Page 45 - 《高原气象》2022年第6期

高 原 气 象 41 卷
1408
nal of Climate，18（16）：3204-3216. DOI：10. 1175/JCLI3468. 1. Climate，9（11）：2751-2767，DOI：10. 1175/1520-0442（1996）
Huang B Y，L'Heureux M，Hu Z Z，et al，2016. Ranking the stron‐ 009<2751：OIVITH>2. 0. CO；2.
gest ENSO events while incorporating SST uncertainty［J］. Geo‐ Quan X W，Diaz H F，Hoerling M P，2004. Change in the tropical
physical Research Letters，43（17）：9165-9172. DOI：10. 1002/ Hadley cell since 1950. The Hadley circulation：past，present，
2016GL070888. and future［J］. Advance in Global Change Research，21：85-
Huang R P，Chen S F，Chen W，et al，2021. Northern poleward edge 120. DOI：10. 1007/978-1-4020-2944-8_4.
of regional Hadley cell over western Pacific during boreal winter： Schott F A，Xie S P，MsCreary J P，2009. Indian Ocean circulation
Year-to-year variability，influence factors and associated winter and climate variability［J］. Reviews of Geophysics，47（1）：
climate anomalies［J］. Climate Dynamics，56：3646-3664. DOI： RG1002. DOI：10. 1029/2007RG000245.
10. 1007/s00382-021-05660-9. Seager R S，Harnik N，Kushnir Y，et al，2003. Mechanisms of hemi‐
Huang R P，Chen S F，Chen W，et al，2019. Recent strengthening of spherically symmetric climate variability［J］. Journal of Climate，
the regional Hadley circulation over the western Pacific during bo‐ 16（18）：2960-2978. DOI：10. 1175/1520-0442（2003）016<
real spring［J］. Advances in Atmospheric Sciences，36（11）： 2960：MOHSCV>2. 0. CO；2.
1251-1264. DOI：10. 1007/s00376-019-9004-2. Son S W，Gerber E P，Perlwitz J，et al，2010. Impact of stratospheric
Johanson C M，Fu Q，2009. Hadley cell widening：Model simulations ozone on southern hemisphere circulation change：A multi-model
versus observations［J］. Journal of Climate，22（10）：2713-2725. assessment［J］. Journal of Geophysical Research，115：D00M07.
DOI：10. 1175/2008JCLI2620. 1. DOI：10. 1029/2010JD014271.
Larkin N K，Harrison D E，2005. Global seasonal temperature and Stachnik J P，Schumacher C，2011. A comparison of the Hadley circu‐
precipitation anomalies during El Niño autumn and winter［J］. lation in modern reanalysis［J］. Journal of Geophysical Research，
Geophysical Research Letters，32（16）：L16705. DOI：10. 1029/ 116：D22102. DOI：10. 1029/2011JD016677.
2005GL022860. Tanaka H L，Ishizaki N，Kitoh A，2004. Trend and interannual vari‐
Li J P，Feng J，2017. Tropical large-scale atmospheric interaction in ability of Walker，monsoon and Hadley circulations defined by
association with subtropical aridity trend［J］. Aridity Trend in velocity potential in the upper troposphere［J］. Tellus A：Dynam‐
Northern China，8：111-136. DOI：10. 1142/9789814723541_ ic Meteorology and Oceanography，56（3）：250-269. DOI：
0006. 10. 3402/tellusa. v56i3. 14410.
Lindzen R S，1994. Climate dynamics and global change［J］. Annual Wang C，2004. ENSO，Atlantic climate variability，and the Walker
Review of Fluid Mechanics，26（1）：353-378. DOI：10. 1146/an‐ and Hadley circulations［J］. The Hadley Circulation：Present，
nurev. fl. 26. 010194. 002033. Past and Future，Advances in Global Change Research，21：173-
Liu J，Song M，Hu Y，et al，2012. Changes in the strength and width 202. DOI：10. 1007/978-1-4020-2944-8_7.
of the Hadley circulation since 1871［J］. Climate of the Past，8 Wang C Z，2002. Atmospheric circulation cells associated with the El
（4）：1169-2012. DOI：10. 5194/cp-8-1169-2012. Niño-Southern Oscillation［J］. Journal of Climate， 15（4）：
Lu J，Vecchi G A，Reichler T，2007. Expansion of the Hadley cell un‐ 399-419.
der global warming［J］. Journal of the Atmospheric Sciences，55 Wang Y Q，Feng J，Li J P，et al，2020. Variability of boreal spring
（14）：2467-2547. DOI：10. 1175/1520-0469（1998）055<2437： Hadley circulation over the Asian monsoon domain and its rela‐
HCAAMO>2. 0. CO；2. tionship with tropical SST［J］. Climate Dynamics，54：1655-
Ma J，Li J P，2007. Strengthening of the boreal winter Hadley circula‐ 1669. DOI：10. 1007/s00382-019-05079-3.
tion and its connection with ENSO［J］. Progress in Natural Sci‐ Weng H Y，Ashok K，Behera S K，et al，2007. Impact of recent El
ence，17（11）：1327-1333. Niño Modoki on dry/wet conditions in the Pacific rim during bore‐
Ma J，Li J P，2008. The principal modes of variability of the boreal al summer［J］. Climate Dynamics，29：113-129. DOI：10. 1007/
winter Hadley cell［J］. Atmospheric Science，35：L01808. DOI： s00382-007-0234-0.
10. 1029/2007GL031883. Yu S Y，Fan L，Zhang Y，et al，2021. Reexamining the Indian sum‐
Martín-Gómez V，Barreiro M，2020. The influence of nonlinearities mer monsoon rainfall ENSO relationship from its recovery in the
st
and different SST spatial patterns on the summertime anomalies 21 Century：role of the Indian Ocean SST anomaly associated
in subtropical South America during strong ENSO events［J］. Cli‐ with types of ENSO evolution［J］. Geophysical Research Letters，
mate Dynamics，54：3765-3779. DOI：10. 1007/s00382-020- 48（12）：e2021GL092873. DOI：10. 1029/2021GL092873.
05201-w. Zhang G，Wang Z，2013. Interannual variability of the Atlantic Had‐
Mitas C M，Clement A，2006. Recent behavior of the Hadley cell and ley circulation in boreal summer and its impacts on tropical cy‐
tropical thermodynamics in climate models and reanalyses［J］. clone activity［J］. Journal of Climate，26（21）：8529-8544. DOI：
Geophysical Research Letters， 33： L01810. DOI： 10. 1029/ 10. 1175/JCLI-D-12-00802. 1.
2005GL024406. Zhang R，Sumi A，Kimoto M，1999. A diagnostic study of the impact
Oort A H，Yienger J J，1996. Observed interannual variability in the of El Niño on the precipitation in China［J］. Advances in Atmo‐
Hadley circulation and its connection to ENS-O［J］. Journal of spheric Science，16（2）：229-241. DOI：10. 1007/BF02973084.