首页 | 本学科首页   官方微博 | 高级检索  
     检索      

北半球500 hPa位势高度场时空频谱特征分析
引用本文:孙诚,李建平.北半球500 hPa位势高度场时空频谱特征分析[J].大气科学,2011,35(6):1079-1090.
作者姓名:孙诚  李建平
作者单位:1.中国科学院大气物理研究所大气科学和流体力学数值模拟国家重点实验室, 北京 100029;中国科学院研究生院, 北京 100049
基金项目:国家重点基础研究发展计划2010CB950400, 国家自然科学基金资助项目41030961、40821092
摘    要:利用1979~2004年NCEP2再分析资料,对逐日的北半球(20°N~90°N) 500 hPa的位势高度进行二维傅里叶的谱展开,并分析了不同波数下的谱展开系数的频域特征.对全年序列分析的结果表明:当纬向波数k和经向波数l均为0时,其谱展开系数表现为显著的低频(10~30天)变化特征;当经向波数l=0时,其谱展开系数...

关 键 词:二维傅里叶分解  标准化功率谱  频散关系  位势高度  经向偶极子

Spatial-Temporal Spectral Analysis of the Northern Hemisphere 500-hPa Geopotential Height
SUN Cheng and LI Jianping.Spatial-Temporal Spectral Analysis of the Northern Hemisphere 500-hPa Geopotential Height[J].Chinese Journal of Atmospheric Sciences,2011,35(6):1079-1090.
Authors:SUN Cheng and LI Jianping
Institution:1.State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029;Graduate University of Chinese Academy of Sciences, Beijing 1000492.State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029
Abstract:Using NCEP2 reanalysis data from 1979 to 2004, the daily 500-hPa geopotential height in the Northern Hemisphere (20°N-90°N) has been expanded into double Fourier series and the signals in the frequency domain have been analyzed for different spatial scales. For the daily series in the entire year, when both the zonal wave number k and the meridional wave number l equal zero, the signals series are characterized by a significant low-frequency variation (10-30 days). When the meridional wave number l equals zero, the signals in the frequency domains vary with the zonal wave number k significantly. The coefficient series consist of a low-frequency variation at larger spatial scales and a high-frequency variation (4-8 days) at smaller spatial scales. When the zonal wave number k equals zero, the signals in the frequency domains vary little with the meridional wave number l. The coefficient series are characterized by a low-frequency variation. When both k and l are not equal to zero, the spatial scales of low-frequency variations mainly concentrate on l=1, corresponding to the dipole structure of low-frequency flows in the mid-high latitudes. The results for daily series during the winter or summer half year are similar to those during the entire year. The diagnosis results can be explained, to a certain extent, by the dispersion relation for the Rossby wave.
Keywords:double Fourier expansion  standardized power spectrum  dispersion relation  geopotential height  meridional dipole structure
本文献已被 CNKI 万方数据 等数据库收录!
点击此处可从《大气科学》浏览原始摘要信息
点击此处可从《大气科学》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号