首页|热带印-太海温与海河流域夏季降水的联合模态及降水预测应用

热带印-太海温与海河流域夏季降水的联合模态及降水预测应用

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利用1961-2020年中国站点观测降水资料和英国Hadley中心海表面温度资料,针对海河流域夏季降水预测困难的问题,通过多变量经验正交分解(MVEOF)方法的正、反向应用,分析了热带印度洋-太平洋前期海温变化与海河流域夏季降水异常年际变化的联合模态特征,据此建立了海河流域夏季降水的客观统计预测模型并检验预测效果.结果表明:(1)前期ENSO事件和热带印度洋(TIO)海温季节演变与海河流域夏季降水异常分布型关系密切.若前冬El Niño事件达到鼎盛,春季开始衰减,并引起TIO海盆尺度滞后增暖,则当年夏季海河流域降水一致性偏多,偏多中心在流域北部;若前秋El Nino向La Nina事件转变,随后TIO暖海温转冷,则夏季海河流域降水易出现西部偏多、东部偏少型分布;此外,如果前期出现太平洋经向模态(冷舌模态)的海温异常分布时,夏季流域降水异常为西北多、东南少(南多北少).(2)根据联合模态统计关系建立的预测模型,对2013-2020年海河流域夏季降水有较好的预测能力.与实况相比,模型对全域降水异常预测的时间相关系数为0.86、趋势预测准确率为87.50%,对站点的趋势预测准确率为51.35%~70.27%,对旱涝程度预测的平均偏差仅为45.92%,但对降水异常空间分布的预测技巧整体较低.本文阐明了前期热带印-太海温与海河流域夏季降水异常的统计关系,并建立了海河流域夏季降水的客观统计预测模型,为我国华北地区短期气候预测提供了一种新的有效参考.
Co-variation modes of tropical Indo-Pacific SST and summer precipitation anomaly in the Haihe River basin and its application on precipitation prediction
The prediction skill of the state-of-the-art dynamic models on the Haihe River basin(HRB)summer rainfall is still limited,leaving challenges in developing statistical prediction methods.This study used observed precipitation dataset in stations and the sea surface temperature(SST)dataset of Hadley Center in the UK during 1961-2020,analyzed the interannual dominant co-variation modes of early stage SST anomalies in the tropical Indo-Pacific Ocean and the summer precipitation anomaly in the HRB,and constructed an objective precipitation prediction model by the multi-variable empirical orthogonal function(MVEOF)method.Main conclusions are as follows:(1)Previous evolution of ENSO event and tropical Indian Ocean(TIO)SST is well correlated with summer precipitation pattern over the HRB:(a)If an El Nino event reached its peak in the previous winter,began to attenuate in spring,and caused the lagged warming response in the TIO,the above normal summer precipitation in the HRB was observed,whose center was located in the north;(b)When an El Nino was converted to La Nina event in the previous autumn,with a transformation of the SST anomaly in the TIO,the summer precipitation in the HRB tended to appear"wet-west and dry-east"pattern;(c)While the Pacific meridional mode(Cold tongue mode)over the tropical Pacific in the early stages is accompanied by"wet-northwest and dry-southeast"("wet-south and dry-north")pattern in the basin.(2)The prediction model can well predict the summer precipitation in the HRB during 2013-2020,with high temporal correlation coefficient,anomaly symbol skill and wet/dry deviation skill.But its spatial prediction skill is still limited.In conclusion,this paper clarifies the statistical relationship between the seasonal evolution of SST anomalies in the tropical Indo-Pacific Ocean and the spatial distribution of summer precipitation anomaly in the HRB,and constructs an objective statistical prediction model which provides a new and effective method for short-term climate prediction in North China.

Haihe River basinSummer precipitationObjective prediction methodTropical Indo-Pacific SSTA

郝钰茜、郝立生、何丽烨、程善俊

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天津市海洋气象重点实验室,天津 300074

天津市气候中心,天津 300074

海河流域 夏季降水 客观预测方法 热带印-太海温异常

中国气象局创新发展专项天津市气象局科研项目

CXFZ2022J017202324ybxm16

2024

地球物理学报
中国地球物理学会 中国科学院地质与地球物理研究所

地球物理学报

CSTPCD北大核心
影响因子:3.703
ISSN:0001-5733
年,卷(期):2024.67(6)
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