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contributor authorPeng, Wei
contributor authorLiang, Xudong
contributor authorZhang, Xin
contributor authorHuang, Xiangyu
contributor authorLu, Bing
contributor authorFu, Qiao
date accessioned2017-06-09T17:34:26Z
date available2017-06-09T17:34:26Z
date copyright2017/06/01
date issued2017
identifier issn0027-0644
identifier otherams-87398.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4231062
description abstractenerally, the results of data assimilation are not well balanced dynamically due to errors in background, observations, or the model itself. So, initialization methods have been introduced to remove spurious gravity waves from the analysis. One of the initialization methods is digital filter initialization (DFI), which has been used in operational forecast systems, though its physical meaning is not well understood. Other methods eliminate high-frequency noise in optimized initial conditions by introducing physical constraints, such as the model constraint scheme, which minimizes the time tendency of model variables. In this study, a physical filter initialization (PFI) scheme, based on the model constraint scheme, is implemented in the four-dimensional variational data assimilation (4DVar) system of the Weather Research and Forecasting (WRF) Model. The impacts of the PFI scheme are examined by both single-observation and real-data experiments. The results indicate that the PFI scheme can eliminate high-frequency noise effectively, obtain flow-dependent analysis increments, and shorten forecast spinup time. Consequently, the precipitation forecast is improved to a certain extent, especially during the first few hours thanks to the shorter spinup time.
publisherAmerican Meteorological Society
titleApplication of Physical Filter Initialization in 4DVar
typeJournal Paper
journal volume145
journal issue6
journal titleMonthly Weather Review
identifier doi10.1175/MWR-D-16-0274.1
journal fristpage2201
journal lastpage2216
treeMonthly Weather Review:;2017:;volume( 145 ):;issue: 006
contenttypeFulltext


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