Relationship between interannual changes of summer rainfall over Yangtze River Valley and South China Sea–Philippine Sea: Possible impact of tropical zonal sea surface temperature gradient

• Published in: International journal of climatology Vol. 39; no. 14; pp. 5522 - 5538
• Main Authors: Ha, Yao, Zhong, Zhong, Zhang, Yun, Ding, Jinfeng, Yang, Xiangrong
• Format: Journal Article
• Language: English
• Published: Chichester, UK John Wiley & Sons, Ltd 30.11.2019; Wiley Subscription Services, Inc
• Subjects: Atmospheric circulation; Boundary layers; Circulation anomalies; Divergence; Environmental conditions; equatorial central and eastern Pacific; Hadley circulation; Interannual variability; middle‐lower reaches of Yangtze River Valley; northern Indian Ocean; Numerical experiments; out‐of‐phase relationship; Phase transitions; Philippine Sea; Precipitable water; Rain; Rainfall; Rainfall variations; Regions; River valleys; Rivers; Sea surface; Sea surface temperature; South China Sea; Summer; Summer rainfall; Surface temperature; Temperature gradients; Tropical climate; Tropical environments; tropical zonal SST gradient; Westerlies; South China Sea; Philippine Sea; Yangtze River
• ISSN: 0899-8418; 1097-0088
• DOI: 10.1002/joc.6169

This study investigates the interannual variability of rainfall over the middle and lower reaches of Yangtze River Valley (MLYRV) and that over the South China Sea and Philippine Sea (SCS‐PS) during boreal summer (June–August) from 1979 to 2012. Results exhibit out‐of‐phase rainfall variations between the MLYRV and the SCS‐PS, which is closely related to the tropical zonal sea surface temperature gradient (ZSG) between the northern Indian Ocean (NIO; 5°–25°N, 60°–100°E) and the equatorial central and eastern Pacific (CEP; 5°S–5°N, 180°–130°W). The ZSG can explain as much as 40% of the total variance of the summer rainfall over the MLYRV and the SCS‐PS in the past 40 years. This is much higher than that explained by the NIO SST (24%), CEP SST (14%) and Niño‐3.4 index (16%) alone. A positive ZSG between the warm NIO and the cold CEP tends to increase rainfall over the MLYRV and decrease rainfall over the SCS‐PS, whereas a negative ZSG between the cold NIO and the warm CEP is generally favourable for rainfall over the SCS‐PS and unfavourable for rainfall over MLYRV. The close connection between the ZSG and the out‐of‐phase interannual rainfall variation over the two regions can be explained by influences of the ZSG on atmospheric circulation over East Asia. A positive ZSG induces anomalous easterlies and Walker‐like circulation in the tropics, which results in an anomalous subsidence and boundary layer divergence over the SCS‐PS. As a result, summer rainfall decreases in this region. Meanwhile, moisture transport increases due to the anomalously strong southwesterlies along the northwestern flank of the intensified western Pacific subtropical high, providing more precipitable water to the MLYRV region. In contrast, a negative ZSG induces surface westerlies and favourable environmental condition for rainfall over the SCS‐PS. Dry descending flow induced by local anomalous Hadley circulation develops over the MLYRV around 30°N, which is unfavourable for rainfall over the MLYRV. The mechanism further examined using numerical experiments. These thermal‐dynamical processes induced by the ZSG work together to cause the out‐of‐phase interannual changes of rainfall between the MLYRV and the SCS‐PS, suggesting that the ZSG is highly indicative of the interannual change of summer rainfall in the two regions. (a) Spatial distribution of the first EOF mode of summer rainfall anomaly (shade; mm/day). (b) the corresponding principal components. (c) Power spectrum of PC1 during 1979–2012, and the dashed line in (c) represents the 95% confidence level.