北半球夏季对流层顶气压与气温的年（代）际变率与趋势分析

朱保林; 管兆勇; 程智

北半球夏季对流层顶气压与气温的年（代）际变率与趋势分析

1.
云南省气象局,云南昆明 650034;2. 南京信息工程大学/江苏省气象灾害重点实验室,江苏南京 210044
2.
南京信息工程大学/江苏省气象灾害重点实验室,江苏南京 210044
3.
安徽省气象局,安徽合肥 230031

计量
- 文章访问数: 1353
- HTML全文浏览量: 0
- PDF下载量: 1804
- 被引次数: 0
出版历程

摘要

摘要: 利用NCEP/NCAR再分析月平均资料，研究了1979—2002年夏季全球对流层顶气压和气温的分布特征与变化趋势。选取了夏季北半球对流层顶年（代）际变率最大区域来定义气压指数和气温指数。分析结果表明：（1）全球对流层顶气压和气温在北半球随纬度的增加而增大，在南半球随纬度先增大再减小，而在整个热带地区对流层顶气压和气温的分布则较为均匀。（2）全球平均的对流层顶气压和气温在分析时段内呈减小趋势，但在中高纬度地区对流层顶气压和气温存在大范围增大现象，表明二者的趋势并不是全球一致的。（3）对流层顶年（代）际变率最大值出现在北半球的中纬度地区和南半球的副热带及高纬度地区，最小值则出现在热带地区。气压指数和气温指数显示出准10年和准3～5年周期。
- 气候学 /
- 年(代)际变率 /
- 小波分析 /
- 趋势 /
- 对流层顶

HTML全文

参考文献(1)

[1]

WMO. Meteorology——A three-dimensional science: Second session of the commission for aerology[J]. WMO Bull, 1957, 4（2）: 134-138.[2] REED R J. A study of a characteristic type of upper level frontogenesis[J]. J Meteorol, 1955, 12（3）: 226-237.[3] HOINKA K P. The tropopause: discovery,definition and demarcation[J]. Meteorol Z, 1997, 6（4）: 281-303.[4] STEINBRECHT W, CLAUDE H, KOHLER U, et al. Correlations between tropopause height and total ozone: Implications for long-term changes[J]. J Geophys Res, 1998, 103（7）: 19 183-19 192.[5] ANGELL J K, KORSHOVER J. Quasi-biennial variations in temperature, total ozone,and tropopause height[J]. J Atmos Sci, 1964, 21（5）: 479-492.[6] ANGELL J K, KORSHOVER J. Quasi-biennial and long-term fluctuations in tropopause pressure and temperature, and the relation to stratospheric water vapor[J]. Mon Wea Rev, 1974, 102（1）: 29-34.[7] REID G C, GAGE K S. Interannual variations in the height of the tropical tropopause[J]. J Geophys Res, 1985, 90（3）: 5 629-5 635. [8] GETTELMAN A, RANDEL W J, MASSIE S, et al. El-Nino as a natural experiment for studying the Tropical Tropopause Region[J]. J Climate, 2001, 14（6）: 3 375-3 392.[9] REID G C, GAGE K S. Troposphere-stratosphere coupling in the tropics: the role of El Nino and the QBO[J]. Chanin, Marie-Lise(ed.). The role of the stratosphere in global change. Heidelberg, Germany, Springer-Verlag, 1993: 245-266.[10] HOINKA K P. Statistics of the global tropopause pressure[J]. Mon Wea Rev, 1998, 126（12）: 3 303-3 325.[11] SANTER B D, WEHNER M F, WIGLEY T M L, et al. Contributions of anthropogenic and natural forcing to recent tropopause height changes[J]. Science, 2003, 301（5632）: 479-483.[12] SEIDEL D J, ROSS R J, ANGELL J K, et al. Climatological characteristics of the tropical tropopause as revealed by radiosondes[J]. J Geophys Res, 2001, 106（D8）: 7 857-7 878.[13] SAUSEN R, SANTER B D. Use of changes in tropopause height to detect human influences on climate[J]. Meteorol Z, 2003, 12(3): 131-136.[14] HIGHWOOD E J, HOSKINS B J. The tropical tropopause[J]. Quart J Roy Meter Soc, 1998, 124（549）: 1 579–1 604.[15] RANDEL W J, WU F, GAFFEN D J. Interannual variability of the tropical tropopause derived from radiosonde data and NCEP reanalyses[J]. J Geophys Res, 2000, 105（D12）: 15 509-15 523.[16] 徐建军，朱乾根. 印度洋-太平洋海温长期变化的周期性及其年代际变化[J]. 热带气象学报，1998，14（4）：353-358.[17] MAXOBEP ЗM著，张贵银, 廖寿发译. 对流层顶气候学（第一版）[M]. 北京：气象出版社，1987.[18] 吴涧，杨茜，符淙斌，等. 全球变暖背景下东亚对流层顶高度演变特征的研究[J]. 热带气象学报，2007，23（6）：595-600.[19] SPRENGER M, MASPOLI M C, WERNLI H. Tropopause folds and cross-tropopause exchange: A global investigation based upon ECMWF analyses for the time period March 2000 to February 2001[J]. J Geophys Res, 2003, 108（D12）, 8518, doi: 10.1029/2002JD002587, STA 3-1-3-11.[20] ELBERN H, HRNDRICKS J, EBEL A. A climatology of tropopause folds by global analyses[J]. Theor Appl Climatol, 1998, 59（2）: 181-200. [21] HIROAKI H, YAMAZAKI K. Interannual variations of temperature and vertical motion at the tropical tropopause associated with ENSO[J]. Geophys Res Latt, 2001, 28（15）: 2 891-2 894.[22] COLE H P. Investigation of a possible relationship between the height of the low-latitude tropopause and the sunspot number[J]. J Atmos Sci, 1975, 32（5）: 998-1 001.[23] STRANZ D. Solar activity and the altitude of the tropopause near the equator[J]. J Atm Terr Pys, 1959, 16（2）: 180-182.

施引文献

资源附件(0)

访问统计