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公颖, 周小珊, 董博. 2018: 辽宁夏季降水时空分布特征及其成因分析. 暴雨灾害, 37(4): 373-382. DOI: 10.3969/j.issn.1004-9045.2018.04.010
引用本文: 公颖, 周小珊, 董博. 2018: 辽宁夏季降水时空分布特征及其成因分析. 暴雨灾害, 37(4): 373-382. DOI: 10.3969/j.issn.1004-9045.2018.04.010
GONG Ying, ZHOU Xiaoshan, Dong Bo. 2018: The characteristic analysis and the research on the mechanism of the summer precipitation in Liaoning province. Torrential Rain and Disasters, 37(4): 373-382. DOI: 10.3969/j.issn.1004-9045.2018.04.010
Citation: GONG Ying, ZHOU Xiaoshan, Dong Bo. 2018: The characteristic analysis and the research on the mechanism of the summer precipitation in Liaoning province. Torrential Rain and Disasters, 37(4): 373-382. DOI: 10.3969/j.issn.1004-9045.2018.04.010

辽宁夏季降水时空分布特征及其成因分析

The characteristic analysis and the research on the mechanism of the summer precipitation in Liaoning province

  • 摘要: 利用国家气象信息中心提供的2008—2013年6—8月中国自动站逐小时降水资料与CMORPH(CPC MORPHing technique)卫星反演降水资料融合生成的逐小时融合降水产品(0.1°网格数据集)和2001—2012年6—8月的NCEP 1°×1°再分析资料,对辽宁省夏季降水时空分布特征及其成因进行了较为深入统计、分析,结果表明:(1)辽宁省平均日降水频率的大值区位于辽东地区,这与该地区位于千山—龙岗山山区和夏季低层盛行偏南风密切相关。(2)辽宁地区平均小时降水率大值区也分布在辽东,辽东南为大值区的中心,主要原因为其一,该地区位于中低层比湿场的湿舌处,其二,该地区夏季中低层盛行的西南风遇千山—龙岗山被迫抬升形成中低层上升速度中心。(3)辽宁省降水日变化特征明显:辽西山区、辽宁西北部、辽东—东南部山区为午后到前半夜降水峰值频发区,而中部平原地区、南部沿海地区为凌晨降水峰值频发区。(4)地理环境决定的局地热力、动力过程和天气系统同时影响日降水峰值发生时间,当天气系统较为稳定的处于发展初期和后期时,其影响区域内降水日变化符合前述规律,但当天气系统明显发展或移动,其影响区域内日降水峰值多数发生在该时刻附近。(5)降水日变化规律与天气类型关系不是很大,即在各类天气系统诱发的降水过程中,由地理环境决定的降水日变化规律均存在。(6)辽宁地区西部山地高原、中部平原、东部山地丘陵、南临海洋的独特地理环境决定的局地热力、动力环流及夜间到凌晨加强的由海到陆的西南风暖湿气流是其降水日变化特征的产生的主要原因。

     

    Abstract: Using long time hourly 0.1°×0.1°resolution merged precipitation products provided by the National Meteorological Information Center of China Meteorological Administration and the NCEP reanalysis data, the characteristics and the causes of summer precipitation in Liaoning province have been analyzed. The results are summarized as follows. (1) The greater averaged daily precipitation frequency in Liaoning province locates in the east, which is closely related to the fact that this area locates in the Qianshan-Longgang mountain region where the southerly wind prevails in middle and low level in summer.(2) The greater average hourly rain rate in Liaoning province also locates in the east. There have two main reasons. Firstly, this area locates in the moist tongue in the middle and low level specific humidity fields. Second, there has a center of ascending velocity there in middle and low levels caused by the southwesterly wind uprising forced by its meeting with Qianshan-Longgang mountain.(3) The diurnal variation characteristics of precipitation in Liaoning province is evident. The diurnal rain peak occurs most frequently from afternoon to midnight in mountain areas and in the northwest, and occurs most frequently in the early morning hours in the central plain and the southern coastal area of Liaoning province.(4) When the synoptic system is at its preliminary stage or at its later stage, the diurnal variation occurs as mentioned above. But, when the synoptic system moves or develops, the local diurnal rain peak often occurs at that moment.(5) The diurnal precipitation variation characteristics seems to be independent of the synoptic type, i.e., it exists in all kinds of rain cases.(6) The local thermodynamic and dynamic cycle, the strengthen nocturnal southwest warm and wet air stream from the sea caused by the individual topography, i.e., mountains and plateaus in the west, plains in the middle, mountains and hills in the east and sea neighbored the south, are the main factors affecting the diurnal rain variation in Liaoning province.

     

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