| 江南雨季地理区域及起止时间的客观确定 |
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| 引用本文： | 詹丰兴,何金海,章毅之,朱志伟.江南雨季地理区域及起止时间的客观确定[J].海洋学报,2015,37(6):1-11. |
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| 作者姓名： | 詹丰兴 何金海 章毅之 朱志伟 |
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| 作者单位： | 1.南京信息工程大学 气象灾害省部共建教育部重点实验室 大气科学学院, 江苏 南京 210044;江西省气象局, 江西 南昌 330046 |
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| 基金项目： | 国家重点基础研究发展计划(973计划)(2013CB430202);长江学者和创新团队发展计划(PCSIRT);公益性行业(气象)科研专项项目(GYHY201406018);江西省科技厅指导性科技计划(2013ZBBG70022);江苏省"青蓝工程"科技创新团队;江苏高校优势学科建设工程资助项目(PAPD)。 |
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| 摘 要： | 本文基于国家气象信息中心整编的全国1 675个台站观测资料以及NCEP/NCAR的再分析资料,定义了候降水指数,利用旋转正交经验函数分解(REOF)法对全国候降水的季节进程进行了诊断分析,得到了表征气候态降水逐候进程的南、北方模态及各自的时间系数,发现REOF第二模态对应降水季节进程中的江南雨季。综合考虑我国南方(31°N以南、110°E以东区域)气候态降水的候进程、降水季节进程(4-6月降水指数减去6-8月降水指数)年际变率以及雨季(4-6月降水指数)降水年际变率的一致性,客观定义了江南雨季的地理范围。利用客观划定区域内的降水指数、925hPa经向风以及西北太平洋副热带高压500hPa脊线位置3个指标,制定了判定江南雨季起止时间的方法,进而对1961-2012年江南雨季起止时间进行了客观确定,给出了江南雨季起止时间序列。本文旨在为规范江南雨季的监测提供参考和借鉴,并为其预测提供科学基础。
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| 关 键 词： | 江南雨季 地理区域客观界定 降水季节进程 起止时间 |
| 收稿时间： | 2015/1/13 0:00:00 |
The objective definition for the geographic region of Jiangnan Rainy Season and its onset and retreat date |
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| Zhan Fengxing,He Jinhai,Zhang Yizhi and Zhu Zhiwei.The objective definition for the geographic region of Jiangnan Rainy Season and its onset and retreat date[J].Acta Oceanologica Sinica (in Chinese),2015,37(6):1-11. |
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| Authors: | Zhan Fengxing He Jinhai Zhang Yizhi and Zhu Zhiwei |
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| Institution: | Key Laboratory of Meteorological Disaster of Ministry of Education(KLME), College of Atmospheric Science, Nanjing University of Information Science and Technology, Nanjing 210044, China;Jiangxi Meteorological Bureau, Nanchang 330046, China,Key Laboratory of Meteorological Disaster of Ministry of Education(KLME), College of Atmospheric Science, Nanjing University of Information Science and Technology, Nanjing 210044, China,Climate Center of Jiangxi Meteorological Bureau, Nanchang 330046, China and Key Laboratory of Meteorological Disaster of Ministry of Education(KLME), College of Atmospheric Science, Nanjing University of Information Science and Technology, Nanjing 210044, China |
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| Abstract: | Using the 1 675 gauge data from National Meteorological Information Center and the NCEP/NCAR reanalysis data, the pentad mean averaged precipitation index which can eliminate the regional differences between gauges is defined. The rotated empirical orthogonal function decomposition (REOF) is applied to investigate the seasonal march of the pentad mean precipitation over the entire China. We obtain two leading modes (e. g. the South and North mode) and their time coefficients. The second mode of REOF presents well the Jiangnan Rainy Season (JRS).Given the consistence of three independent criterion, e.g., the seasonal process of pentad mean precipitation, the interannual variability of precipitation index seasonal variation (April-June mean minus June-August mean) and the interannual variability of mean state of rainy season (April-June) in south of China (south of 31°Nand east of 110°E), the overlap region of these three is objective defined as the geographic region of JRS. Using three variables in the defined geographic region of JRS, e.g., the rainfall index, regional 925 hPa meridional wind and the western North Pacific subtropical high ridge line position at 500 hPa, the onset and retreat dates of JRS from 1961 to 2012 are determined objectively. The purposes of this paper are to provide reference for monitoring JRS and scientific basis for its prediction. |
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| Keywords: | Jiangnan Rainy Season objectively definition of geographic region rainfall seasonal march the onset and retreat date |
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