Abstract
Using the outgoing long-wave radiation (OLR) data from NOAA, the ERA-Interim reanalysis products from ECMWF, and daily observations at 756 stations provided by National Meteorological Information Center of China Meteorology Administration, we have examined the relationships of interannual variations of summer precipitation in Southwest China with the convective activity in the Maritime Continent (MC) region by employing the singular value decomposition (SVD) method and the regional climate model RegCM4.4. The first SVD mode (here after SVD1) indicates that high precipitation anomalies in Southwest China correspond to abnormally weak convective activity in northeastern MC and strong convective activity in Southwestern MC if the time-series of coefficients of SVD1 is in positive phase. When convective activity are anomalously strong in Southern MC, the anomalous divergence at 700 hPa and convergence at 200 hPa are observed over the tropical western Pacific and South China Sea. The propagation of wave energy at 700 hPa from Western Europe and the tropics provide a favorable condition for inducing more precipitation in most of Southwest China. The atmospheric water vapor transport from northern Indochina and the South China Sea to Southwest China intensifies while the western Pacific subtropical high is stronger than normal and extends more westward. All these results along with the simulations demonstrate that the summer precipitation in Southwest China is significantly affected by the convective activity over the MC region. These results above are helpful for our better understanding the role of the MC in regulating the summer climate in Southwest China.
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References
Alexander AM (2002) The atmospheric bridge: the influence of ENSO teleconnections on air-sea interaction over the global oceans. J Clim 15(16):2205–2231
Ashok KZ, Guan Z, Yamagata T (2003) A look at the relationship between the ENSO and the Indian Ocean dipole. J Meteorol Soc Jpn 81(1):41–56
Bao Y, Kang Z, Jin R et al (2007) Analysis of floods and droughts in Chongqing and East Sichuan. Meteorol Monthly 33(5):85–93 (Chinese)
Chang CP, Lau KM (1982) Short-term planetary-scale interactions over the tropics and midlatitude during northern winter. Part I, Contrasts between active and inactive periods. Mon Weather Rev 110(8):1666–1672
Chang CP, Harr PA, Chen HJ (2005) Synoptic Disturbances over the Equatorial South China Sea and Western Maritime Continent during Boreal Winter. Mon Weather Rev 133:489–503
Chen W, Guan Z (2017) A joint monsoon index for East Asian- Australian monsoons during boreal summer. Atmos Sci Lett 18:403–408
Chen Y, Li Y, Qi D (2011) Variations of South Asia High and West Pacific Subtropical High and their relationships with precipitation. Plateau Meteor 30(5):1148–1157 (Chinese)
Chen Z, Wen Z, Wu R et al (2014) Influence of two types of El Niño on the East Asian climate during boreal summer: a numerical study. Clim Dyn 43(1):469–481
Decker M, Zeng X (2009) Impact of modified Richards equation on global soil moisture simulation in the Community Land Model (CLM3. 5). J Adv Model Earth Syst 1(3):1–22
Dee DP, Uppala SM, Simmons AJ et al (2011) The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Q J R Meteorol Soc 137(656):553–597
Dickinson RE, Hendersonsellers A, Kennedy J(1993) Biosphere- atmosphere transfer scheme (BATS) version 1e as coupled to the NCAR community climate model. NCAR Tech. Note
Duan C, Zhu Y, You W (2007) Characteristic and formation cause of drought and flood in Yunnan province rainy season. Plateau Meteor 26(2):402–408 (Chinese)
Feng L, Li T, Yu W (2014) Cause of severe droughts in Southwest China during 1951–2010. Clim Dyn 43:7–8
Findlater J (1969) A major low-level air currents near the Indian Ocean during the northern summer. Q J R Meteorol Soc 95(2):362–380
Fritsch JM, Chappell CF (1980) Numerical prediction of convectively driven mesoscale pressure systems. Part I. Convective parameterization. J Atmos Sci 37(3):1722–1733
Gill AE (1980) Some simple solutions for heat-induced tropical circulation. Q J R Meteorol Soc 106(449):447–462
Giorgi F, Coppola E, Solmon F et al (2012) RegCM4: model description and preliminary tests over multiple CORDEX domains. Clim Res 52(1):7–29
Giorgi F, Coppola E, Raffaele F et al (2014) Changes in extremes and hydroclimatic regimes in the CREMA ensemble projections. Clim Change 125(1):39–51
Grell G (1993) Prognostic evaluation of assumptions used by cumulus parameterizations. Mon Weather Rev 121(3):764–787
Guan Z, Jin D (2013) Two opposite extreme events in seasonal mean winter rainfall over East China during the past three decades. Atmos Ocean Sci Lett 6(5):240–247
Guan Z, Lin C (1989) Some characteristics of circulation over middle and low latitudes of eastern hemisphere during anomalous droughts and floods in 1981 and 1983. Sci Meteorol Sin 9(1):80–85 (Chinese)
Guan Z, Yamagata T (2003) The unusual summer of 1994 in East Asia, IOD teleconnections. Geophys Res Lett 30(10):1544
Guan Z, Ashok K, Yamagata T (2003) Summertime response of the tropical atmosphere to the Indian Ocean sea surface temperature anomalies. J Meteorol Soc Jpn 81(3):533–561
Hamada J, Yamanaka M, Matsumoto J et al (2002) Spatial and temporal variations of the rainy season over Indonesia and their link to ENSO. J Meteorol Soc Jpn 80(2):285–310
Hamada J, Yamanaka M, Mori S et al (2008) Differences of rainfall characteristics between coastal and interior areas of central western Sumatera, Indonesia. J Meteorol Soc Jpn 86(5):593–611
Hasumi H, Emori S (eds) (2004) K-1 coupled model (MIROC) description, K-1 technical report 1, Center for Climate System Research, University of Tokyo
He J, Wen M, Ding Y et al (2006) Possible Mechanism of The Effect of Convection over Asian-Australian “Land Bridge” on the East Asian Summer Monsoon Onset. Sci China Earth Sci 49(11):1223–1232 (Chinese)
Holtslag A, Bruijn E, Pan HL (1990) A high resolution air mass transformation model for short-range weather forecasting. Mon Weather Rev 118:1561–1575
Huang R, Yan B (1987) The physical effects of topography and heat sources on the formation and maintenance of the summer monsoon over Asia. Adv Atmos Sci 4(1):13–23
Huang H, Li Q, Gao Y et al (2011) Diagnosis of the Severe Drought in Autumn/Winter 2009-2010 in Yunnan Province. Trop Geogr 31(1):28–33 (Chinese)
Huang R, Liu Y, Wang L (2012) Analyses of the causes of severe drought occurring in Southwest China from the fall of 2009 to the spring of 2010. Chin J Atmos Sci 36(3):443–457 (Chinese)
Huang X, Guan Z, Dai Z et al (2013) A further look at the interannual variations of East Asian trough intensity and their impacts on winter climate of China. Acta Meteorol Sin 71(3):416–428 (Chinese)
Hung CW, Yanai M (2004) Factors contributing to the onset of the Australian summer monsoon. Q J R Meteorol Soc 130(597):739–761
Hurrell JW, Holland MM, Gent PR et al (2013) The community earth system model, a framework for collaborative research. Bull Am Meteorol Soc 94(9):1339–1360
Jiang X, Li Y, Li C et al (2007) Characteristics of summer water vapor transportation in Sichuan Basin and its relationship with regional drought and flood. Plateau Meteor 26(3):476–484 (Chinese)
Jiang L, Guan Z, Lu C et al (2009) Interdecadal characters of relationships of the interannual variability of East Asian Summer Monsoon with IOD and ENSO. J Nanjing Inst Meteorol 32(1):32–44 (Chinese)
Jin D, Guan Z, Tang W (2013) The extreme drought event during winter–spring of 2011 in east china, combined influences of teleconnection in mid- high- latitudes and thermal forcing in maritime continent region. J Clim 26(20):8210–8222
Jin D, Guan Z, Huo L et al (2017) Possible impacts of spring sea surface temperature anomalies over South Indian Ocean on summer rainfall in Guangdong-Guangxi region of China. Clim Dyn 49:3075–3090
Kajikawa Y, Yasunari T, Kawamura R (2003) The role of the local Hadley circulation over the western Pacific on the zonally asymmetric anomalies over the Indian Ocean. J Meteorol Soc Jpn 81(2):259–276
Kiehl J, Hack J, Bonan G et al (1993) Description of the NCAR community climate model (CCM3). NCAR Tech Note 11(2):55–60
Kumar A, Hoerling MP (1995) Prospects and limitations of seasonal atmospheric GCM predictions. Bull Am Meteorol Soc 76(3):335–345
Lau KM, Chan PH (1983a) Short-term climate variability and atmospheric teleconnections from satellite-observed outgoing longwave radiation. Part I: simultaneous relationships. J Atmos Sci 40(12):2735–2750
Lau KM, Chan PH (1983b) Short–term climate variability and atmospheric teleconnections from satellite-observed outgoing longwave radiation, Part II: lagged correlations. J Atmos Sci 40(12):2735–2750
Lawrence DM, Oleson KW, Flanner MG et al (2011) Parameterization improvements and functional and structural advances in version 4 of the Community Land Model. J Adv Model Earth Syst 3(1):265–375
Lawrence DM, Oleson KW, Flanner MG et al (2012) The CCSM4 land simulation, 1850–2005: assessment of surface climate and new capabilities. J Clim 25(7):2240–2260
Li YH, Xu HM, Liu D (2006) Feature of the extremely severe drought in the east of Southwest China and anomalies of atmospheric circulation in summer 2006. Acta Meteorol Sin 67(1):122–132 (Chinese)
Li X, Liang W, Wen Z (2010) Characteristics of the atmospheric water vapor and its relationship with rainfall in South China in northern autumn, winter and spring. J Trop Meteorol 26(5):626–632 (Chinese)
Liebmann B, Smith C (1996) Description of a complete (interpolated) outgoing longwave radiation dataset. Bull Am Meteorol Soc 77(6):1275–1277
Liu Y, Xu H, Lei Z (2009) Possible causes for drought in Sichuan-Chongqing region in summer 2006. Trans Atmos Sci 32(5):686–694 (Chinese)
Lv J, Ju J, Ren J et al (2012) The influence of the Madden-Julian Oscillation activity anomalies on Yunnan’s extreme drought of 2009-2010. Sci China Earth Sci 55(1):98–112 (Chinese)
Matsumoto J, Murakami T (2002) Seasonal migration of monsoons between the Northern and Southern Hemisphere as revealed from equatorially symmetric and asymmetric OLR data. J Meteorol Soc Jpn 80(3):419–437
Matsumoto J, Murakami T, Jun M et al (2000) Annual changes of tropical convective activities as revealed from equatorial symmetric OLR data. J Meteorol Soc Jpn 78(5):543–561
McBride J (1998) Indonesia, Papua New Guinea, and tropical Australia, the southern hemisphere monsoon. Meteorology of the Southern Hemisphere. Am Meteorol Soc 49:89–99
McBride J, Haylock M, Nicholls N (2003) Relationships between the Maritime Continent heat source and the El Nin˜o–Southern Oscillation phenomenon. J Clim 16:2905–2914
Meehl G (1987) The annual cycle and interannual variability in the tropical Pacific and Indian Ocean regions. Mon Weather Rev 115(1):27–50
Neale R, Slingo J (2003) The Maritime Continent and its role in the global climate, A GCM Study. J Clim 16:834–848
Nitta Tsuyoshi (1987) Convective activities in the tropical western Pacific and their impact on the Northern Hemisphere summer circulation. J Meteorol Soc Jpn 65(3):373–390
Pal JS, Small EE, Eltahir E (2000) Simulation of regional-scale water and energy budgets: representation of subgrid cloud and precipitation processes within RegCM. J Geophys Res Atmos 105(D24):29579–29594
Qi D, Li Y, Li Y et al (2010) Variation of atmospheric heat source over east of the T-P in summer and its influence on climate of surrounding region. J Arid Meteor 28(2):113–120 (Chinese)
Qian D, Guan Z, Tang W (2018) Joint Impacts of SSTA in tropical Pacific and Indian Oceans on Variations of WPSH. J Meteorol Res 32(4):548–559
Ramage CS (1968) Role of a tropical “Maritime Continent” In the atmospheric circulation. Mon Weather Rev 96(6):365–370
Reynolds RW, Rayner NA, Smith TM et al (2002) An improved in situ and satellite SST analysis for climate. J Clim 15:1609–1625
Ropelewski CF, Halpert MS (1987) Global and regional scale precipitation patterns associated with the El Nino/Southern Oscillation. Mon Weather Rev 115:1606–1626
Saji NH, Goswami BN, Vinayachandran PN et al (1999) A dipole mode in the tropical Indian ocean. Nature 401(6751):360–363
Sardeshmukh PD, Hoskins BJ (1988) The generation of global rotational flow by steady, 598 idealized tropical divergence. J Atmos Sci 45:1228–1251
Sardeshmukh PD, Compo GP, Penland C (2000) Changes of probability associated with El Niño. J Clim 13:4268–4286
Song D, Guan Z, Tang W (2011) Variations of OLR in Maritime Continent regions in association with droughts and floods in the upper and middle reaches of Yangtze River of China in boreal summer. J Trop Meteorol 27(4):560–568 (Chinese)
Takaya K (2001) A formulation of a phase-independent wave-activity flux for stationary and migratory quasi-geostrophic eddies on a zonally varying basic flow. J Atmos Sci 58(6):608–627
Takaya K, Nakamura H (1997) A formulation of a wave-activity flux for stationary Rossby waves on a zonally varying basic flow. Geophys Res Lett 24(23):2985–2988
Tao S, Chen L (1987) A review of recent research on the East Asian summer monsoon in China. Monsoon Meteorology. Oxford University Press, London, pp 60–92
Tao S, Zhu F (1964) The 100-Mb flow patterns in Southern Asia in summer and its relation to the advance and retreat of the West Pacific subtropical anticyclone over the far east. Acta Meteorol Sin 34(4):385–396 (Chinese)
Wang B, Li Y (2010) Relationship analysis between south branch trough and severe drought of Southwest China during autumn and winter 2009/2010. Plateau Mt Meteor Res 30(4):26–35 (Chinese)
Wang B, Lin H (2002) Rainy season of the Asian–Pacific summer monsoon. J Clim 15(4):386–398
Wang XM, Zhou SW, Zhou B (2012) Causative analysis of continuous drought in Southwest China from autumn 2009 to Spring 2010. Meteorol Month 38(11):1399–1407
Wang J, Wen Z, Wu R et al (2016) The mechanism of growth of the low-frequency East Asia-Pacific teleconnection and the triggering role of tropical intraseasonal oscillation. Clim Dyn 46(11):3965–3977
Wang M, Guan Z, Jin D (2017) Two new sea surface temperature anomalies indices for capturing the eastern and central equatorial Pacific type El Niño-Southern Oscillation events during boreal summer. Int J Climatol 2018:1–11
Xia Y, Guan Z, Sun Y (2015) Interannual variations of OLR in maritime continent in late autumn and early winter and their relationships with precipitation anomalies over Yunnan-Kweichow Plateau. Acta Meteorol Sin 73(4):725–736 (Chinese)
Xia Y, Wan X, Yan X et al (2016) Variations of spring precipitation over Southwest China and circulation characteristics about its anomaly. Acta Meteorol Sin 74(4):510–524 (Chinese)
Xu Q, Guan Z (2017) Interannual variability of summertime outgoing longwave radiation over the Maritime Continent in relation to East Asian summer monsoon anomalies. J Meteorol Res 31(4):35–47
Xu Q, Guan Z, Jin D, Hu D (2019) Regional characteristics of interannual variability of summer rainfall in the Maritime Continent and their related anomalous circulation patterns. J Clim 32:4179–4192. https://doi.org/10.1175/JCLI-D-18-0480.1
Yang S, Lau KM, Kim KM (2002) Variations of the East Asian jet stream and Asian–Pacific–American winter climate anomalies. J. Clim 15:306–325
Yang J, Wang C, Lei Y (2013) Development and structure characteristic of southwest heat low in spring. Meteor Mon 39(2):146–155 (Chinese)
Zeng X, Zhao M, Dickinson RE (1998) Inter-comparison of bulk aerodynamic algorithms for the computation of sea surface fluxes using TOGA-coare and TAO data. J Clim 11:2628–2644
Zhang C, Hagos SM (2009) Bi–modal structure and variability of large-scale diabatic heating in the tropics. J Atmos Sci 66(12):3621–3640
Zhang W, Jin F, Zhao J et al (2013) The possible influence of a nonconventional el niño on the severe autumn drought of 2009 in southwest china. J Clim 26(21):8392–8405
Zhang Y, Fan G, Zhou D (2014) Variation of springtime southern branch trough and its relationship with precipitation and atmospheric circulation. Plateau Meteor 33(1):97–105 (Chinese)
Acknowledgements
This work is supported by the project of Natural Science Foundation of China (No. 41330425). NCEP/NCAR re-analyses are downloaded from the website of NOAA Earth System Research Laboratory (http://www.esrl.noaa.gov/). NOAA_OI_SST_V2 data provided by the NOAA/OAR/ESRL PSD, Boulder, Colorado, USA, from their Web site at https://www.esrl.noaa.gov/psd/. Figures are plotted using both Grads and NCL software packages.
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Xia, Y., Guan, Z. & long, Y. Relationships between convective activity in the Maritime Continent and precipitation anomalies in Southwest China during boreal summer. Clim Dyn 54, 973–986 (2020). https://doi.org/10.1007/s00382-019-05039-x
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DOI: https://doi.org/10.1007/s00382-019-05039-x