Abstract
The Maritime Continent (MC) is characterized by a seasonal evolution of rainfall distinct from other regions, due to its unique land–sea distribution and topography. In this study, the roles of surface properties and terrains in controlling the regional climatological rainfall were investigated, based on general circulation model experiments. Results show that the existence of terrain can increase the MC land (MCL) rainfall mainly through its dynamical lifting effect, but otherwise has only moderate influence on rainfall over the MC ocean (MCO). On the other hand, the impact of MC land–sea distribution on the regional rainfall is more seasonally dependent. When replacing the MC flat-land with ocean, rainfall is significantly increased over both MCL and MCO during boreal summer-to-fall, but not in the winter-to-spring season. Further inspection showed that by eliminating the MC flat-land, there is enhanced atmospheric water vapor and convective instability in the summer-to-fall period, contributing to a dramatic increase in precipitation. On the other hand, changes in convective instability and atmospheric water vapor over the MCL act to counteract each other, leading to an only moderate change in rainfall during boreal winter-to-spring. The model-based results suggest that this seasonally dependent influence of the MC flat-land on regional climate mean rainfall is not determined by its modulation on the diurnal cycle. Our results also suggest a larger sensitivity of model bias in representing land–sea distribution/fraction over the MC region during the dry season (i.e. boreal summer) than in the wet season (i.e. boreal winter).
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References
Adler RF, Huffman GJ, Chang A, Ferraro R, Xie P-P, Janowiak J, Rudolf B, Schneider U, Curtis S, Bolvin D, Gruber A, Susskind J, Arkin P, Nelkin E (2003) The version 2 global precipitation climatology project (GPCP) monthly precipitation analysis (1979–present). J Hydrometeor 4:1147–1167. https://doi.org/10.1175/1525-7541(2003)004%3c1147:TVGPCP%3e2.0.CO;2
Aldrian E, Susanto D (2003) Identification of three dominant rainfall regions within Indonesia and their relationship to sea surface temperature. Int J Climator 23:1435–1452. https://doi.org/10.1002/joc.950
Aldrian E, Dümenil Gates L, Widodo FH (2007) Seasonal variability of Indonesian rainfall in ECHAM4 simulations and in the reanalyses: the role of ENSO. Theor App Climator 87:41–59. https://doi.org/10.1007/s00704-006-0218-8
Chang C-P, Wang Z, McBride J, Liu C (2005a) Annual cycle of southeast Asia-maritime continent rainfall and the asymmetric monsoon transition. J Clim 18:287–301. https://doi.org/10.1175/JCLI-3257.1
Chang C-P, Harr PA, Chen H-J (2005b) Synoptic disturbances over the equatorial South China Sea and western Maritime Continent during boreal winter. Mon Weather Rev 133:489–503. https://doi.org/10.1175/mwr-2868.1
Chen T-C, Tsay J-D, Matsumoto J, Alpert J (2015a) Development and formation mechanism of the southeast Asian winter heavy rainfall events around the South China Sea. Part I: formation and propagation of cold surge vortex. J Clim 28:1417–1443. https://doi.org/10.1175/jcli-d-14-00170.1
Chen T-C, Tsay J-D, Matsumoto J (2015b) Development and formation mechanism of the southeast Asian winter heavy rainfall events around the South China Sea. Part II: multiple interactions. J Clim 28:1444–1464. https://doi.org/10.1175/jcli-d-14-00171.1
Ciesielski PE, Johnson RH (2006) Contrasting characteristics of convection over the northern and southern South China Sea during SCSMEX. Mon Weather Rev 134:1041–1062. https://doi.org/10.1175/mwr3113.1
Cronin TW, Emanuel KA, Molnar P (2015) Island precipitation enhancement and the diurnal cycle in radiative-convective equilibrium. Q J R Meteorol Soc 141:1017–1034. https://doi.org/10.1002/qj.2443
Gesch DB, Verdin KL, Greenlee SK (1999) New land surface digital elevation model covers the Earth. Eos Earth Sp Sci News 80:69–70. https://doi.org/10.1029/99EO00050
Gianotti RL, Zhang D, Eltahir EAB (2012) Assessment of the regional climate model version 3 over the MC using different cumulus parameterization and land surface schemes. J Clim 25:638–656. https://doi.org/10.1175/jcli-d-11-00025.1
Haarsma RJ, Roberts MJ, Vidale PL, Senior CA, Bellucci A, Bao Q, Chang P, Corti S, Fučkar NS, Guemas V, von Hardenberg J, Hazeleger W, Kodama C, Koenigk T, Leung LR, Lu J, Luo JJ, Mao J, Mizielinski MS, Mizuta R, Nobre P, Satoh M, Scoccimarro E, Semmler T, Small J, von Storch JS (2016) High resolution model intercomparison project (HighResMIP v1.0) for CMIP6. Geosci Model Dev 9:4185–4208. https://doi.org/10.5194/gmd-9-4185-2016
Hamada J-I, Yamanaka MD, Matsumoto J, Fukao S, Winarso PA, Sribimawati T (2002) Spatial and temporal variations of the rainy season over Indonesia and their link to ENSO. J Meteorol Soc Jpn 80:285–310. https://doi.org/10.2151/jmsj.80.285
Hara M, Yoshikane T, Takahashi HG, Kimura F, Noda A, Tokioka T (2009) Assessment of the diurnal cycle of precipitation over the MC simulated by a 20 km Mesh GCM using TRMM PR data. J Meteorol Soc Jpn 87A:413–424. https://doi.org/10.2151/jmsj.87A.413
Haylock M, McBride J (2001) Spatial coherence and predictability of Indonesian wet season rainfall. J Clim 14:3882–3887. https://doi.org/10.1175/1520-0442(2001)014%3c3882:SCAPOI%3e2.0.CO;2
Hendon HH (2003) Indonesian rainfall variability: impacts of ENSO and local air–sea interaction. J Clim 16:1775–1790. https://doi.org/10.1175/1520-0442(2003)016%3c1775:IRVIOE%3e2.0.CO;2
Holland GJ, Keenan TD (1980) Diurnal variations of convection over the “MC”. Mon Weather Rev 108:223–225. https://doi.org/10.1175/1520-0493(1980)108%3c0223:DVOCOT%3e2.0.CO;2
Huffman GJ, Bolvin DT, Nelkin EJ, Wolff DB, Adler RF, Gu G, Hong Y, Bowman KP, Stocker EF (2007) The TRMM Multisatellite Precipitation Analysis (TMPA): quasi-global, multiyear, combined-sensor precipitation estimates at fine scales. J Hydrometeor 8:38–55. https://doi.org/10.1175/JHM560.1
Hung C-W, Liu X, Yanai M (2004) Symmetry and asymmetry of the Asian and Australian summer monsoons. J Clim 17:2413–2426. https://doi.org/10.1175/1520-0442(2004)017%3c2413:Saaota%3e2.0.Co;2
Hurrell JW, Hack JJ, Shea D, Caron JM, Rosinski J (2008) A new sea surface temperature and sea ice boundary dataset for the community atmosphere model. J Clim 21:5145–5153. https://doi.org/10.1175/2008JCLI2292.1
Hurrell JW, Holland MM, Gent PR et al (2013) The community earth system model: a framework for collaborative research. Bull Am Meteorol Soc 94:1339–1360. https://doi.org/10.1175/BAMS-D-12-00121.1
Im E-S, Eltahir EAB (2018) Simulation of the diurnal variation of rainfall over the western MC using a regional climate model. Clim Dyn 51:73–88. https://doi.org/10.1007/s00382-017-3907-3
Jiang X, Yang S, Li Y, Kumar A, Wang W, Gao Z (2013) Dynamical prediction of the East Asian winter monsoon by the NCEP climate forecast system. J Geophys Res 118:1312–1328. https://doi.org/10.1002/jgrd.50193
Kida S, Richards KJ (2009) Seasonal sea surface temperature variability in the Indonesian Seas. J Geophys Res Oceans 114:C06016. https://doi.org/10.1029/2008JC005150
Kim H-M, Kim D, Vitart F, Toma VE, Kug J-S, Webster PJ (2016) MJO propagation across the maritime continent in the ECMWF ensemble prediction system. J Clim 29:3973–3988. https://doi.org/10.1175/jcli-d-15-0862.1
Lau K-M, Chan PH (1983a) Short-term climate variability and atmospheric teleconnections from satellite-observed outgoing oongwave radiation. Part I: Simultaneous relationships. J Atmos Sci 40:2735–2750. https://doi.org/10.1175/1520-0469(1983)040%3c2735:Stcvaa%3e2.0.Co;2
Lau K-M, Chan PH (1983b) Short-term climate variability and atmospheric teleconnections from satellite-observed outgoing oongwave radiation. Part II: Lagged correlations. J Atmos Sci 40:2751–2767. https://doi.org/10.1175/1520-0469(1983)040%3c2751:Stcvaa%3e2.0.Co;2
Li Y, Jourdain NC, Taschetto AS, Gupta AS, Argüeso D, Masson S, Cai W (2017) Resolution dependence of the simulated precipitation and diurnal cycle over the MC. Clim Dyn 48:4009–4028. https://doi.org/10.1007/s00382-016-3317-y
Li Y, Yang S, Deng Y, Hu X, Cai M (2018) A process-level attribution of the annual cycle of surface temperature over the Maritime Continent. Clim Dyn 51:2759–2772. https://doi.org/10.1007/s00382-017-3975-4
Love BS, Matthews AJ, Lister GMS (2011) The diurnal cycle of precipitation over the MC in a high-resolution atmospheric model. Q J R Meteorol Soc 137:934–947. https://doi.org/10.1002/qj.809
Lui YS, Tam C-Y, Au-Yeung YM, Lau N-C (2018) Role of cumulus parameterization scheme on the diurnal cycle of precipitation over Southeast Asia in RegCM4. Clim Dyn. https://doi.org/10.1007/s00382-018-4517-4
Mapes BE, Warner TT, Xu M (2003) Diurnal patterns of rainfall in northwestern South America. Part III: Diurnal gravity waves and nocturnal convection offshore. Mon Weather Rev 131:830–844. https://doi.org/10.1175/1520-0493(2003)131%3c0830:Dporin%3e2.0.Co;2
Matsumoto J (1992) The seasonal changes in Asian and Australian monsoon regions. J Meteorol Soc Jpn 70:257–273
McBride JL, Haylock MR, Nicholls N (2003) Relationships between the Maritime Continent heat source and the El Niño-Southern Oscillation phenomenon. J Clim 16:2905–2914. https://doi.org/10.1175/1520-0442(2003)016%3c2905:RBTMCH%3e2.0.CO;2
Mori S, Jun-Ichi H, Tauhid YI, Yamanaka MD, Okamoto N, Murata F, Sakurai N, Hashiguchi H, Sribimawati T (2004) Diurnal land–sea rainfall peak migration over Sumatera Island, Indonesian Maritime Continent, observed by TRMM satellite and intensive rawinsonde soundings. Mon Weather Rev 132:2021–2039. https://doi.org/10.1175/1520-0493(2004)132%3c2021:Dlrpmo%3e2.0.Co;2
Neale R, Slingo J (2003) The MC and its role in the global climate: a GCM study. J Clim 16:834–848. https://doi.org/10.1175/1520-0442(2003)016%3c0834:Tmcair%3e2.0.Co;2
Nesbitt SW, Zipser EJ (2003) The diurnal cycle of rainfall and convective intensity according to 3 years of TRMM measurements. J Clim 16:1456–1475. https://doi.org/10.1175/1520-0442-16.10.1456
Nguyen H, Franklin C, Protat A (2017) Understanding the ACCESS model errors over the MC using CloudSat and CALIPSO simulators. Q J R Meteorol Soc 143:3136–3152. https://doi.org/10.1002/qj.3168
Oh J-H, Kim K-Y, Lim G-H (2012) Impact of MJO on the diurnal cycle of rainfall over the western Maritime Continent in the austral summer. Clim Dyn 38:1167–1180. https://doi.org/10.1007/s00382-011-1237-4
Peatman SC, Matthews AJ, Stevens DP (2015) Propagation of the Madden–Julian oscillation and scale interaction with the diurnal cycle in a high-resolution GCM. Clim Dyn 45 (9–10):2901–2918. https://doi.org/10.1007/s00382-015-2513-5
Qian J-H (2008) Why precipitation is mostly concentrated over islands in the MC. J Atmos Sci 65:1428–1441. https://doi.org/10.1175/2007jas2422.1
Qian J-H, Robertson AW, Moron V (2010) Interactions among ENSO, the monsoon, and diurnal cycle in rainfall variability over Java, Indonesia. J Atmos Sci 67:3509–3524. https://doi.org/10.1175/2010jas3348.1
Ramage CS (1968) Role of a tropical “Maritime Continent” in the atmospheric circulation. Mon Weather Rev 96:365–369. https://doi.org/10.1175/1520-0493(1968)096%3c0365:ROATMC%3e2.0.CO;2
Rashid HA, Hirst AC (2017) Mechanisms of improved rainfall simulation over the MC due to increased horizontal resolution in an AGCM. Clim Dyn 49:1747–1764. https://doi.org/10.1007/s00382-016-3413-z
Remote Sensing Systems (2016) Monthly mean total precipitable water data set on a 1 degree grid made from Remote Sensing Systems Version-7 Microwave Radiometer Data, V07r01. Santa Rosa, CA, USA. http://www.remss.com
Ren H-L, Wu J, Zhao C-B, Cheng Y-J, Liu X-W (2016) MJO ensemble prediction in BCC-CSM1.1(m) using different initialization schemes. Atmos Ocean Sci Lett 9:60–65. https://doi.org/10.1080/16742834.2015.1116217
Saha S, Moorthi S, Pan H-L, Wu X, Wang J, Nadiga S, Tripp P, Kistler R, Woollen J, Behringer D, Liu H, Stokes D, Grumbine R, Gayno G, Wang J, Hou Y-T, Chuang H-Y, Juang H-MH, Sela J, Iredell M, Treadon R, Kleist D, Delst PV, Keyser D, Derber J, Ek M, Meng J, Wei H, Yang R, Lord S, Dool HVD, Kumar A, Wang W, Long C, Chelliah M, Xue Y, Huang B, Schemm J-K, Ebisuzaki W, Lin R, Xie P, Chen M, Zhou S, Higgins W, Zou C-Z, Liu Q, Chen Y, Han Y, Cucurull L, Reynolds RW, Rutledge G, Goldberg M (2010) The NCEP Climate Forecast System reanalysis. Bull Am Meteorol Soc 91:1015–1057. https://doi.org/10.1175/2010BAMS3001.1
Sato T, Miura H, Satoh M, Takayabu YN, Wang Y (2009) Diurnal cycle of precipitation in the tropics simulated in a global cloud-resolving model. J Clim 22:4809–4826. https://doi.org/10.1175/2009jcli2890.1
Skamarock WC, Klemp JB, Dudhia J, Gill DO, Barker DM, Duda MG, Huang X-Y, Wang W (2008) A description of the advanced research WRF version 3. Technical Report (June) 113
Skamarock WC, Klemp JB, Duda MJ, Fowler L, Park S-H, Ringler TD (2012) A multi-scale nonhydrostatic atmospheric model using centroidal voronoi tesselations and C-grid staggering. Mon Weather Rev 240:3090–3105. https://doi.org/10.1175/MWR-D-11-00215.1
Slingo JM, Sperber KR, Boyle JS, Ceron JP, Dix M, Dugas B, Ebisuzaki W, Fyfe J, Gregory D, Gueremy JF, Hack J, Harzallah A, Inness P, Kitoh A, Lau WK-M, McAvaney B, Madden R, Matthews A, Palmer TN, Parkas CK, Randall D, Renno N (1996) Intraseasonal oscillations in 15 atmospheric general circulation models: results from an AMIP diagnostic subproject. Clim Dyn 12:325–357
Sobel AH, Burleyson CD, Yuter SE (2011) Rain on small tropical islands. J Geophys Res Atmos 116:D08102. https://doi.org/10.1029/2010JD014695
Tan H, Ray P, Barrett BS, Tewari M, Moncrieff MW (2018) Role of topography on the MJO in the maritime continent: a numerical case study. Clim Dyn. https://doi.org/10.1007/s00382-018-4275-3
Taylor KE, Stouffer RJ, Meehl GA (2012) An overview of CMIP5 and the experiment design. Bull Am Meteorol Soc 93:485–498. https://doi.org/10.1175/BAMS-D-11-00094.1
Toh YY, Turner AG, Johnson SJ, Holloway CE (2018) MC seasonal climate biases in AMIP experiments of the CMIP5 multimodel ensemble. Clim Dyn 50:777–800. https://doi.org/10.1007/s00382-017-3641-x
Wang S, Sobel AH (2017) Factors controlling rain on small tropical islands: diurnal cycle, large-scale wind speed, and topography. J Atmos Sci 74:3515–3532. https://doi.org/10.1175/JAS-D-16-0344.1
Webster PJ, Clayson CA, Curry JA (1996) Clouds, radiation, and the diurnal cycle of the sea surface temperature in the tropical western Pacific. J Clim 9:1712–1730. https://doi.org/10.1175/1520-0442(1996)009%3c1712:cratdc%3e2.0.co;2
Wu R, Hu Z-Z, Kirtman BP (2003) Evolution of ENSO-related rainfall anomalies in East Asia. J Clim 16:3742–3758. https://doi.org/10.1175/1520-0442(2003)016%3c3742:EOERAI%3e2.0.CO;2
Xie P, Arkin PA (1997) Global rainfall: a 17-year monthly analysis based on gauge observations, satellite estimates, and numerical model outputs. Bull Am Meteorol Soc 78:2539–2558. https://doi.org/10.1175/1520-0477(1997)078%3c2539:GPAYMA%3e2.0.CO;2
Yang G-Y, Slingo J (2001) The diurnal cycle in the Tropics. Mon Weather Rev 129:784–801. https://doi.org/10.1175/1520-0493(2001)129%3c0784:Tdcitt%3e2.0.Co;2
Zhang T, Yang S, Jiang X, Zhao P (2016a) Seasonal-interannual variation and prediction of wet and dry season rainfall over the Maritime Continent: roles of ENSO and monsoon circulation. J Clim 29:3675–3695. https://doi.org/10.1175/JCLI-D-15-0222.1
Zhang T, Yang S, Jiang X, Huang B (2016b) Roles of remote and local forcings in the variation and prediction of regional Maritime Continent rainfall in wet and dry Seasons. J Clim 29:8871–8879. https://doi.org/10.1175/JCLI-D-16-0417.1
Zhang T, Yang S, Jiang X, Dong S (2016c) Sub-seasonal prediction of the MC rainfall of wet-dry transitional seasons in the NCEP Climate Forecast Version 2. Atmosphere 7:28. https://doi.org/10.3390/atmos7020028
Zhang T, Huang B, Yang S, Chen J, Jiang X (2018) Dynamical and thermodynamical influences of the Maritime Continent on ENSO evolution. Sci Rep 8:15352. https://doi.org/10.1038/s41598-018-33436-5
Zhu J, Huang B, Kumar A, Kinter JL III (2015) Seasonality in prediction skill and predictable pattern of tropical Indian Ocean SST. J Clim 28:7962–7984. https://doi.org/10.1175/JCLI-D-15-0067.1
Acknowledgements
The authors thank the anomalous reviewers for their constructive comments on an earlier version of the manuscript. This study was jointly supported by the Vice-Chancellor’s Discretionary Fund of The Chinese University of Hong Kong (4930744), and the National Natural Science Foundation of China (Grant 41661144019). The appointment of Ngar-Cheung Lau at The Chinese University of Hong Kong is partially supported by the AXA Research Fund.
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Zhang, T., Tam, CY., Jiang, X. et al. Roles of land-surface properties and terrains on Maritime Continent rainfall and its seasonal evolution. Clim Dyn 53, 6681–6697 (2019). https://doi.org/10.1007/s00382-019-04951-6
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DOI: https://doi.org/10.1007/s00382-019-04951-6