Oceanic drivers and empirical prediction of interannual rainfall variability in late summer over Northeast China

被引:0
|
作者
Junhu Zhao
Han Zhang
Jinqing Zuo
Liu Yang
Jie Yang
Kaiguo Xiong
Guolin Feng
Wenjie Dong
机构
[1] National Climate Center,Laboratory for Climate Studies
[2] China Meteorological Administration,College of Atmospheric Sciences
[3] Lanzhou University,Department of Physical Science and Technology
[4] Jiangsu Climate Center,Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, School of Atmospheric Sciences
[5] Wuhan Regional Climate Center,undefined
[6] Yangzhou University,undefined
[7] Sun Yat-sen University,undefined
来源
Climate Dynamics | 2022年 / 58卷
关键词
Northeast China monsoon rainfall; Interannual variability; Oceanic drivers; Empirical prediction model;
D O I
暂无
中图分类号
学科分类号
摘要
Northeast China (NEC) is located between the subtropical monsoon and temperate-frigid monsoon regions and exhibits two successive rainy seasons with different natures: the northeast cold vortex rainy season in early summer (May–June) and the monsoon rainy season in late summer (July–August). Summer rainfall over NEC (NECR) has a fundamental influence on society, yet its successful seasonal prediction remains a long-term scientific challenge to current dynamical models. The poor NECR prediction skill is partly attributed to the large NECR variability at both the interannual and interdecadal time scales. Here, we focus on the oceanic drivers of the late summer NECR variability and associated physical processes at interannual time scale. Then, we establish an empirical prediction model to predict the interannual variability of summer NECR at 1-month lead time (in June). The analysis of observations spanning 40 years (1963–2002) reveals three physically and synergistically influencing predictors of the late summer NECR interannual variability. Above-normal NECR is preceded in the previous spring by (a) warm sea surface temperature (SST) anomalies in the tropical northern Indian Ocean, (b) a positive thermal contrast tendency in the tropical West–East Pacific SST, and (c) a positive tendency of the North Atlantic tripolar SST. These precursors enhance the anomalous low-level anticyclone over the western North Pacific and southerly anomalies over NEC in late summer, which are beneficial to enhancing NECR. An empirical prediction model built on these three predictors achieves a forecast temporal correlation coefficient (TCC) skill of 0.72 for 1961–2019, and a 17-year (2003–2019) independent forecast shows a significant TCC skill of 0.70. The skill is substantially higher than that of five state-of-the-art dynamical models and their ensemble mean for 1979–2019 (TCC = 0.24). These results suggest that the proposed empirical model is a meaningful approach for the prediction of NECR, although the dynamical prediction of NECR has considerable room for improvement.
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页码:861 / 878
页数:17
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