S2S模式对2023年夏季华北极端高温的次季节预测技巧及其可预报性来源OA
Subseasonal prediction skills of ECMWF and CMA S2S models for the extreme high-temperature event over North China in summer 2023 and the sources of predictability
2023年 6-7月,华北地区经历破纪录的极端高温事件,多个气象站气温突破 40℃,这次高温事件存在 6月 14-18日(P1)、21-25日(P2)和 6月 30日—7月 3日(P3)3次相对独立过程.本研究基于次季节至季节预报(S2S)计划中 ECMWF和CMA回报数据,通过对局地温度诊断方程、地表能量方程和大尺度环流的诊断分析,评估 ECMWF和 CMA动力模式对 2023年华北 3次极端高温过程空间分布和强度的预测能力,并揭示模式预测误差来源以及极端高温的可预报性来源.结果表明:(1)ECMWF和 CMA对 P1、P2和 P3的地表气温(SAT)异常的预测时效分别为 10-11、12-14及 3-6 d,均低估了 SAT异常的强度,尤其是 P3时期;(2)P1、P2(P3)超过 15(5)d时效后,模式难以捕捉欧亚大陆中高纬度罗斯贝波列,造成华北局地高压异常位置以及强度的预测偏差;(3)模式对华北局地高压异常的预测偏差进一步影响了其对局地物理过程和地表气温异常的预测准确度.模式对 P1、P3过程中局地短波辐射以及长波辐射的低估,导致以非绝热加热项为主要贡献的温度局地变化呈现负偏差;而模式低估了 P2过程中做主要贡献的绝热加热,导致 SAT也被低估.本研究强调了中高纬度次季节大气遥相关波列是华北次季节极端高温的重要可预报性来源,模式对其的捕捉能力是进一步提升华北高温预测水平的关键.
During June—July 2023,North China(NC)experienced a record-breaking Extreme High Temperature(EHT)event with temperatures exceeding 40℃at many meteorological stations.This event consisted of three relatively distinct processes,occurring during 14-18 June(P1),21-25 June(P2),and 30 June—3 July(P3),respectively.Using hindcast data from the European Centre for Medium-Range Weather Forecasts(ECMWF)and the China Meteorological Administration(CMA)within the Subseasonal-to-Seasonal(S2S)Prediction Project and diagnostic analysis of the local temperature budget,surface energy budget,and large-scale atmospheric circulation,this study evaluates the performance of ECMWF and CMA dynamic models in forecasting the spatial distribution and intensity of the three EHT processes,and further reveals the sources of forecast errors and predictability.The results indicate that:(1)ECMWF and CMA models can predict the spatial distribution of Surface Air Temperature(SAT)anomalies over NC for P1,P2 and P3 with lead time of 10-11,12-14,and 3-6 d,respectively.However,both models underestimate the amplitude of SAT anomalies,especially during P3;(2)when the forecast lead time exceeds 15 d for P1 and P2,and 5 d for P3,both models fail to capture features of the mid-to high-latitude Rossby wave train over Eurasia,resulting in prediction biases in both the location and intensity of localized high-pressure anomalies over NC;(3)prediction biases of the localized high-pressure anomalies over NC further induce biases in the forecast of local physical processes and SAT anomalies.During P1 and P3,the models'underestimation of both shortwave and longwave radiation leads to local negative temperature tendency biases,with diabatic heating being the primary contributor.In contrast,during P2,the underestimation of adiabatic heating is primarily responsible for the cold bias in predicted SAT.This study highlights the mid-to high-latitude subseasonal Rossby wave train teleconnection as a critical source of predictability for subseasonal EHT in NC,suggesting that better representation of this wave pattern is a key to improve EHT prediction skills over NC.
袁可芯;李娟;黄红洁;胡娅敏;朱志伟
南京信息工程大学气候系统预测与变化应对全国重点实验室/气象灾害教育部重点实验室/气象灾害预报预警与评估协同创新中心,南京,210044||南京信息工程大学大气科学学院,南京,210044||苏州市环境监测站,苏州,215011南京信息工程大学气候系统预测与变化应对全国重点实验室/气象灾害教育部重点实验室/气象灾害预报预警与评估协同创新中心,南京,210044||南京信息工程大学大气科学学院,南京,210044南京信息工程大学气候系统预测与变化应对全国重点实验室/气象灾害教育部重点实验室/气象灾害预报预警与评估协同创新中心,南京,210044||南京信息工程大学大气科学学院,南京,210044广东省气候中心,广州,510640南京信息工程大学气候系统预测与变化应对全国重点实验室/气象灾害教育部重点实验室/气象灾害预报预警与评估协同创新中心,南京,210044||南京信息工程大学大气科学学院,南京,210044
天文与地球科学
华北极端高温次季节预测中高纬度罗斯贝波列
Extreme high temperature over North ChinaSubseasonal predictionMid-to high-latitude Rossby wave train
《气象学报》 2026 (4)
678-693,16
国家自然科学基金气象联合基金项目(U2342208)、甘肃省自然科学基金项目(24JRRA720).
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