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  • Ananthakrishnan, R., and M. K. Soman (1988), The onset of south-west monsoon over Kerala: 1901–1980, Int. J. Climatol., 8, 283296.
  • Ananthakrishnan, R., and M. K. Soman (1989), The onset of southwest monsoon over Kerala for the period 1870-1990, Int. J. Climatol., 9, 283296.
  • Boos, W. R., and K. A. Emanuel (2009), Annual intensification of the Somali jet in a quasi-equilibrium framework: observational composites, Q. J. R. Meteorol. Soc., 135, 319335.
  • Boos, W. R., and Z.-m. Kuang (2010), Dominant control of the South Asian monsoon by orographic insulation versus plateau heating, Nature, 463, 218222.
  • Bordoni, S., and T. Schneider (2008), Monsoons as eddy-mediated regime transitions of the tropical overturning circulation, Nat. Geosci., 1, 515519.
  • Braconnot, P., O. Marti, S. Joussaume, and Y. Leclainche (2000), Ocean feedback in response to 6 kyr BP insolation, J. Climate, 13, 15371553.
  • Bryson, R. A., and A. M. Swain (1981), Holocene variations of monsoonal rainfall in Rajasthan, Quat. Res., 16, 135145.
  • Chakraborty, A., R. S. Nanjundiah, and J. Srinivasan (2002), Role of Asian and African orography in Indian summer monsoon, Geophys. Res. Lett., 29(20), 1989, doi:10.1029/2002GL015522.
  • Chakraborty, A., R. S. Nanjundiah, and J. Srinivasan (2006), Theoretical aspects of the onset of Indian summer monsoon from perturbed orography simulations in a GCM, Ann Geophys, 24, 20752089.
  • Clift, P. D., and R. A. Plumb (2008), The Asian Monsoon: Causes, History and Effects, Cambridge University Press, New York, 270.
  • Currie, B. S., D. B. Rowley, and N. J. Tabor (2005), Middle Miocene paleoaltimetry of southern Tibet: Implications for the role of mantle thickening and delamination in the Himalayan orogen, Geology, 33, 181184.
  • DeCelles, P. G., J. Quade, P. Kapp, M.-j. Fan, D. L. Dettman, and L. Ding (2007), High and dry in central Tibet during the Late Oligocene, Earth Planet. Sci. Lett., 253, 389401.
  • Emanuel, K. A. (1995), On thermally direct circulations in moist atmospheres, J. Atmos. Sci., 52, 15291534.
  • Emanuel, K. (2007), Quasi-equilibrium dynamics of the tropical atmosphere, in The Global Circulation of the Atmosphere, ed. by T. Schneider and A. H. Sobel, Princeton Univ. Press., Princeton, N.J., 186218.
  • Emanuel, K. A., J. D. Neelin, and C. S. Bretherton (1994), On large-scale circulations in convecting atmospheres, Quart. J. Roy. Meteorol. Soc, 120, 11111143.
  • Enzel, Y., L. L. Ely, S. Mishra, R. Ramesh, R. Amit, B. Lazar, S. N. Rajaguru, V. R. Baker, and A. Sandler (1999), High-resolution Holocene environmental changes in the Thar Desert, northwestern India, Science, 284, 125128.
  • Fieux, M., and H. Stommel (1977), Onset of the southwest monsoon over the Arabian Sea from marine reports of surface winds: Structure and variability, Mon. Weather Rev., 105, 231236.
  • Flohn H. (1968), Contributions to a meteorology of the Tibetan highlands, Atmospheric Science Paper 130, Colorado State University, Fort Collins, Colorado, 120.
  • Garzione, C. N., D. L. Dettman, J. Quade, P. G. DeCelles, and R. F. Butler (2000a), High times on the Tibetan Plateau: Paleoelevation of the Thakkhola graben, Nepal, Geology, 28, 339342.
  • Garzione, C. N., J. Quade, P. G. DeCelles, and N. B. English (2000b), Predicting paleoelevation of Tibet and the Himalaya from δ18O vs. altitude gradients of meteoric water across the Nepal Himalaya, Earth Planet. Sci. Lett., 183, 215229.
  • Goswami, B. N., and P. K. Xavier (2005), ENSO control on the south Asian monsoon through the length of the rainy season, Geophys. Res. Lett., 32, L18717, doi:10.1029/2005GL023216.
  • Goswami, B. N., V. Krishnamurthy, and H. Annamalai (1999), A broad scale circulation index for the interannual variability of the Indian summer monsoon, Quart. J. Roy. Meteor., 125, 611633.
  • Gupta, A. K., D. M. Anderson, and J. T. Overpeck (2003), Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean, Nature, 421, 354357.
  • Hahn, D. G., and S. Manabe (1975), The role of mountains in the south Asian monsoon circulation, J. Atmos. Sci., 32, 15151541.
  • Halpern, D., and P. M., Woiceshyn (1999), Onset of the Somali Jet in the Arabian Sea during June 1997, J. Geophys. Res., 104, 18,04118,046.
  • Harrison, T. M., P. Copeland, W. S. F. Kidd, and A. Yin (1992), Raising Tibet, Science, 255, 16631670.
  • He, H.-y., J. McGinnis, Z.-s. Song, and M. Yanai (1987). Onset of the Asian summer monsoon in 1979 and the effect of the Tibetan Plateau, Mon. Wea. Rev., 115, 19661995.
  • He, H.-y., C.-H. Sui, M.-q. Jian, Z.-p. Wen, and G.-d. Lan (2003), The evolution of tropospheric temperature field and its relationship with the onset of Asian summer monsoon, J. Meteor. Soc. Japan, 81, 12011223.
  • Held, I. M., and B. J. Soden (2006), Robust responses of the hydrological cycle to global warming, J. Climate, 19, 56755699.
  • Hoskins, B. J., and M. J. Rodwell (1995), A model of the Asian summer monsoon. Part I: The global scale, J. Atmos. Sci., 52, 13291340.
  • Hurley, J. V., and W. R. Boos (2013), Interannual variability of monsoon precipitation and subcloud equivalent potential temperature, J. Climate (in press).
  • Huybers, P. (2006), Early Pleistocene glacial cycles and the integrated summer insolation forcing, Science, 313, 508511.
  • Joseph, P. V., K. P. Sooraj, and C. K. Rajan (2006) The summer monsoon onset process over South Asia and an objective method for the date of monsoon onset over Kerala, Int. J. Climatology, 26, 18711893. Doi: 10.1002/joc.1340.
  • Kalnay, E., M. Kanamitsu, R. Kistler, W. Collins, D. Deaven, L. Gandin, M. Iredell, S. Saha, G. White, J. Woollen, Y. Zhu, A. Leetmaa, B. Reynolds, M. Chelliah, W. Ebisuzaki, W. Higgins, J. Janowiak, K. C. Mo, C. Ropelewski, J. Wang, R. Jenne, and D. Joseph (1996), The NCEP/NCAR 40-Year Reanalysis Project, Bull. Amer. Meteor. Soc., 77, 437472.
  • Kaplan, A., M. Cane, Y. Kushnir, A. Clement, M. Blumenthal, and B. Rajagopalan (1998), Analyses of global sea surface temperature 1856-1991, J. Geophys. Res., 103, 18,56718,589.
  • Kienast, M., S. S. Kienast, S. E. Calvert, T. I. Eglinton, G. Mollenhauer, R. François, and A. C. Mix (2006), Eastern Pacific cooling and Atlantic overturning circulation during the last deglaciation, Nature, 443, 846849.
  • Koutavas, A., J. Lynch-Stieglitz, T. M. Marchitto, Jr., and J. P. Sachs (2002), El Niño-like pattern in Ice Age tropical pacific sea surface temperature, Science, 297, 226230.
  • Koutavas, A., P. B. deMenocal, G. C. Olive, and J. Lynch-Stieglitz (2006), Mid-Holocene El Niño-Southern Oscillation (ENSO) attenuation revealed by individual foraminifera in eastern tropical Pacific sediments, Geology, 34, 993996.
  • Krishnamurti, T. N., P. Ardanuy, Y. Ramanathan, and R. Pasch (1981), On the onset vortex of the summer monsoon, Mon. Wea. Rev., 109, 344363.
  • Kroon, D., T. Steens, and S. R. Troelstra (1991), Onset of monsoonal related upwelling in the western Arabian Sea as revealed by planktonic foraminifers, in W. L. Prell, N. Niitsuma, et al., Proceedings of the Ocean Drilling Project, Sci. Results, vol. 117, College Station, Texas (Ocean Drilling Program), 257263.
  • Kutzbach, J. E., P. J. Guetter, W. F. Ruddiman, and W. L. Prell (1989), The sensitivity of climate to Late Cenozoic uplift in southern Asia and the American west: Numerical experiments, J. Geophys. Res., 94, 18,39318,407.
  • Kutzbach, J. E., W. L. Prell, and W. F., Ruddiman (1993), Sensitivity of Eurasian climate to surface uplift of the Tibetan Plateau, J. Geol., 101, 177190.
  • Kutzbach, J. E., W. F. Ruddiman, and W. L. Prell (1997), Possible effects of Cenozoic uplift and CO2 lowering on global and regional hydrology, in Tectonic Uplift and Climate Change, ed. by W. F., Ruddiman, 150170, Plenum, New York.
  • Leduc, G., L. Vidal, K. Tachikawa, F. Rostek, C. Sonzogni, L. Beaufort, and E. Bard (2007), Moisture transport across Central America as a positive feedback on abrupt climatic changes, Nature, 445, 908911.
  • Leduc, G., R. Schneider, J.-H. Kim, and G. Lohmann (2010), Holocene and Eemian sea surface temperature trends as revealed by alkenone and Mg/Ca paleothermometry, Quat. Sci. Rev. 29, 9891004.
  • Li, C.-f., and M. Yanai (1996), The onset and interannual variability of the Asian summer monsoon in relation to land-sea thermal contrast, J. Climate, 9, 358375.
  • Lindzen, R. S., and A. Y. Hou (1988), Hadley circulations for zonally averaged heating centered off the equator, J. Atmos. Sci., 45, 24162427.
  • Liu, Y.-m., G.-x. Wu, J.-l. Hong, B.-w. Dong, A.-m. Duan, Q. Bao, and L.-j. Zhou (2012), Revisiting Asian monsoon formation and change associated with Tibetan Plateau forcing: II. Change, Clim. Dyn., 39, 11831195.
  • Mitchell, T. D., and P. D. Jones (2005), An improved method of constructing a database of monthly climate observations and associated high-resolution grids, Int J Climatol, 25, 693712.
  • Molnar, P., and K. A. Emanuel (1999), Temperature profiles in radiative-convective equilibrium above surfaces of different heights, J. Geophys. Res., 104, 24,26524,271.
  • Molnar, P., P. England, and J. Martinod (1993), Mantle dynamics, uplift of the Tibetan Plateau, and the Indian monsoon, Rev. Geophys., 31, 357396.
  • Neelin, J. D. (2007), Moist dynamics of tropical convection zones in monsoons, teleconnections, and global warming, in The Global Circulation of the Atmosphere, edited by T., Schneider, and A. H., Sobel, Princeton Univ. Press, Princeton, N. J., 267301.
  • Nie, J., W. R. Boos, and Z.-m., Kuang (2010), Observational evaluation of a convective quasi-equilibrium view of monsoons, J. Climate, 23, 44164428.
  • Pai, D. S., and R. M. Nair (2009), Summer monsoon onset over Kerala: New definition and prediction, J. Earth Syst. Sci., 118, 123135.
  • Pahnke, K., J. P. Sachs, L. Keigwin, A. Timmermann, and S.-P. Xie (2007), Eastern tropical Pacific hydrologic changes during the past 27,000 years from D/H ratios in alkenones, Paleoceanography, 22, PA4214, doi:10.1029/2007PA001468.
  • Plumb, R. A. (2007), Dynamical constraints on monsoon circulations, in The Global Circulation of the Atmosphere, ed. by T., Schneider and A. H., Sobel, Princeton Univ. Press, Princeton, N.J., 252266.
  • Plumb, R. A., and A. Y. Hou (1992), The response of a zonally symmetric atmosphere to subtropical thermal forcing: Threshold behavior, J. Atmos. Sci., 49, 17901799.
  • Prasad, S., and Y. Enzel (2006), Holocene paleoclimates of India, Quaternary Res., 66, 442453.
  • Prasad, S., S. Kusumgar, and S. K. Gupta (1997), A mid–late Holocene record of palaeoclimatic changes from Nal Sarovar—A palaeodesert margin lake in western India, J. Quaternary Sci., 12, 153159.
  • Prell, W. L., and J. E. Kutzbach (1992), Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution, Nature, 360, 647652.
  • Prell, W. L., D. W. Murray, S. C. Clemens, and D. M. Anderson (1992), Evolution and variability of the Indian Ocean summer monsoon: Evidence from the western Arabian Sea drilling program, in Synthesis of Results from Scientific Drilling in the Indian Ocean, edited by R. A. Duncan, R. B. Kidd, U. von Rad, and J. K. Weissel, Geophysical Monograph 70, America Geophysical Union, Washington, D. C., 447469.
  • Privé, N. C., and R. A. Plumb (2007a), Monsoon dynamics with interactive forcing. Part I: Axisymmetric studies, J. Atmos. Sci., 64, 14171430.
  • Privé, N. C., and R. A. Plumb (2007b), Monsoon dynamics with interactive forcing. Part II: Impact of eddies and asymmetric geometries, J. Atmos. Sci., 64, 14311442.
  • Rajagopalan, B., and P. Molnar (2012), Pacific Ocean sea-surface temperature variability and predictability of rainfall in the early and late parts of the Indian summer monsoon season, Climate Dynamics, DOI 10.1007/s00382-011-1194-y, 39(6), 1543-1557.
  • Rajeevan, M., J. Bhate, J. D. Kale, and B. Lal (2006), High resolution daily gridded rainfall data for the Indian region: Analysis of break and active monsoon spells, Curr. Sci., 91(3), 296306.
  • Rodwell, M. J., and B. J. Hoskins (1995), A model of the Asian summer monsoon, Part II: Cross-equatorial flow and PV behavior, J. Atmos. Sci., 52, 13411356.
  • Rowley, D. B., and B. S. Currie (2006), Palaeo-altimetry of the late Eocene to Miocene Lunpola basin, central Tibet, Nature, 439, 677681.
  • Rowley, D. B., R. T. Pierrehumbert, and B. S. Currie (2001), A new approach to stable isotope-based paleoaltimetry: implications for paleoaltimetry and paleohypsometry of the High Himalaya since the Late Miocene, Earth Planet. Sci. Lett., 188, 253268.
  • Saylor, J. E., J. Quade, D. L. Dettman, P. G. DeCelles, P. A. Kapp, and L. Ding (2009), The Late Miocene through present paleoelevation history of southwestern Tibet, Am. J. Sci., 309, 142.
  • Singh, G., R. D. Joshi, and A. B. Singh (1972), Stratigraphic and radiocarbon evidence for the age and development of three salt-lake deposits in Rajasthan, India, Quat. Res., 2, 496505.
  • Singh, G., R. J. Wasson, and D. P. Agarwal (1990), Vegetational and seasonal climatic changes since the last full glacial in the Thar Desert, Rev. Paleobot. Palynol., 64, 351358.
  • Sinha, R., D. Stueben, and Z. Berner (2004), Palaeohydrology of the Sambhar Playa, Thar Desert, India, using geomorphological and sedimentological evidences, J. Geol. Soc. India, 64, 419430.
  • Soman, M., and K. Krishna Kumar (1993), Space-time evolution of meteorological features associated with the onset of Indian summer monsoon, Mon. Weather Rev., 121, 11771194.
  • Spicer, R. A., N. B. W. Harris, M. Widdowson, A. B. Herman, S. Guo, P. J. Valdes, J. A. Wolfe, and S. P. Kelley (2003), Constant elevation of southern Tibet over the past 15 million years, Nature, 421, 622624.
  • Webster, P. J., and S. Yang (1992), Monsoon and ENSO: Selectively interactive systems, Quar. J. Roy. Met. Soc., 118, 877926.
  • Wilks, D. S. (1995), Statistical Methods in the Atmospheric Sciences, Elsevier, New York.
  • Wu, G.-x., and Y.-s. Zhang (1998), Tibetan Plateau forcing and the timing of the monsoon onset over South Asia and the South China Sea, Mon. Weath. Rev., 126, 913927.
  • Wu, G.-x., Y.-m Liu, B. He, Q. Bao, A.-m. Duan, and F.-F. Jin (2012a), Thermal controls on the Asian summer monsoon, Sci. Rep., 2, 404, DOI: 10.1038/srep00404.
  • Wu, G.-x., Y.-m. Liu, B.-w. Dong, X.-y. Liang, A.-m. Duan, Q. Bao, and J.-l. Yu (2012b), Revisiting Asian monsoon formation and change associated with Tibetan Plateau forcing: I. Formation, Clim. Dyn., 39, 11691181.
  • Xavier, P. K., C. Marzin, and B. N. Goswami (2007), An objective definition of the Indian summer monsoon season and a new perspective of the ENSO-monsoon relationship, Quart. J. Roy. Meteo. Soc., 133, 749764. doi:10.1002/qj.45.
  • Xie, P.-p., A. Yatagai, M.-y. Chen, T. Hayasaka, Y. Fukushima, C.-m. Liu, and S. Yang (2007), A gauge-based analysis of daily precipitation over East Asia, J. Hydrometeorol., 8, 607627.
  • Yanai, M., and G.-X. Wu (2006), Effects of the Tibetan Plateau, in The Asian Monsoon, edited by B. Wang, Springer, 513549.
  • Yanai, M., C.-f. Li, and Z.-s. Song (1992), Seasonal heating of the Tibetan Plateau and its effects on the evolution of the Asian summer monsoon, J. Meteor. Soc. Japan, 70, 319351.
  • Yasunari, T., K. Saito, and K. Takata (2006), Relative roles of large-scale orography and land surface processes in the global hydroclimate. Part I: Impacts on monsoon systems and the tropics, J. Hydrometeorol., 7, 626641.