Anton
contributor authorChevallier, Frederic
contributor authorHólm, Elías
contributor authorJanisková, Marta
contributor authorKållberg, Per
contributor authorKelly, Graeme
contributor authorLopez, Philippe
contributor authorMcnally, Anthony
contributor authorMoreau, Emmanuel
contributor authorSimmons, Adrian J.
contributor authorThépaut, Jean-Noël
contributor authorTompkins, Adrian M.
date accessioned2017-06-09T16:42:47Z
date available2017-06-09T16:42:47Z
date copyright2005/03/01
date issued2005
identifier issn0003-0007
identifier otherams-72794.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4214836
description abstractSeveral new types of satellite instrument will provide improved measurements of Earth's hydrological cycle and the humidity of the atmosphere. In an effort to make the best possible use of these data, the modeling and assimilation of humidity, clouds, and precipitation are currently the subjects of a comprehensive research program at the European Centre for Medium-Range Weather Forecasts (ECMWF). Impacts on weather prediction and climate reanalysis can be expected. The preparations for cloud and rain assimilation within ECMWF's four-dimensional variational data assimilation system include the development of linearized moist physics, the development of fast radiative transfer codes for cloudy and precipitating conditions, and a reformulation of the humidity analysis scheme. Results of model validations against in situ moisture data are presented, indicating generally good agreement?often to within the absolute calibration accuracy of the measurements. Evidence is also presented of shortcomings in ECMWF's humidity analysis, from the operational data assimilation and forecasting system in 2002, and from the recently completed ERA-40 reanalysis project. Examples are shown of biases in the data and in the model that lead to biased humidity analyses. Although these biases are relatively small, they contribute to an overprediction of tropical precipitation and to an overly intense Hadley circulation at the start of the forecast, with rapid adjustments taking place during the first 6?12 h. It is shown that with an improved humidity analysis this long-standing ?spindown? problem can be reduced.
publisherAmerican Meteorological Society
titleAssimilation and Modeling of the Atmospheric Hydrological Cycle in the ECMWF Forecasting System
typeJournal Paper
journal volume86
journal issue3
journal titleBulletin of the American Meteorological Society
identifier doi10.1175/BAMS-86-3-387
journal fristpage387
journal lastpage402
treeBulletin of the American Meteorological Society:;2005:;volume( 086 ):;issue: 003
contenttypeFulltext


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