THE EXTRATROPICAL UPPER TROPOSPHERE AND LOWER STRATOSPHERE

被引:276
作者
Gettelman, A. [1 ]
Hoor, P. [4 ]
Pan, L. L. [1 ]
Randel, W. J. [1 ]
Hegglin, M. I. [3 ]
Birner, T. [2 ]
机构
[1] Natl Ctr Atmospher Res, Boulder, CO 80304 USA
[2] Colorado State Univ, Dept Atmospher Sci, Ft Collins, CO 80523 USA
[3] Univ Toronto, Dept Phys, Toronto, ON M5S 1A7, Canada
[4] Johannes Gutenberg Univ Mainz, Inst Atmospher Phys, D-55099 Mainz, Germany
基金
英国自然环境研究理事会; 美国国家科学基金会;
关键词
TROPOPAUSE INVERSION LAYER; BREWER-DOBSON CIRCULATION; SUBTROPICAL LOWER STRATOSPHERE; POTENTIAL VORTICITY STREAMERS; TROPICAL UPPER TROPOSPHERE; IN-SITU MEASUREMENTS; LOCAL MIXING EVENTS; WATER-VAPOR; NORTHERN-HEMISPHERE; LARGE-SCALE;
D O I
10.1029/2011RG000355
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The extratropical upper troposphere and lower stratosphere (Ex-UTLS) is a transition region between the stratosphere and the troposphere. The Ex-UTLS includes the tropopause, a strong static stability gradient and dynamic barrier to transport. The barrier is reflected in tracer profiles. This region exhibits complex dynamical, radiative, and chemical characteristics that place stringent spatial and temporal requirements on observing and modeling systems. The Ex-UTLS couples the stratosphere to the troposphere through chemical constituent transport (of, e. g., ozone), by dynamically linking the stratospheric circulation with tropospheric wave patterns, and via radiative processes tied to optically thick clouds and clear-sky gradients of radiatively active gases. A comprehensive picture of the Ex-UTLS is presented that brings together different definitions of the tropopause, focusing on observed dynamical and chemical structure and their coupling. This integral view recognizes that thermal gradients and dynamic barriers are necessarily linked, that these barriers inhibit mixing and give rise to specific trace gas distributions, and that there are radiative feed-backs that help maintain this structure. The impacts of 21st century anthropogenic changes to the atmosphere due to ozone recovery and climate change will be felt in the Ex-UTLS, and recent simulations of these effects are summarized and placed in context.
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页数:31
相关论文
共 253 条
  • [1] Ambaum M, 1997, J ATMOS SCI, V54, P555, DOI 10.1175/1520-0469(1997)054<0555:IFOTT>2.0.CO
  • [2] 2
  • [3] [Anonymous], 2010, Scientific Assessment of Ozone Depletion: 2010
  • [4] [Anonymous], 2003, 47 WMO
  • [5] Fragmentation of stratospheric intrusions
    Appenzeller, C
    Davies, HC
    Norton, WA
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D1) : 1435 - 1456
  • [6] Seasonal variation of mass transport across the tropopause
    Appenzeller, C
    Holton, JR
    Rosenlof, KH
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 1996, 101 (D10) : 15071 - 15078
  • [7] Assmann R., 1902, Sitzungsber. K. Preuss. Akad. Wiss, V24, P495
  • [8] SOME FEATURES OF THE STRUCTURE OF THE TROPICAL TROPOPAUSE
    ATTICKS, MG
    ROBINSON, GD
    [J]. QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 1983, 109 (460) : 295 - 308
  • [9] Stratospheric harbingers of anomalous weather regimes
    Baldwin, MP
    Dunkerton, TJ
    [J]. SCIENCE, 2001, 294 (5542) : 581 - 584
  • [10] Atmospheric Chemistry Experiment (ACE):: Mission overview -: art. no. L15S01
    Bernath, PF
    McElroy, CT
    Abrams, MC
    Boone, CD
    Butler, M
    Camy-Peyret, C
    Carleer, M
    Clerbaux, C
    Coheur, PF
    Colin, R
    DeCola, P
    Bernath, PF
    McElroy, CT
    Abrams, MC
    Boone, CD
    Butler, M
    Camy-Peyret, C
    Carleer, M
    Clerbaux, C
    Coheur, PF
    Colin, R
    DeCola, P
    DeMazière, M
    Drummond, JR
    Dufour, D
    Evans, WFJ
    Fast, H
    Fussen, D
    Gilbert, K
    Jennings, DE
    Llewellyn, EJ
    Lowe, RP
    Mahieu, E
    McConnell, JC
    McHugh, M
    McLeod, SD
    Michaud, R
    Midwinter, C
    Nassar, R
    Nichitiu, F
    Nowlan, C
    Rinsland, CP
    Rochon, YJ
    Rowlands, N
    Semeniuk, K
    Simon, P
    Skelton, R
    Sloan, JJ
    Soucy, MA
    Strong, K
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2005, 32 (15)