Read e-book online Precipitation Modeling and Quantitative Analysis PDF

By Xiaofan Li, Shouting Gao

ISBN-10: 9400723806

ISBN-13: 9789400723801

The e-book examines floor rainfall tactics via cloud-resolving modeling and quantitative research of floor rainfall funds and summarizes modeling and research ends up in contemporary seven years. The publication indicates validation of precipitation modeling opposed to observations and derives a collection of diagnostic precipitation equations. The ebook offers specific discussions of the functions of precipitation equations to the exam of results of sea floor temperature, vertical wind shear, radiation, and ice clouds on torrential rainfall procedures within the tropics and mid-latitudes, and to the reviews of sensitivity of precipitation modeling to uncertainty of the preliminary stipulations and to the estimate of precipitation potency. The e-book can be utilized as a textual content ebook for graduate scholars and may be necessary to researchers and forecasters for precipitation procedure reviews and operational forecasts.

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Extra resources for Precipitation Modeling and Quantitative Analysis

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There is a similarity in the peak rainfall period, whereas the differences between observed and simulated rain rate could be up to 2 mm h−1, particular at the beginning and end of the period. The differences may result partially from the comparison of small hourly local sampling of rain gauge observations over 35% of model domain over land and no rain gauge observations over 65% of model domain over ocean with large model domain averages of model simulation data in PSR with imposed 6-hourly large-scale forcing.

7) during a selected area and period of rainfall event in SCSMEX. A major rainband initiates around 670 km after 0500 LST as started by the enhanced water vapor convergence. The water vapor convergence plus surface evaporation is used to moisten local atmosphere. At 0600 LST, water vapor convergence rate increases significantly, which supports local atmospheric moistening, the growth of clouds and surface rainfall. Only water microphysical process occurs at this time. The vapor condensation produces rainfall mainly through the collection of cloud water by rain (PRACW).

2009) compared domain-mean simulated surface rain rate in BILIS with observed surface rain rate in Fig. 8. The observed surface rain rate is calculated using the rain gauge data in the model domain (108–116°E, 23–24°N). The simulated and observed surface rain rates show a similarity, in particular, during the period of 16–17 July 2006. The simulated rain rate differs from the observed rain rate. First, the simulated rain rate leads the observed rain rate by 3–5 h. Second, the simulated rain rate is generally higher than the observed rain rate, in particular, in late afternoon of 16 July and early morning of 17 July 2006.

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Precipitation Modeling and Quantitative Analysis by Xiaofan Li, Shouting Gao


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