Ananthakrishnan R, Srinivasan V, Ramakrishna A R, et al. 1968. Synoptic features associated with onset of southwest monsoon over Kerala. Forcasting Manual, IV-18.2, India Meteorological Department
[5]
Chang C P, Harr P, Ju J. 2001. Possible roles of Atlantic circulations on the weakening Indian monsoon rainfall-ENSO relationship. J Clim, 14: 2376-2380
[6]
Fasullo J, Webster P J. 2003. A hydrological definition of Indian Monsoon onset and withdrawal. J Clim, 16: 3200-3211
[7]
Gadgil S. 2003. The Indian monsoon and its variability. Annu Rev Earth Planet Sci, 31: 429-467
[8]
Gadgil S, Rajeevan M, Zubair L, et al. 2011. South Asian Monsoon: Interannual variation. In: Chang C P, Ding Y H, Lau N C, et al, eds. The Global Monsoon System: Research and Forecast. 2nd ed. New York: World Scientific. 25-42
[9]
Goswami B N. 2005a. South Asian summer monsoon: An overview. In: Chang C P, Wang B, Lau N C, et al, eds. The Global Monsoon System: Research and Forecast. 2nd ed. New York: World Scientific. 47-71
[10]
Goswami B N. 2005b. South Asian monsoon. In: Lau K M, Waliser D E, eds. Intraseasonal Variability in the Atmosphere-Ocean Climate System. London: Springer. 19-61
[11]
Huffman G J, Adler R F, Rudolf B, et al. 1995. Global precipitation estimates based on a technique for combining satellite-based estimates, rain gauge analysis, and NWP model precipitation information. J Clim, 8: 1284-1295
[12]
Hoskins P J, Mclntyre M E, Robertson A W. 1985. On the use of significance of isentropic potential vorticity maps. Q J R Meteorol Soc, 111: 877-946
[13]
Joseph P V, Eischeid J K, Pyle R J. 1994. Interannual variability of the onset of the Indian summer monsoon and its association with atmospheric features, El Ni?o, and sea surface temperature anomalies. J Clim, 7: 81-105
[14]
Joseph P V, Sooraj K P, Rajan C K. 2006. The summer monsoon onset process over South Asia and an objective method for the date of monsoon onset over Kerala. Int J Climatol, 26: 1871-1893
[15]
Kalnay E, Kanamitsu M, Kistler R, et al. 1996. The NCEP/NCAR 40-year reanalysis project. Bull Amer Meteorol Soc, 77: 437-471
[16]
Krishnamurti T N, Low-Nam S, Pasch R. 1983. Cumulus parameterization and rainfall rates II. Mon Weather Rev, 111: 816-828
[17]
Lau N C, Ploshay J J. 2009. Simulation of synoptic and sub-synoptic scale phenomena associated with the East Asian Summer Monsoon using a high-resolution GCM. Mon Weather Rev, 137: 137-160
[18]
Liebmann B, Smith C A. 1996. Description of a complete (interpolated) outgoing longwave radiation dataset. Bull Amer Meteorol Soc, 77: 1275-1277
[19]
Liu B Q, Wu G X, Mao J Y, et al. 2013. Genesis of the South Asian high and its impact on the Asian Summer Monsoon onset. J Clim, 26: 2976-2991
[20]
Mao J Y, Chan J C L, Wu G X. 2004. Relationship between the onset of the South China Sea summer monsoon and the structure of the Asian subtropical anticyclone. J Meteorol Soc Jpn, 82: 845-859
[21]
Mao J Y, Wu G X. 2007. Interannual variability in the onset of the summer monsoon over the Eastern Bay of Bengal. Theor Appl Climatol, 89: 155-170
[22]
Prasad V S, Hayashi T. 2005. Onset and withdrawal of Indian summer monsoon. Geophys Res Lett, 32: L20715, doi: 10.1029/2005GL023269
[23]
Robock A M, Mu M Q, Vinnikov K, et al. 2003. Land surface conditions over Eurasia and Indian summer monsoon rainfall. J Geophys Res, 108: 4131, doi: 10.1029/2002JD002286
[24]
Saha K. 2010. Chapter 4: Monsoon over Southern Asia (comprising Pakistan, India, Bangladesh, Myanmar and Countries of Southeastern Asia) and adjoining Indian Ocean (Region-I). In: Saha K, ed. Tropical Circulation Systems and Monsoons. London: Springer. 89-121
[25]
Saha S, Saha K. 1980. A hypothesis on onset, advance and withdrawal of the Indian Summer Monsoon. Pure Appl Geophys, 118: 1066-1075
[26]
Taniguchi K, Koike T. 2006. Comparision of definitions of Indian summer monsoon onset: Better representation of rapid transitions of atmospheric conditions. Geophys Res Lett, 33: L02709, doi: 10.1029/2005GL024526
[27]
Tomas R A, Webster P J. 1997. The role of inertial instability in determining the location and strength of near-equatorial convection. Q J R Meteorol Soc, 123: 1445-1482
[28]
Tomas R A, Holton J R, Webster P J. 1999. The influence of cross-equatorial pressure gradients on the location of near-equatorial convection. Q J R Meteorol Soc, 125: 1107-1127
[29]
Wang B, Ding Q H, Joseph P V. 2009. Objective definition of the Indian summer monsoon onset. J Clim, 22: 3303-3316
[30]
Wu G X, Zhang Y S. 1998. Tibetan Plateau forcing and the timing of the monsoon onset over South Asia and the South China Sea. Mon Weather Rev, 126: 913-927
[31]
Xavier P K, Marzin C, Goswami B N. 2007. An objective definition of the Indian Summer Monsoon season and a new perspective on the ENSO-monsoon relationship. Q J R Meteorol Soc, 133: 749-764
[32]
Yang S, Lau K M, Rao M S. 1996. Precursory signals associated with the interannual variability of the Asian Summer Monsoon. J Clim, 9: 949-964
[33]
Yu L S, Jin X Z, Weller R A. 2007. Annual, seasonal, and interannual variability of air-sea heat fluxes in the Indian Ocean. J Clim, 20: 3190-3209