2019
DOI: 10.1155/2019/1762505
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Connection between Two Leading Modes of Autumn Rainfall Interannual Variability in Southeast China and Two Types of ENSO-Like SSTA

Abstract: The interannual variability of autumn rainfall in Southeast China (SEC) is significant, with two major modes, namely, monopole and dipole modes. It is found that the monopole mode is closely related to EP ENSO-like sea surface temperature anomaly (SSTA), and the dipole mode is related to CP ENSO-like SSTA. During the warm phase of EP ENSO-like SSTA, an anomalous anti-Walker circulation emerges in the tropical Pacific, with an anomalous subsiding during 110°E–120°E and an anomalous ascending branch in SEC. Thes… Show more

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Cited by 5 publications
(3 citation statements)
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“…The SST anomaly in the tropical Paci c is closely related to autumn rainfall in SEC (Liu et al, 2019;Jia et al, 2015;Gu et al, 2012); therefore, we also calculate the difference in SST and mixed layer sea temperature between 1991-2009 and 1971-1990 (Fig. 4).…”
Section: Tropical Central Paci C Warming Associated With the Interdec...mentioning
confidence: 99%
See 1 more Smart Citation
“…The SST anomaly in the tropical Paci c is closely related to autumn rainfall in SEC (Liu et al, 2019;Jia et al, 2015;Gu et al, 2012); therefore, we also calculate the difference in SST and mixed layer sea temperature between 1991-2009 and 1971-1990 (Fig. 4).…”
Section: Tropical Central Paci C Warming Associated With the Interdec...mentioning
confidence: 99%
“…Southeast China (SEC) includes Fujian, Guangdong, East Guangxi, Jiangxi, Hunan, South Hubei, and South Zhejiang, which is economically booming and a crucial tropical and subtropical agricultural production base in China (Liu et al, 2019). Therefore, the climatology and variation features of rainfall in SEC, as well as associated droughts and oods, have received much attention (Xin et al, 2006;Qiu et al, 2009;Wan et al, 2009;Jin et al, 2017;Liu et al, 2019).…”
Section: Introductionmentioning
confidence: 99%
“…The interaction between northerly and water vapor from southerly is responsible for the precipitation events over West China. In addition, the surface thermal regime and snow cover on the Tibetan Plateau (Chen et al, 2001;Huo et al, 2014), sea surface temperature (SST) in the tropical Pacific (Gu et al, 2014;Wang et al, 2015;Zhang et al, 2014), and the Indian Ocean Dipole Mode (Liu & Yuan, 2006) also significantly affect the variability of WCAP.…”
Section: Introductionmentioning
confidence: 99%