Search for other works by this author on: This Site. El Niño–Southern Oscillation (ENSO) is an irregularly periodic variation in winds and sea surface temperatures over the tropical eastern Pacific Ocean, affecting the climate of much of the tropics and subtropics. The Madden–Julian oscillation (MJO) is the largest element of the intraseasonal ... As the MJO progresses eastward, the favored region for tropical cyclone activity also shifts eastward from the western Pacific to the eastern Pacific and finally to the Atlantic basin. Western Pacific Index* From NOAA Climate Prediction Center (CPC) EA/WR Eastern Asia/Western Russia From NOAA Climate Prediction Center (CPC) NAO North Atlantic Oscillation* From NOAA Climate Prediction Center (CPC) NAO (Jones) North Atlantic Oscillation From CRU. Author information: (1)State Key Laboratory of Earth Surface Processes and Resource Ecology and College of Global Change and Earth System Science, Beijing Normal University, Beijing 100875, China. The positive phase of the WP pattern is associated with above-average temperatures over the lower latitudes of the western North Pacific in both winter and spring, and with below-average temperatures over eastern Siberia in all seasons. western Pacific subtropical high (WPSH), tropospheric biennial oscillation (TBO), East Asian monsoon, tropical sea surface temperature (SST) anomaly, intensity index, western boundary index

Changes in Western Pacific Tropical Cyclones Associated with the El Niño–Southern Oscillation Cycle Richard C. Y. Li; Richard C. Y. Li Guy Carpenter Asia-Pacific Climate Impact Centre, School of Energy and Environment, City University of Hong Kong, Hong Kong, China .

OeyThe Philippines–Taiwan oscillation: monsoonlike interannual oscillation of the subtropical–tropical western North Pacific wind system and its impact on the ocean Journal of Climate, 25 (2012), pp. The MJO is most evident in the Indian and western Pacific Oceans, where it includes variations in wind, sea-surface temperature, cloudiness, and rainfall that, in turn, affect the intensity and break periods of the Asian and Australian monsoons. Sun C(1), Kucharski F(2)(3), Li J(1)(4), Jin FF(5), Kang IS(3)(6), Ding R(7).

Google Scholar. ENSO is just one of many oscillations in… Over a wide range of realistic parameters the instability grows rapidly and is phase-locked to the calendar year in a similar way to the observations. Their relationship seems to be a seesaw feature, and this relationship resulting from the different pattern of convection in those two regions is caused by the differnt type of local meridional circulation. Together with, La Niña, these make up two of the three states of the constantly changing El Niño/Southern Oscillation (ENSO) that can affect weather patterns around the globe. A third anomaly center is located over the eastern North Pacific and southwestern United States in all seasons. Wen Zhou. The intraseasonal oscillation (convection) over the South China Sea and tropical western Pacific area is closely related to the summer rainfall (convection) in the southern China. This study examines the relationship between the zonal oscillation of the western Pacific subtropical high (WPSH) and underneath sea surface temperature (SST) variation on a subseasonal time scale, associated with the persistent heavy rainfall (PHR) events over the middle and lower reaches of the Yangtze River valley (MLYRV) in China. El Niño is a warming of surface waters in the eastern tropical Pacific Ocean. It can also interact with the Southern Oscillation, contributing to the intensity of an El Niño or La Niña event.

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