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长江下游地区不同边界层参数化方案的试验研究

徐慧燕 朱业 刘瑞 沈杭锋 王东海 翟国庆

大气科学2013,Vol.37Issue(1):149-159,11.
大气科学2013,Vol.37Issue(1):149-159,11.DOI:10.3878/j.issn.1006-9895.2012.12021

长江下游地区不同边界层参数化方案的试验研究

Simulation Experiments with Different Planetary Boundary Layer Schemes in the Lower Reaches of the Yangtze River

徐慧燕 1朱业 2刘瑞 1沈杭锋 3王东海 1翟国庆1

作者信息

  • 1. 浙江大学地球科学系,杭州310027
  • 2. 中国气象科学研究院灾害天气国家重点实验室,北京 100081
  • 3. 浙江省海洋监测预报中心,杭州310007
  • 折叠

摘要

Abstract

By using several planetary boundary layer schemes (Mellor-Yamada-Janjic; quasi-normal scale elimination; Yonsei University; asymmetric convective, version 2; Bougeault-Lacarrere (Boulac); Mellor-Yamada-Nakanishi- Niino, level 2.5; and Mellor-Yamada-Nakanishi-Niino, level 3) in a Weather Research and Forecasting (WRF) numerical model, seven sets of model simulations for three rainstorm cases in the lower reaches of the Yangtze River were performed. This paper thoroughly analyzes and compares the simulation ability of seven planetary boundary layer parameterizations with respect to the distribution of 24-hour total rainfall, boundary layer structure in the rainstorm area, fundamental fields of meteorological elements, and statistical test results for total rainfall. A comparison of the simulations and the observations indicated that the quasi-normal scale elimination planetary boundary layer scheme is superior to the other six.

关键词

边界层参数化方案/WRF模式/降水/Ts评分

Key words

Planetary boundary layer parameterizations/ WRF model/ Precipitation/ TS verification

分类

天文与地球科学

引用本文复制引用

徐慧燕,朱业,刘瑞,沈杭锋,王东海,翟国庆..长江下游地区不同边界层参数化方案的试验研究[J].大气科学,2013,37(1):149-159,11.

基金项目

国家自然科学基金资助项目41175047,国家公益性行业科研专项GYHY201006014、GYHY201006007 ()

大气科学

OA北大核心CSCDCSTPCD

1006-9895

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