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The mechanism of EAP-EU combined impact on summer rainfall over North Asia

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Abstract

This article uses wave activity flux and sea surface temperature (SST) to explore the mechanism of EAP-EU combined impact on summer rainfall in North Asia (NA). EAP and EU teleconnections can be divided into four categories of configuration according to their anomaly phase features. The category I (II) configurations cause rainfall in the Urals and the Okhotsk Sea and the region from Northeast China to Japan being less (more), the Lake Baikal to the Okhotsk Sea being more (less), which leads to the summer rainfall in NA mainly presenting the “− + −” (“+ − +”) a tripole wavelike structure. Category I (II) configurations also show the West-East reverse anomalies of summer rainfall in northern NA and the North-South opposite anomalies in eastern NA. The EAP and EU teleconnections have an obvious correlation with the ENSO-like pattern of SST anomalies over the tropical Pacific. When warm ENSO is in the development phase, it is conducive to stimulate Rossby waves propagating eastward from the North Atlantic Ocean via the PNA teleconnection, forming the EU teleconnection across the Eurasia continent. Meanwhile, the warm summer SSTA anomalies over tropical east Pacific and IMC are conducive to the local thermal convective over Indo-Pacific warm pool and motivate the EAP teleconnection, propagating northward to mid-high latitude region. EAP and the EU teleconnections overlapped with each other, form the tripole atmospheric structure in NA, and produce relevant rainfall anomaly patterns. For the category IV of EAP-EU configuration, the warm SST anomalies in the equatorial region gradually weaken from previous winter to summer. Weak tropical east Pacific SST anomalies are conducive to excite the EU teleconnection with different wave train features against the category II, presenting a strong positive anomaly center over the Ural mountain and Baikal lake. This positive center connected with the EAP caused positive anomalies over FER resulting in the dipole pattern of atmospheric and rainfall anomalies in the summer season. The condition is opposite for the category III (I) configuration against that of category IV (II). It is also found that the influence on EAP-EU configuration caused by ENSO-like pattern of SST anomalies over the tropical Pacific has an obvious asymmetric feature that category II (I) configuration relevant SST forcing is much significant than that of category IV(III) configuration.

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References

  • Andrews D G, McIntyre M E (1976) Planetary waves in horizontal and vertical shear: The generalized Eliassen-Plam relation and the mean zonal acceleration [J]. J. Atmos. Sci., 33(11):2031-2-48.

  • Bjerknes J (1969) Monthly weather review atmospheric teleconnections from the equatorial pacific. Mon. Wea. Rev. 97(3):163–172

    Google Scholar 

  • Bueh C, Shi N, Ji LR et al (2008) Features of the EAP events on the medium-range evolution process and the mid- and high-latitude Rossby wave activities during the Meiyu period. Chin. Sci. Bull. 53:610–623

    Google Scholar 

  • Chen G, Huang G (2012) Excitation mechanisms of the teleconnection pattern affecting the July rainfall in Northwest China. J. Climate 25(22):7834–7851

    Google Scholar 

  • Chen Y, Zhai PM (2015) Synoptic-scale precursor features of East Asia/Pacific teleconnection pattern responsible for persistent extreme rainfall in the Yangtze River valley. Quart. J. Roy. Meteor. Soc. 141:1389–1403

    Google Scholar 

  • Chen Y, Chen T, Wang LY (2019) A review of the warm-sector rainstorms in China. Torrential Rain and Disasters 38(5):493–493

    Google Scholar 

  • Choi KS, Moon IJ (2012) Influence of the Western Pacific teleconnection pattern on Western North Pacific tropical cyclone activity. Dynamics of Atmospheres and Oceans 57:1–16

    Google Scholar 

  • Choi KS, Wu CC, Cha EJ (2010) Change of tropical activity by Pacific-Japan teleconnection pattern in the western North Pacific. Journal of Geophysical Research Atmospheres 115:D19114

    Google Scholar 

  • Chu PS (1998) Extratropical forcing and the burst of equatorial westerlies in the western Pacific - a synoptic study. J.Meteor.Soc. Japan 35:997–1011

    Google Scholar 

  • Clarke AJ, Shu L (2000) Biennial wind in the far western equatorial Pacific Phase-locking El Nino to the seasonal cycle. Geophys. Res. Letters 27(6):771–774

    Google Scholar 

  • Ding (2019) The major advances and development process of the theory of heavy rainfalls in China. Torrential Rain and Disasters 38(5):395–406

    Google Scholar 

  • Dogar MM, Kucharski F, Azharuddin S (2017) Study of the global and regional climatic impacts of ENSO magnitude using SPEEDY AGCM. Journal of Earth System Science 126(2):30

    Google Scholar 

  • Dogar MM, Kucharski F, Sato T et al (2019) Towards understanding the global and regional climatic impacts of Modoki magnitude. Global and Planetary Change 172:223–241

    Google Scholar 

  • Gong ZQ, Dogar MM, Qiao SB et al (2017a) Assessment and correction of BCC_CSM’s performance of capturing leading modes of summer precipitation over North Asia. Int. J. Climate 38:2201–2214

    Google Scholar 

  • Gong ZQ, Dogar MM, Qiao SB et al (2017b) Limitations of BCC_CSM’s ability to predict summer precipitation over East Asia and the Northwestern Pacific. Atmospheric Research 193:184–191

    Google Scholar 

  • Gong ZQ, FengGL DMMA, Huang G (2017c) The possible physical mechanism for the EAP-SR co-action. Climate Dynamics 51:1499–1516

    Google Scholar 

  • Held IM, Hoskins BJ (1985) Large-scale eddies and the general circulation of the troposphere. Advances in Geophysics 28:3–31

    Google Scholar 

  • Hoskins BJ and Karoly DJ (1981) The steady linear response of a spherical atmosphere to thermal and orographic forcing. Journal of Atmospheric Sciences, 38(6): 1179-1196.

  • Huang G (2004) An index measuring the interannual variation of the East Asian summer monsoon – the EAP index. Advances in Atmospheric Sciences 21(1):41–52

    Google Scholar 

  • Huang RH, Li WJ (1987) Influence of the heat source anomaly over the tropical western Pacific on the subtropical high over East Asia. Proc. Internal. Conf. on the General Circulation of East Asia, Chengdu, 10(15):40-51.

  • Huang RH, Sun FY (1992) Impacts of tropical western Pacific on the East Asia summer monsoon. J. Meteor. Soc. Japan. 1:243–256

    Google Scholar 

  • Huang RH, Chen JL, Huang G (2007) Characteristics and variations of the East Asian monsoon system and its impacts on climate disasters in China. Advances in Atmospheric Sciences 24:993–1023

    Google Scholar 

  • Kosaka Y, Nakamura H (2006) Structure and dynamics of the summertime Pacific–Japan teleconnection pattern. Quarterly Journal of the Royal Meteorological Society 132:2009–2030

    Google Scholar 

  • Kosaka Y, Xie SP, Nakamura H (2011) Dynamics of interannual variability in summer precipitation over East Asia. Journal of Climate 24:5435–5453

    Google Scholar 

  • Kurihara K, Kawahara M (1986) Extremes of East Asian weather during the post ENSO years of 1983/84[J]. Journal of the Meteorological Society of Japan 64:493–503

    Google Scholar 

  • Lau KM (1992) East Asian summer Monsoon rainfall variability and climate teleconnection [J]. J. Meteor. Soc. Japan 70:211–242

    Google Scholar 

  • Lee EJ, Jhun JG, Park CK (2005) Remote connection of the northeast Asian summer rainfall variation revealed br a newly defined monsoon index. J. Climate. 18(21):4381–4393

    Google Scholar 

  • Li J, Yu RC, Zhou TJ (2008) Teleconnection between NAO and climate downstream of the Tibetan Plateau. J. Climate. 21(18):4680–4690

    Google Scholar 

  • Li L, Zhai PM, Chen Y, Ni YQ (2016) Low-frequency oscillations of the East Asia-Pacific teleconnection pattern and their impacts on persistent heavy rainfall in the Yangtze-Huai River Valley. Journal of Meteorological Research 30(4):459–471

    Google Scholar 

  • Liu HB, Wen M, He JH et al (2012) Characteristics of the northeast cold vortex at intraseasonal timescale and its impact. Chinese Journal Atmospheric Science (in Chinese) 36(5):959–973

    Google Scholar 

  • Liu YY, Wang L, Zhou W, Chen W (2014) Three Eurasian teleconnection patterns: spatial structures, temporal variability, and associated winter climate anomalies. Clim. Dyn. 42(11):2817–2839

    Google Scholar 

  • Nitta T (1987) Convective activities in the tropical western Pacific and their impact on the northern hemisphere summer circulation. J. Meteor. Soc. Japan 65(3):373–390

    Google Scholar 

  • Peng SL, Robinson WA, Li SL (2003) Mechanisms for the NAO responses to the North Atlantic SST Tripole [J]. J. Clim. 16(12):1987–2004

    Google Scholar 

  • Phiander SGH (1981) The Response of equatorial oceans to a relaxation of the trade winds. Journal of Physical Oceanography 11(2):176–189

    Google Scholar 

  • Picaut J, Loualalen M, Menkes C et al (1996) Mechanism of the zonal displacements of the Pacific warm pool: implications of ENSO. Science 274:1486–1489

    Google Scholar 

  • Plumb RA (1985) On the three-dimensional propagation of stationary waves. J. Atmos. Sci. 42:217–229

    Google Scholar 

  • Rogers JC, Coleman JSM (2003) Interactions between the Atlantic Multidecadal Oscillation El Nino/La Nina, and the PNA in winter Mississippi Valley Stream flow. Geophysical Research Letters 30(10):1518

    Google Scholar 

  • Shi N, Bueh JLR et al (2008) The impact of mid-and high-latitude Rossby wave activities on the medium-range evolution of EAP event in the pre-rainy period of South China. Acta Meteorologica Sinica (in Chinese) 66(6):1020–1031

    Google Scholar 

  • Shi CH, Jin X, Liu RQ (2017) The differences in characteristics and applicability among three types of Rossby wave activity flux in atmospheric dynamics. Transactions of Atmospheric Sciences (in Chinese) 40(6):850–855

    Google Scholar 

  • Sui C, Chung P, Li T (2007) Interannual and interdecadal variability of the summertime western North Pacific subtropical high. Geophysical Research Letters 34(11):93–104

    Google Scholar 

  • Tachibana Y, Nakamura T, Tazou N (2007) Interannual variation in snow accumulation events in Tokyo and its relationship to the Eurasian pattern. Sci. Online Lett. Atmos. 3:129–131

    Google Scholar 

  • Takaya K, Nakamura H (1997) A formulation of a wava-activity flux for stationary Rossby waves on a zonally varying basic flow. Geophys. Res. Lett. 24(23):2985–2988

    Google Scholar 

  • Takaya K, Nakamura H (2001) A formulation of a phase-independent wave activity flux for stationary and migratory quasigeostrophic eddies on a zonally varying basic flow [J]. J. Atmos. Sci. 58:608–627

    Google Scholar 

  • Trenberth KE (1986) An assessment of the impact of transient eddies on the zonal flow during a blocking episode using localized Eliassen-Palm flux diagnostic. J. Atmos. Sci. 43:2070–2087

    Google Scholar 

  • Wakabayashi S, Kawanura R (2004) Extraction of major teleconnection patterns possibly associated with the anomalous summer climate in Japan. J. Meteor. Soc. Japan. 82(6):1577–1588

    Google Scholar 

  • Wallace JM, Gutzler DS (1981) Teleconnection in the geopotential height field during the Northern Hemisphere winter. Mon. Wea. Rev. 109:748–812

    Google Scholar 

  • Wang LJ, Wang C, Guo D (2018) Evolution mechanism of synoptic-scale EAP teleconnection pattern and its relationship to summer precipitation in China. Atmospheric Research 214:150–162

    Google Scholar 

  • Yang RW, Tao Y, Cao J (2010) A mechanism for the interannual variation of the early summer East Asia-Pacific teleconnection wave train. Acta Meteorologica Sinica 24(4):452–458

    Google Scholar 

  • Zou SS, Guo PW, Yang HJ (2013) The configuration between the East Asia Pacific and the Eurasian teleconnection patterns and its influence on the summer climate of China. Journal of the Meteorological Sciences (in Chinese) 33(1):10–18

    Google Scholar 

Download references

Funding

This research was supported by the National Key Research and Development Program of China (2018YFC1507702 and 2018YFA0606301) and the National Natural Science Foundation Project of China (41875100 and 41530531).

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Authors and Affiliations

  1. Hubei Key Laboratory for Heavy Rain Monitoring and Warning Research, Institute of Heavy Rain, China Meteorological Administration, Wuhan, China

    Po Hu

  2. School of Environmental Science and Engineering, Yancheng Institute of Technology, Yancheng, China

    Jianbo Cheng

  3. Laboratory for Climate Studies, National Climate Research Center CMA, Beijing, China

    Guolin Feng & Zhiqiang Gong

  4. Global Change Impact Studies Centre, Ministry of Climate Change, Islamabad, Pakistan

    Muhammad Mubashar Ahmad Dogar

  5. College of Physics and Electronic Engineering, Changshu Institute of Technology, Changshu, China

    Zhiqiang Gong

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  1. Po Hu
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  2. Jianbo Cheng
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  5. Zhiqiang Gong
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Correspondence to Zhiqiang Gong.

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Hu, P., Cheng, J., Feng, G. et al. The mechanism of EAP-EU combined impact on summer rainfall over North Asia. Theor Appl Climatol 142, 117–128 (2020). https://doi.org/10.1007/s00704-020-03295-0

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