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Chu, J. E., Wang, B., Lee, J. Y., & Ha, K. J. (2017). Boreal Summer Intraseasonal Phases Identified by Nonlinear Multivariate Empirical Orthogonal Function–Based Self-Organizing Map (ESOM) Analysis. Journal of Climate, 30(10), 3513-3528.

ByJung-Eun Chu, Bin Wang, June-Yi Lee, Kyung-Ja HaSeptember 08,2017

Boreal Summer Intraseasonal Phases Identified by Nonlinear Multivariate Empirical Orthogonal Function–Based Self-Organizing Map (ESOM) Analysis

JUNG-EUNCHU
Division of Earth Environmental System, College of Natural Science, and Research Center for Climate Sciences, Pusan National University, Busan, South Korea
BINWANG
International Pacific Research Center, and Department of Meteorology, University of Hawai‘i at Manoa, Honolulu, Hawaii, and Earth System Modeling Center, Nanjing University of Information Science and Technology, Nanjing, China
JUNE-YILEE
Research Center for Climate Sciences, Pusan National University, Busan, South Korea
KYUNG-JAHA
Division of Earth Environmental System, College of Natural Science, Research Center for Climate Sciences, and Department of Atmospheric Sciences, Pusan National University, Busan, South Korea
(Manuscript received 7 September 2016, in final form 3 January 2017)
 
ABSTRACT
This study develops an empirical orthogonal function (EOF)-based self-organizing map (SOM) (ESOM)  analysis to identify the nonlinear characteristics of the boreal summer intraseasonal oscillation (BSISO),  which involves interactions between the summer mean circulation and the convectively coupled equatorial  waves, which make BSISO evolution more complex than the Madden–Julian oscillation. The method utilizes the first five principal components of the outgoing longwave radiation (OLR) and the zonal wind at 850 hPa (U850) and has the advantages of filtering out uncertainties from noise and being free from mathematical restrictions, such as orthogonality and linearity.  The ESOM analysis enables the detection of BSISO over the Asian summer monsoon region with eight phases. The four most distinguishable phases represent 1) a pair of stationary patterns with a dipole between the eastern Indian Ocean and the Philippine Sea (phases 1 and 5) and 2) a pair of propagating patterns with a northwest–southeast-tilted rain belt structure (phases 3 and 7). Phases 1 and 5 show an alternating seesaw  oscillation throughout the summer with a 30–60-day period, whereas phases 3 and 7 peak in mid-June and  early June denoting the monsoon rainy season and premonsoon period of Asian summer monsoon. ESOM captures that phases 1 and 5 happen more frequently and last longer than phases 3 and 7, whereas multivariate EOF analysis fails to describe this nonlinear occurrence. Phases 3 and phase 7 display distinct asymmetries in convective activity over the eastern Indian Ocean related to the relatively slow-growing and fast-decaying convective activity. The relationship with large-scale SST forcing is also discussed.