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我国江南夏季极端高温季节内变化特征初探
引用本文:高庆九,尤琦.我国江南夏季极端高温季节内变化特征初探[J].长江流域资源与环境,2019,28(7):1682-1690.
作者姓名:高庆九  尤琦
作者单位:南京信息工程大学气象灾害教育部重点实验室/气候与环境变化国际合作联合实验室/气象灾害预报预警与评估协同创新中心/大气科学学院气候动力学研究中心,江苏南京,210044;南京信息工程大学气象灾害教育部重点实验室/气候与环境变化国际合作联合实验室/气象灾害预报预警与评估协同创新中心/大气科学学院气候动力学研究中心,江苏南京,210044
基金项目:国家重点研发计划;国家自然科学基金
摘    要:利用1979~2013年逐日最高温度观测资料,通过Butterworth带通滤波和功率谱分析等方法,分析我国江南夏季极端高温季节内变化特征。结果表明:7月中旬至8月中旬,江南地区(110°E ~125°E,22.5°N~30°N)为高温日数高值区,高温日数存在季节内振荡信号。功率谱结果表明该地区日最高温度呈现出10~25 d的季节内振荡周期;在以10~15 d和20~25 d周期为主的低频变化典型年份(1989和1993年)中,影响系统与副热带高压并无直接联系,对流层中高层45°N存在2~3波的纬向波列,该波列的移动与传播可能与温度的低频变化有关。

关 键 词:极端高温  季节内变化  纬向波列

Preliminary Analysis of Intraseasonal Oscillation of Summer Extreme Daily Temperature in China
GAO Qing-jiu,YOU Qi.Preliminary Analysis of Intraseasonal Oscillation of Summer Extreme Daily Temperature in China[J].Resources and Environment in the Yangtza Basin,2019,28(7):1682-1690.
Authors:GAO Qing-jiu  YOU Qi
Institution:(Key Laboratory of Meteorological Disaster, Ministry of Education(KLME)/Joint International Research Laboratory of Climate and Environment Change(ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD)/Climate Dynamics Research Center(CDRC) of the College of Atmospheric Sciences, Nanjing University of Information Science & Technology, Nanjing 210044,China);
Abstract:Based on the daily observation data during 1979-2013, the characteristics of internal oscillation in summer extreme high temperature in southern of the Yangtze river were further discussed. By using Butterworth filter and power spectrum methods, results show that: From the middle of July to the middle of August, the high value center moves into southern of the Yangtze river(110°-125°E,22.5°N-30°N) and averaged hot days beyond 95% threshold show oscillation feature. Result of Power spectrum indicates daily maximum temperature presents the characteristics of intraseasonal variation in 10-25d. The impact system is not directly related to the subtropical high in the typical low frequency year(1989 and 1993). On the middle and high troposphere, the geopotential height presents 2 to 3 waves with the obvious intraseasonal oscillation features(10-15 day and 20-25day). The motion and propagation of the wave may be related to the low frequency variation of temperature.
Keywords:
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