Abstract
The boreal summer intraseasonal oscillation (BSISO) has strong convective activity centers in Indian (I), Western North Pacific (WNP), and North American (NA) summer monsoon (SM) regions. The present study attempts to reveal BSISO teleconnection patterns associated with these dominant intraseasonal variability centers. During the active phase of ISM, a zonally elongated band of enhanced convection extends from India via the Bay of Bengal and Philippine Sea to tropical central Pacific with suppressed convection over the eastern Pacific near Mexico. The corresponding extratropical circulation anomalies occur along the waveguides generated by the North African-Asian jet and North Atlantic-North European jet. When the tropical convection strengthens over the WNPSM sector, a distinct great circle-like Rossby wave train emanates from the WNP to the western coast of United States (US) with an eastward shift of enhanced meridional circulation. In the active phase of NASM, large anticyclonic anomalies anchor over the western coast of US and eastern Canada and the global teleconnection pattern is similar to that during a break phase of the ISM. Examination of the evolution of the BSISO teleconnection reveals quasi-stationary patterns with preferred centers of teleconnection located at Europe, Russia, central Asia, East Asia, western US, and eastern US and Canada, respectively. Most centers are embedded in the waveguide along the westerly jet stream, but the centers at Europe and Russia occur to the north of the jet-induced waveguide. Eastward propagation of the ISO teleconnection is evident over the Pacific-North America sector. The rainfall anomalies over the elongated band near the monsoon domain over the Indo-western Pacific sector have an opposite tendency with that over the central and southern China, Mexico and southern US, providing a source of intraseasonal predictability to extratropical regions. The BSISO teleconnection along and to the north of the subtropical jet provides a good indication of the surface sir temperature anomalies in the NH extratropics.
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
Chen TC, Murakami M (1988) The 30–50 day variation of convective activity over the western Pacific Ocean with the emphasis on the northwestern region. Mon Weather Rev 116:892–906
Comeaux JL (1991) The origion and structure of the low-frequency modes. MS thesis Florida State University, Tallahassee, FL
Ding Q, Wang B (2007) Intraseasonal teleconnection between the summer Eurasian wave train and the Indian monsoon. J Clim 20:3751–3767
Duchon CE (1979) Lanczos filtering in one and two dimensions. J Appl Meteorol 18:1016–1022
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
Higgins RW, Schemm JKE, Shi W, Leetmaa A (2000) Extreme precipitation events in the western United States related to tropical forcing. J Clim 13:793–820
Hsu HH, Weng CH, Wu CH (2004) Contrasting characteristics between the northward and eastward propagation of the intraseasonal oscillation during the boreal summer. J Clim 17:727–743
Jiang X, Lau NC (2008) Intraseasonal teleconnection between North American and western North Pacific monsoons with 20-day time scale. J Clim 21:2664–2679
Jiang X, Waliser DE (2009) Two dominant subseasonal variability modes of the eastern Pacific ITCZ. Geophys Res Lett 36:L04704. doi:10.1029/2008GL036820
Jiang X, Li T, Wang B (2004) Structures and mechanisms of the northward propagating boreal summer intraseasonal oscillation. J Clim 17:1022–1039
Kawamura R, Murakami T, Wang B (1996) Tropical and mid-latitude 45-day perturbations over the western Pacific during the northern summer. J Meteorol Soc Jpn 74:867–890
Kemball-Cook S, Wang B (2001) Equatorial waves and air-sea interaction in the boreal summer intraseasonal oscillation. J Clim 14:2923–2942
Kikuchi K, Wang B (2009) Global perspective of the quasi-biweekly oscillation. J Clim 22:1340–1359
Kikuchi K, Wang B (2010) Formation of tropical cyclones in the northern Indian Ocean associated with two types of tropical intraseasonal oscillation modes. J Meteorol Soc Jpn 88(3):475–496
Knutson TR, Weickmann KM, Kutzbach JE (1986) Global-scale intraseasonal oscillations of outgoing longwave radiation and 250 mb zonal wind during northern hemisphere summer. Mon Weather Rev 114:605–623
Krishnamurti TN, Sinha MC, Krishnamurti R, Oosterhof D, Comeaux J (1992) Angular momentum, length of day and monsoonal low frequency mode. J Meteorol Soc Jpn 70:131–166
Lee JY, Wang B, Kang IS, Shukla J et al (2010) How are seasonal prediction skills related to models’ performance on mean state and annual cycle? Clim Dyn 35:267–283
Lee JY, Wang B, Ding Q, Ha KJ, Ahn JB, Kumar A, Stern B, Alves O (2011) How predictable is the northern hemisphere summer upper-tropospheric circulation? Clim Dyn 37:1189–1203
Liu AZ, Ting M, Wang H (1998) Maintenance of circulation anomalies during the 1988 drought and 1993 floods over the United States. J Atmos Sci 55:2810–2832
Lorenz DJ, Hartmann DL (2006) The effect of the MJO on the North American monsoon. J Clim 19:333–343
Madden RA, Julien PR (1971) Detection of a 40–50 day oscillation in the zonal wind in the tropical Pacific. J Atmos Sci 28:702–708
Mao JY, Chan JCL (2005) Intraseasonal variability of the South China Sea summer monsoon. J Clim 18:2388–2402
Mo KC (2000) Intraseasonal modulation of summer precipitation over North America. Mon Weather Rev 128:1490–1505
Mullen SL, Schmitz JT, Renno NO (1998) Intraseasonal variability of the summer monsoon over southeast Arizona. Mon Weather Rev 126:3016–3035
Newman M, Sardeshmukh PD (1998) The impact of the annual cycle on the North Pacific/North American response to remote low-frequency forcing. J Atmos Sci 55:1336–1353
Plumb RA (1985) On the three-dimensional propagation of stationary waves. J Atmos Sci 42:217–229
Schubert S, Wang H, Suarez M (2011) Warm season subseasonal variability and climate extremes in the Northern Hemisphere: the role of stationary Rossby waves. J Clim 24:4773–4792
Teng H, Wang B (2003) Interannual variations of the boreal summer intraseasonal oscillation in the Asia-Pacific region. J Clim 16:3572–3584
Wang B, Fan Z (1999) Choice of South Asian summer monsoon indices. Bull Am Meteorol Soc 80:629–638
Wang B, Rui H (1990) Synoptic climatology of transient tropical intraseasonal convection anomalies: 1975–1985. Meteorol Atmos Phys 44:43–61
Wang B, Xie X (1997) A model for the boreal summer intraseasonal oscillation. J Atmos Sci 54:72–86
Wang B, Wu RG, Lau KM (2001) Interannual variability of the Asian summer monsoon: contrasts between the Indian and the western North Pacific-east Asian monsoon. J Clim 14:4073–4090
Wang B, Webster B, Kikuchi K, Yasunari T, Qi Y (2006) Boreal summer quasi-monthly oscillation in the global tropics. Clim Dyn 27:661–675
Wang B, Lee JY, Shukla J, Kang IS et al (2009) Advance and prospectus of seasonal prediction: assessment of APCC/CliPAS 14-model ensemble retrospective seasonal prediction (1980–2004). Clim Dyn 33:93–117
Xie P, Yatagai A, Chen M, Hayasaka T, Fukushima Y, Liu C, Yang S (2007) A gauge-based analysis of daily precipitation over East Asia. J Hydrometeorol 8:607–626
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
Yasunari T (1979) Cloudiness fluctuations associated with the Northern Hemisphere summer monsoon. J Meteorol Soc Jpn 57:227–242
Zhu B, Wang B (1993) The 30–60 day convection seesaw between the tropical Indian and western Pacific Oceans. J Atmos Sci 50:184–199
Acknowledgments
This work was supported by the Climate Dynamics Program of the National Science Foundation under award No AGS-1005599 and by GRL grant of the National Research Foundation (NRF) funded by Korean government (MEST) (No. 2011-0021927). ECMWF ERA-Interim data used in this study have been obtained from the ECMWF data server. This manuscript is SOEST Contribution No. 8677 and IPRC contribution No. 888.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Moon, JY., Wang, B., Ha, KJ. et al. Teleconnections associated with Northern Hemisphere summer monsoon intraseasonal oscillation. Clim Dyn 40, 2761–2774 (2013). https://doi.org/10.1007/s00382-012-1394-0
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00382-012-1394-0