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6 期 杜梦莹等:亚洲季风区内北半球秋季哈德莱环流特征及其与热带海温之间关系 1407
的影响更大。这些研究结果需要数值模拟的进一 surrounding regions[J]. Meteorology and Atmospheric Physics,
步验证。此外,不同类型的 ENSO 事件会影响不同 129:229-246. DOI:10. 1007/s00703-016-0477-6.
Frierson D M,Lu J,Chen G,2007. Width of the Hadley cell in sim‐
的 SST 分布,进而带来不同的大气环流(Larkin and
ple and comprehensive general circulation models[J]. Atmospher‐
Harrison,2005;Weng et al,2007)。那么下一步还
ic Science,34(18):L18804. DOI:10. 1029/2007GL031115.
需结合数值模拟等方法,对不同类型的 ENSO 事件 Fu Q,Johanson C M,Wallace J M,et al,2006. Enhanced mid-lati‐
期间下区域 HC 的异常变化,以及它所带来的天气 tude tropospheric warming in satellite measurements[J]. Sci‐
气候效应进行研究和验证。 ence,312(5777):1179. DOI:10. 1126/science. 1125566.
Gong X P,Wang Q,Liu Y L,2015. Interannual variability of the
参考文献: Hadley circulation associated with tropical Pacific SST anomaly
[J]. Journal of Ocean University of China,14(4):596-603.
Bjerknes J,1966. A possible response of the atmospheric Hadley circu‐
DOI:10. 1007/s11802-015-2465-8.
lation to equatorial anomalies of ocean temperature[J]. Tellus A:
Guo Y P,Li J P,2016. Impact of ENSO events on the interannual
Dynamic Meteorology Oceanography,18(4):820-829. DOI:
variability of Hadley circulation extents in boreal winter[J]. Ad‐
10. 1111/j. 2153-3490. 1966. tb00303. x.
vance in Climate Change Research,7:46-53. DOI:10. 1016/j.
Chen S F,Wei K,Chen W,et al,2014. Regional changes in the an‐
accre. 2016. 05. 001.
nual mean Hadley circulation in recent decades[J]. Journal of
Guo Y P,LI J P,Feng J,et al,2016. The multidecadal variability of
Geophysical Research:Atmospheres,119(13):7815-7832.
the asymmetric mode of the boreal autumn Hadley circulation and
DOI:10. 1002/2014JD021540.
its link to the Atlantic multidecadal oscillation[J]. Journal of Cli‐
Chikamoto Y,Tanimoto Y,Mukougawa H,et al,2010. Subtropical
mate,29(15):5625-5641. DOI:10. 1175/JCLI-D-15-0025. 1.
Pacific SST variability related to the local Hadley Circulation dur‐
Guo Y P,Tan Z M,2018. Impacts of the boreal spring Indo-Pacific
ing the premature stage of ENSO[J]. Journal of the Meteorologi‐
warm pool Hadley circulation on tropical cyclone activity over
cal Society of Japan,88(2):183-202. DOI:10. 2151/jm‐
the western north Pacific[J]. Journal of Climate,31(4):1361-
sj. 2010-205.
1375. DOI:10. 1175/JCLI-D-17-0422. 1.
Diaz H F,Bradley R S,2004. The Hadley circulation:Present,past
Hadley G,1735. VI. Concerning the cause of the general trade-winds
and future[M]. Advances in Global Change Research. DOI:10.
[J]. Philosophical Transactions of the Royal Society of London,
1007/978-1-4020-2944-8.
39:58-62. DOI:10. 1098/rstl. 1735. 0014.
Feng J,Li J P,Jin F F,et al,2016. Contrasting responses of the Had‐
Han W Q,Meehl G A,Rajagppalan B,et al,2010. Patterns of Indian
ley circulation to equatorially asymmetric and symmetric meridio‐
Ocean sea-level change in a warming climate[J]. Nature Geosci‐
nal sea surface temperature structures[J]. Journal of Climate,29
ence,3:546-550. DOI:10. 1038/ngeo901.
(24):8949-8963. DOI:10. 1175/JCLI-D-16-0171. 1.
Haylock M,Mcbride J,2001. Spatial coherence and predictability of
Feng J,Li J P,2013. Contrasting impacts of two types of ENSO on
the Boreal Spring Hadley circulation[J]. Journal of Climate,26 Indonesian wet season rainfall[J]. Journal of Climate,14(18):
(13):4773-4789. DOI:10. 1175/JCLI-D-12-00298. 1. 3882-3887. DOI: 10. 1175/1520-0442 (2001) 014<3882:
SCAPOI>2. 0. CO;2.
Feng J,Li J P,Jin F F,et al,2019. Effect of El Niño on the response
ratio of Hadley circulation to different SST meridional structures Held I M,Hou A Y,1980. Nonlinear axially symmetric circulations in
[J]. Climate Dynamics,53:3877-3891. DOI:10. 1007/s00382- a nearly inviscid atmosphere[J]. Journal of the Atmospheric Sci‐
019-04756-7. ences,37(3):515-533. DOI:10. 1175/1520-0469(1980)037<
Feng J,Li J P,Wang Y Q,et al,2017. Decreased response contrast 0515:NASCIA>2. 0. CO;2.
of Hadley circulation to the equatorially asymmetric and symmet‐ Hou A Y,1998. Hadley circulation as a modulator of the extratropical
ric tropical SST structures during the recent hiatus[J]. Scientific climate[J]. Journal of the Atmospheric Sciences,55(14):2437-
Online Letters on the Atmosphere,13:181-185. DOI:10. 2151/ 2457. DOI:10. 1175/1520-0469(1998)055<2437:HCAAMO>
sola. 2017-033. 2. 0. CO;2.
Feng J,Li J P,Xie F,2013. Long-term variation of the principal Hou A Y,Lindzen R S,1992. The influence of concentrated heating
mode of boreal spring Hadley circulation linked to SST over the on the Hadley circulation[J]. Journal of Atmospheric Sciences,
Indo-Pacific warm pool[J]. Journal of Climate,26(2):532- 49(14):1233-1241. DOI:10. 1175/1520-0469(1992)049<
544. DOI:10. 2307/26192162. 1233:TIOCHO>2. 0. CO;2.
Feng R,Li J P,Wang J C,2011. Regime change of the boreal sum‐ Hu D Z,Guo,Y P,Tan Z M,et al,2019. Interannual relationship be‐
mer Hadley circulation and its connection with the tropical SST tween the boreal Arctic Oscillation and the northern hemisphere
[J]. Journal of Climate,24(15):3867-3877. DOI:10. 2307/ Hadley circulation extent[J]. Journal of Climate,32(14):4395-
26191121. 4408. DOI:10. 1175/JCLI-D-18-0657. 1.
Freitas A C V,Aímola L,Ambrizzi T,et al,2017. Change in intensi‐ Hu Y Y,Tung K K,Liu J P,2005. A closer comparison of early and lat‐
ty of the regional Hadley cell in Indian Ocean and its impacts on er-winter atmospheric trends in the northern hemisphere[J]. Jour‐