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中国降水对热带太平洋海温的滞后响应特征探讨

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研究热带太平洋海温与中国降水之间的关系对提升我国气候预测水平具有重要科学意义.基于长时间序列的中国160站逐月降水资料和美国气候预测中心(Climate Prediction Center,CPC)的逐月海温指数,采用一种新的滞后累积相关分析方法,研究中国降水对热带太平洋海温的滞后响应特征.结果表明:(1)该分析方法能够有效揭示前期海温异常累积效应对降水的影响,进而为筛选最优预测因子提供依据;(2)在Niño1+2、Niño3、Niño4和Niño3.4等海温指数中,前期Niño1+2指数与中国降水的相关性最显著,尤其是Niño1+2海温序列与滞后4个月的中国降水呈现最显著正相关,而Niño1+2累积2个月海温序列与滞后9个月的中国降水呈最显著负相关;(3)Niño1+2海温序列对中国季风区降水影响明显,其正反馈区主要集中在青藏高原东部和云南地区;(4)Niño1+2海温序列与滞后4个月的中国平均降水量的线性拟合分析显示,拟合得到的降水量变化趋势与实测降水量一致,冬春季拟合误差较小,夏秋季拟合误差较大.
Exploration of the hysteresis response characteristics of precipitation in China to tropical Pacific sea surface temperature
Examine the relationship between tropical Pacific sea surface temperature(SST)and precipitation in China has scientific significance for improving China's climate prediction level.Based on the long-term monthly rain gauge data of 160 stations in China and the monthly SST index from Climate Prediction Center(CPC),USA,this paper explores the response characteristics of precipitation in China to tropical Pacific SST changes through a new method of lag cumulative correlation.The results are as follows:(1)This method is able to reveal the cumulative effect of previous abnormal SST on the precipitation effectively,so as to provide a basis for selecting the optimal predictive factors.(2)Among Niño1+2,Niño3,Niño4,and Niño3.4 SST indices,previous Nino1+2 index has the most signifi-cant relationship with China's precipitation.More precisely,the positive correlation between Niño1+2 timeseries and the 4-month lagged precipitation,and the negative link between 2-month cumulative Niño1+2 time series and the the 9-month lagged precipitation in China are most significant.(3)The Niño1+2 SST can distinctly influence the precipitation in China's monsoon regions,with the stron-gest positive feedback are as primarily locate in the eastern part of the Qinghai-Tibet Plateau and Yunnan Province.(4)The linear fit-ting between the Niño1+2 time series and the average precipitation of China with a lag of 4 months shows that the fluctuation trend of fitted precipitation is consistent with that of the rain gauge data,with relative small fitting errors in winter and spring and larger errors in summer and autumn.

precipitation in Chinatropical Pacific SSTlag cumulative correlation coefficient

高志伟、刘佳、陈艳、钟爱华

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大理国家气候观象台,云南 大理 671000

中国气象局横断山区(低纬高原)灾害性天气研究中心,云南 昆明 650034

云南省红河州气象局,云南 蒙自 661199

云南省气象科学研究所,云南 昆明 650034

云南省大理白族自治州气象局,云南 大理 671000

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中国降水 热带太平洋海温 滞后累积相关系数

云南省科技厅重点研发专项国家自然科学基金项目云南省气象局高原湖泊生态气象服务创新团队项目中国气象科学研究院基本科研业务费专项基金项目

202203AC100006419650052022CX082023Z010

2024

干旱气象
中国气象局兰州干旱气象研究所 中国气象学会干旱气象学委员会

干旱气象

CSTPCD
影响因子:1.9
ISSN:1006-7639
年,卷(期):2024.42(2)
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