How Robust is the Asian Precipitation–ENSO Relationship during the Industrial Warming Period (1901–2017)?

• Published in: Journal of climate Vol. 33; no. 7; pp. 2779 - 2792
• Main Authors: Wang, Bin, Luo, Xiao, Liu, Jian
• Format: Journal Article
• Language: English
• Published: Boston American Meteorological Society 01.04.2020
• Subjects: Aridity; Atmospheric precipitations; Climate; Climate models; Coefficients; Correlation; Correlation coefficient; Correlation coefficients; Datasets; East Asian monsoon; El Nino; El Nino phenomena; El Nino-Southern Oscillation event; Environmental assessment; Hydroclimate; La Nina; Monsoons; Precipitation; Rain; Rainfall; Robustness; Sea surface; Seasonal variations; Seasonality; Southern Oscillation; Summer; Surface temperature; Time series; Tropical climate; Wind; Winter monsoon; Indian Ocean; Asia
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/jcli-d-19-0630.1

Instrumental observations (1901–2017) are used to uncover the seasonality, regionality, spatial–temporal coherency, and secular change of the relationship between El Niño–Southern Oscillation (ENSO) and Asian precipitation (AP). We find an abrupt seasonal reversal of the AP–ENSO relationship occurring from October to November in a large area of Asia north of 20°N due to a rapid northward shift of the ENSO-induced subsidence from Indonesia to the Philippines. We identified six subregions that have significant correlations with ENSO over the past 116 years with |r| > 0.5 (p < 0.001). Regardless of the prominent subregional differences, the total amount of AP during a monsoon year (from May to the next April) shows a robust response to ENSO with r = −0.86 (1901–2017), implying a 4.5% decrease in the total Asian precipitation for 1° of SST increase in the equatorial central Pacific. Rainfall in tropical Asia (Maritime Continent, Southeast Asia, and India) shows a stable relationship with ENSO with significant 31-yr running correlation coefficients (CCs). However, precipitation in North China, the East Asian winter monsoon front zone, and arid central Asia exhibit unstable relationships with ENSO. Since the 1950s, the AP–ENSO relationships have been enhanced in all subregions except over India. A major factor that determines the increasing trends of the AP–ENSO relationship is the increasing ENSO amplitude. Notably, the AP response is asymmetric with respect to El Niño and La Niña and markedly different between the major and minor ENSO events. The results provide guidance for seasonal prediction and a metric for assessment of climate models’ capability to reproduce the Asian hydroclimate response to ENSO and projected future change.