Diurnal Variation of Tropical Cyclone Rainfall in the Western North Pacific in 2008–2010

Diurnal Variation of Tropical Cyclone Rainfall in the Western North Pacific in 2008–2010
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2008—2010年西北太平洋热带气旋降雨量日变化

DOI:
10.1080/16742834.2013.11447064
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发表时间:
2013-01
影响因子:
2.3
通讯作者:
Bin XU
Bin XU
中科院分区:
地球科学4区
文献类型:
--
作者:
Shu Hailong;Qinghong Zhang;Bin XU

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利用美国国家海洋和大气管理局(NOAA)高分辨率气候预测中心的变形技术(CMORPH)产品,对北太平洋西部热带气旋(TC)降水的日变化进行了研究。2008年1月至2010年10月,联合台风预警中心共录得72个热带气旋及389个热带气旋降雨日数。利用客观天气分析技术(OSAT)对TC雨率进行了划分,并插值到当地标准时间(LST)中。采用谐波分析分析降水的日变化。近70%的TC降雨日数存在明显的日循环。
Abstract Diurnal variation of tropical cyclone (TC) rainfall in the western North Pacific (WNP) is investigated using the high-resolution Climate Prediction Center's morphing technique (CMORPH) products obtained from the National Oceanic and Atmospheric Administration (NOAA). From January 2008 to October 2010, 72 TCs and 389 TC rainfall days were reported by the Joint Typhoon Warning Center's (JTWC) best-track record. The TC rain rate was partitioned using the Objective Synoptic Analysis Technique (OSAT) and interpolated into Local Standard Time (LST). Harmonic analysis was applied to analyze the diurnal variation of the precipitation. Obvious diurnal cycles were seen in approximately 70% of the TC rainfall days.
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