Different Impacts of the East Asian Winter Monsoon on the Surface Air Temperature in North America during ENSO and Neutral ENSO Years

• Published in: Journal of climate Vol. 33; no. 24; pp. 10671 - 10690
• Main Authors: Ma, Tianjiao, Chen, Wen, Graf, Hans-F., Ding, Shuoyi, Xu, Peiqiang, Song, Lei, Lan, Xiaoqing
• Format: Journal Article
• Language: English
• Published: Boston American Meteorological Society 15-12-2020
• Subjects: Air temperature; Anomalies; Barotropic mode; Circulation anomalies; Convection; Downstream effects; East Asian monsoon; Eddies; El Nino; El Nino phenomena; El Nino-Southern Oscillation event; Energy conversion; Jet stream; Jet streams (meteorology); Kinetic energy; Monsoons; Planetary waves; Rossby waves; Southern Oscillation; Surface temperature; Surface-air temperature relationships; Tropical climate; Tropical convection; Upstream; Wave packets; Wave reflection; Wind; Winter; Winter monsoon; North America
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/JCLI-D-18-0760.1

The present study investigates different impacts of the East Asian winter monsoon (EAWM) on surface air temperature (Ts) in North America (NA) during ENSO and neutral ENSO episodes. In neutral ENSO years, the EAWM shows a direct impact on the Ts anomalies in NA on an interannual time scale. Two Rossby wave packets appear over the Eurasian–western Pacific (upstream) and North Pacific–NA (downstream) regions associated with a strong EAWM. Further analysis suggests that the downstream wave packet is caused by reflection of the upstream wave packet over the subtropical western Pacific and amplified over the North Pacific. Also, the East Asian subtropical westerly jet stream (EAJS) is intensified in the central and downstream region over the central North Pacific. Hence, increased barotropic kinetic energy conversion and the interaction between transient eddies and the EAJS tend to maintain the circulation anomaly over the North Pacific. Therefore, a strong EAWM tends to result in warm Ts anomalies in northwestern NA via the downstream wave packet emanating from the central North Pacific toward NA. A weak EAWM tends to induce cold Ts anomalies in western-central NA with a smaller magnitude. However, in ENSO years, an anomalous EAJS is mainly confined over East Asia and does not extend into the central North Pacific. The results confirm that the EAWM has an indirect impact on the Ts anomalies in NA via a modulation of the tropical convection anomalies associated with ENSO. Our results indicate that, for seasonal prediction of Ts anomalies in NA, the influence of the EAWM should be taken into account. It produces different responses in neutral ENSO and in ENSO years.