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大范围持续性强降水过程与30~60 d低频降水的联系及其预报指数

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研究低频振荡是目前开展强降水过程延伸期预报的有效途径.利用1981-2010年中国753站逐日的降水观测资料、NCEP/NCAR第二套再分析资料及实况天气图等资料,分析大范围持续性强降水过程与30~60 d低频降水的联系,并根据前期低频信号构造强降水过程预报指数.研究表明,(1)大范围持续性强降水过程与低频降水紧密相联,低频降水对强降水过程有显著贡献.在30~60 d低频降水显著年,强降水过程均发生在低频降水峰值阶段;但对于低频降水而言,仅有56%的峰值阶段发生强降水过程.(2)当低频降水峰值阶段发生强降水过程时,来自东北亚和南海的低频位势高度低值系统在长江中下游汇合, “南北高、中间低”的低频位势高度分布有利于低频气流强烈辐合,并在经向上形成两个完整的反向低频垂直环流圈,促进了上升运动发展,导致强降水过程发生;而对于低频降水峰值未发生强降水过程的情况,北方冷空气南下较弱,高纬度低频影响系统位置偏北,长江中下游附近表现为“南高北低”的低频位势高度分布和单圈垂直环流,不利于低频气流强烈辐合.(3)综合高、中、低纬的前期低频信号构造了强降水过程预报指数,对延伸期(10~25 d)长江中下游大范围强降水过程预报具有参考价值.
THE RELATIONSHIP BETWEEN LARGE-SCALE PERSISTENT HEAVY RAINFALL PROCESSES AND 30-60 DAY LOW-FREQUENCY RAINFALL AND ITS FORECASTING INDEX
Low-frequency oscillation has been employed effectively to develop extended range forecast.Using daily observed precipitation data from 753 stations of China from 1981 to 2010,NCEP/NCAR daily reanalysis data and real-time weather maps,we analyzed the relationship between large-scale persistent heavy rainfall processes and 30 ~ 60 d low-frequency rainfall.A Heavy rainfall process index (HRPI) is also constructed based on the precedent low-frequency signal.The results have the following suggestions:(1) The heavy rainfall process (HRP) has close relationship with 30 ~ 60 d low-frequency rainfall,which contributes greatly to the HRP.In the years of significant 30 ~ 60 d oscillation low-frequency rainfall,HRP all occurs at their peak stages but only 56% of the peak stages have HRP.(2) When HRP happened at the peak stage of low-frequency rainfall,low-value areas of low-frequency geopotential height from northeast Asia and South China Sea converge in the middle-lower reaches of the Yangtze River so that the distribution of low-frequency geopotential height being higher in the north and south than in the middle is in favor of severe low-frequency air convergence,formation of two reversed low-frequency vertical circulation,and development of upward movement,thus causing HRP.When the peak stage of low-frequency rainfall is not with HRP,cold air from the north is relatively weak,low-frequency systems at high latitudes are abnormally northward.The middle-lower reaches of the Yangtze River are characterized by the distribution of low-frequency geopotential height being higher in the south than in the north and having one single vertical circulation cell,which is not good for low-frequency air convergence.(3) HRPI is constructed based on precedent low-frequency signals from high,middle and low latitudes,which has value of guidance for the extend-period forecasting of heavy rainfall processes in the middle-lower reaches of the Yangtze River.

heavy rainfall process30 ~ 60 daylow-frequency oscillationforecasting indexmiddle-lower reaches of the Yangtze River

魏晓雯、梁萍、何金海、穆海振

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南京信息工程大学,江苏南京210044

上海市气候中心,上海200030

强降水过程 30~60d 低频振荡 预报指数 长江中下游

国家自然科学基金资助项目公益性行业(气象)科研专项

41205060GYHY201306030

2015

热带气象学报
中国气象局广州热带海洋气象研究所

热带气象学报

CSTPCDCSCD北大核心
影响因子:0.768
ISSN:1004-4965
年,卷(期):2015.31(1)
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