Abstract
The present study documents the factors for year-to-year changes in the intensity of 10–20-day intraseasonal oscillations (ISOs) and investigates the feedback of the 10–20-day ISO intensity on seasonal mean sea surface temperature (SST) change in the tropical western North Pacific during boreal spring through fall. An analysis of local correlation reveals a significant negative correlation of the 10–20-day ISO intensity and the seasonal mean SST tendency in the tropical western North Pacific during spring, summer, and fall, suggesting a plausible feedback of the ISO intensity on seasonal mean SST anomaly. The 10–20-day ISO intensity change over the tropical western North Pacific is influenced by El Niño-Southern Oscillation (ENSO) through modulation of vertical shear of zonal winds, lower-level moisture, and upward motion. Due to the phase dependence of location of these ENSO-induced background field changes, the ISO intensity is subject to ENSO influence in different regions during the three seasons. The feedback of the 10–20-day ISO intensity on local seasonal mean SST change in the tropical western North Pacific is demonstrated by separating latent heat flux anomalies into components on different time scales. The ISO-induced latent heat flux anomalies may accumulate in a season and overcome interannual anomalies due to seasonal mean changes. Thus, the ISO-induced surface heat flux change may play an important role in the seasonal mean SST anomaly in the tropical western North Pacific.
Similar content being viewed by others
References
Annamalai H, Slingo JM (2001) Active/break cycles: diagnosis of the intraseasonal variability of the Asian summer monsoon. Clim Dyn 18:85–102
Cao X, Wu R, Chen SF (2016) Contrast of 10–20-day and 30–60-day intraseasonal SST propagation during summer and winter over the South China Sea and western North Pacific. Clim Dyn. doi:10.1007/s00382-016-3138-z
Chen TC, Chen JM (1995) An observational study of the South China Sea monsoon during the 1979 summer: onset and life cycle. Mon Weather Rev 123:2295–2318
Chen JP, Wen ZP, Wu R, Chen ZS, Zhao P (2015) Influences of northward propagating 25–90-day and quasi-biweekly oscillations on eastern China summer rainfall. Clim Dyn 45(102):105–124
Chen X, Ling J, Li C (2016) Evolution of Madden–Julian Oscillation in two types of El Niño. J Clim 29(5):1919–1934
Chou S-H, Nelkin E, Ardizzone J, Altas RM (2004) A comparison of latent heat fluxes over global oceans for four flux products. J Clim 17:3973–3989
de Boyer Montégut C, Madec G, Fischer AS, Lazar A, Iudicone A (2004) Mixed layer depth over the global ocean: an examination of profile data and a profile-based climatology. J Geophys Res 109:C12003. doi:10.1029/2004JC002378
Feng X, Wu R, Chen J, Wen ZP (2013) Factors for interannual variations of September–October rainfall in Hainan, China. J Clim 26:8962–8978
Feng J, Liu P, Chen W, Wang XC (2015) Contrasting Madden–Julian Oscillation activity during various stages of EP and CP El Niños. Atmos Sci Lett 16:32–37
Fukutomi Y, Yasunari T (1999) 10–25-day intraseasonal variations of convection and circulation over East Asia and western North Pacific during early summer. J Meteorol Soc Jpn 77:753–769
Gill AE (1980) Some simple solutions for heat-induced tropical circulation. Q J R Meteorol Soc 106(449):447–462
Griffies SM, Harrison MJ, Pacanowski RC, Rosati A (2004) A technical guide to MOM4. GFDL ocean group technical report no. 5. NOAA/Geophysical Fluid Dynamics Laboratory, Princeton, p 342
Gushchina D, Dewitte B (2012) Intraseasonal tropical atmospheric variability associated with the two flavors of El Niño. Mon Weather Rev 140:3669–3681
Hendon HH, Wheeler M, Zhang C (2007) Seasonal dependence of the MJO-ENSO relationship. J Clim 20:531–543
Huang P, Chou C, Huang R (2011) Seasonal modulation of tropical intraseasonal oscillations on tropical cyclone genesis in the western North Pacific. J Clim 24:6339–6352
Kajikawa Y, Yasunari T (2005) Interannual variability of the 10–25- and 30–60-day variation over the South China Sea during boreal summer. Geophys Res Lett 32:L04710. doi:10.1029/2004GL021836
Kanamitsu M, Ebisuzaki W, Woollen J, Yang SK, Hnilo JJ, Fiorino M, Potter GL (2002) NCEP–DOE AMIP-II reanalysis (R-2). Bull Am Meteorol Soc 83:1631–1643
Kikuchi K, Wang B (2009) Global perspective of the quasi-biweekly oscillation. J Clim 22:1340–1359
Kulkarni A, Kripalani R, Sabade S, Rajeevan M (2011) Role of intraseasonal oscillations in modulating Indian summer monsoon rainfall. Clim Dyn 36:1005–1021
Lindzen RS, Nigam S (1987) On the role of sea surface temperature gradients in forcing low-level winds and convergence in the tropics. J Atmos Sci 44:2418–2436
Liu F, Zhou L, Ling J, Fu X, Huang G (2016a) Relationship between SST anomalies and the intensity of intraseasonal variability. Theor Appl Climatol. doi:10.1007/s00704-015-1458-2
Liu F, Li T, Wang H, Deng L, and Zhang YW (2016b) Modulation of boreal summer intraseasonal oscillations over the western North Pacific by ENSO. J Clim accepted
Mao J, Chan JCL (2005) Intraseasonal variability of the South China Sea summer monsoon. J Clim 18(13):2388–2402
Reynolds RW, Rayner NA, Smith TM, Stokes DC, Wang W (2002) An improved in situ and satellite SST analysis for climate. J Clim 15:1609–1625
Tam CY, Lau NC (2005) Modulation of the Madden–Julian Oscillation by ENSO: inferences from observations and GCM simulations. J Meteorol Soc Jpn 83(5):727–743
Tang Y, Yu B (2008) MJO and its relationship to ENSO. J Geophys Res 113:D14106. doi:10.1029/2007JD009230
Teng H, Wang B (2003) Interannual variations of the boreal summer intraseasonal oscillation in the Asian-Pacific Region. J Clim 16:3572–3584
Wu R (2010) Subseasonal variability during the South China Sea summer monsoon onset. Clim Dyn 34:629–642
Wu R, Cao X (2016) Relationship of boreal summer 10–20-day and 30–60-day intraseasonal oscillation intensity over the tropical western North Pacific to tropical Indo-Pacific SST. Clim Dyn. doi:10.1007/s00382-016-3282-5
Wu R, Kirtman BP (2007) Regimes of local air-sea interactions and implications for performance of forced simulations. Clim Dyn 29:393–410
Wu R, Wang B (2000) Interannual variability of summer monsoon onset over the western North Pacific and the underlying processes. J Clim 13:2483–2501
Wu R, Wang B (2001) Multi-stage onset of the summer monsoon over the western North Pacific. Clim Dyn 17:277–289
Wu R, Hu ZZ, Kirtman BP (2003) Evolution of ENSO-related rainfall anomalies in East Asia. J Clim 16:3741–3757
Wu R, Kirtman BP, Pegion K (2006) Local air-sea relationship in observations and model simulations. J Clim 19(19):4914–4932
Wu R, Cao X, Chen SF (2015) Co-variations of SST and surface heat flux on 10–20-day and 30–60-day time scales over the South China Sea and western North Pacific. J Geophys Res 120(24):12486–12499
Yang J, Wang B, Wang B (2008) Anticorrelated intensity change of the quasi-biweekly and 30–50-day oscillations over the South China Sea. Geophys Res Lett 35:L16702. doi:10.1029/2008GL034449
Ye KH, Wu R (2015) Contrast of local air-sea relationship between 10–20-day and 30–60-day intraseasonal oscillations during May-September over the South China Sea and the western North Pacific. Clim Dyn 45(11–12):3441–3459
Zhang C (2005) Madden–Julian Oscillation. Rev Geophys. doi:10.1029/2004RG000158
Zhang C (2013) Madden–Julian Oscillation: bridging weather and climate. J Clim 94:1849–1870
Zhang C, Gottschalck J (2002) SST anomalies of ENSO and the Madden–Julian Oscillation in the equatorial Pacific. J Clim 15:2429–2445
Zhang LN, Wang BZ, Zeng CQ (2009) Impacts of the Madden–Julian Oscillation on summer rainfall in southeast China. J Clim 22:201–216
Acknowledgments
The two anonymous reviewers’ comments help to improve the paper. This study is supported by the National Key Basic Research Program of China grant (2014CB953902), the National Key Research and Development Program grant (2016YFA0600603), and the National Natural Science Foundation of China grants (41475081, 41275081, and 41530425). The NCEP-DOE reanalysis 2 data and the NOAA OLR data were obtained from ftp://ftp.cdc.noaa.gov/. The NOAA OI version 2 SST data are obtained from http://www.esrl.noaa.gov/psd/.
Author information
Authors and Affiliations
Corresponding author
Additional information
This paper is a contribution to the special issue on East Asian Climate under Global Warming: Understanding and Projection, consisting of papers from the East Asian Climate (EAC) community and the 13th EAC International Workshop in Bei**g, China on 24–25 March 2016, and coordinated by Jian** Li, Huang-Hsiung Hsu, Wei-Chyung Wang, Kyung-Ja Ha, Tim Li, and Akio Kitoh.
Rights and permissions
About this article
Cite this article
Wu, R. Feedback of 10–20-day intraseasonal oscillations on seasonal mean SST in the tropical Western North Pacific during boreal spring through fall. Clim Dyn 51, 4169–4184 (2018). https://doi.org/10.1007/s00382-016-3362-6
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00382-016-3362-6