Abstract
The wind-induced, upwelling-related productivity records from the western Arabian Sea have been used to reconstruct past variations in the Southwest (SW) monsoon wind strength. In contrast, the eastern Arabian Sea stores precipitation signal as it receives abundant freshwater, either as overhead precipitation or as surface runoff from the adjacent Western Ghats during the SW monsoon. A sediment core, SK 145-9 (12.6°N, 74.3°E; water depth 400 m, analyzed AMS dated length 50 cm-spanning past ~2,800 years) from the eastern Arabian Sea, was analyzed with high-resolution (sub-centennial) for δ18O and δ13C variations in three different species of planktic foraminifera (Globigerinoides ruber, Globigerinoides sacculifer and Globorotalia menardii) that documents past precipitation changes. Periods of aridity were observed at ~2,000, 1,500, 1,100, 850 and 500 cal yr BP (calibrated ages) in the eastern Arabian Sea, which were matched with data from western Arabian Sea depicting wind intensity. The wind strength exhibits good correlation with the precipitation intensity; reduced precipitation is accompanied by weakened winds, thus providing the paleoclimatic evidence for the control exhibited by SW monsoon precipitation over the wind strength via latent heat release.
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References
Agnihotri R, Bhattacharya SK, Sarin MM, Somayajulu BLK (2003) Changes in the surface productivity and subsurface denitrification during the Holocene: a multiproxy study from the eastern Arabian Sea. Holocene 13(5):701–713
Anderson DM, Prell WL (1993) A 300 kyr record of upwelling off Oman during the Late Quaternary: evidence of the Asian Southwest monsoon. Paleoceanography 8:193–208
Anderson DM, Overpeck JT, Gupta AK (2002) Increase in the Asian SW monsoon during the past four centuries. Science 297:596–599
Bé AWH (1977) An ecological, zoogeographic and taxonomic review of recent planktonic foraminifera. In: Ramsey ATS (ed) Oceanic micropaleontology. Academic, London, p 100
Bhattathiri PMA, Pant A, Sawant S, Gauns M, Matondakar SGP, Mohanraju R (1996) Phytoplankton production and chlorophyll distribution in the eastern and central Arabian Sea in 1994–1995. Curr Sci 71(11):857–862
Chauhan OS, Vogelsang E, Basavaiah N, Kader USA (2009) Reconstruction of the variability of the southwest monsoon during the past 3 ka, from the continental margin of the southeastern Arabian Sea. J Quat Sci 25(5):798–807
Clemens SC, Prell W, Murray G, Shimmield G, Weedon G (1991) Forcing mechanisms of the Indian Ocean monsoon. Nature 353:720–725
Clemens SC, Murray DW, Prell W (1996) Non-stationary phase of the Plio-Pleistocene Asian monsoon. Science 274:943–948
Duplessy JC, Bé AWH, Blanc PL (1981) Oxygen and carbon isotopic composition of planktonic foraminifera in the Indian Ocean. Palaeogeogr Palaeoclimatol Palaeoecol 33:9–46
Fairbanks RG (1989) A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep ocean circulation. Nature 342:637–642
Fairbanks RG, Wiebe PH, Bé AWH (1980) Vertical distribution and isotopic composition of living planktonic foraminifera in the western North Atlantic. Science 207:61–63
Fleitmann D, Burns SJ, Mudelsee M, Neff U, Kramers J, Mangini A, Matter A (2003) Holocene forcing of the Indian Monsoon recorded in a stalagmite from southern Oman. Science 300:1737–1739
Gadgil S (2003) The Indian monsoon and its variability. Annu Rev Earth Planet Sci 31:429–467
Govil P, Naidu PD (2010) Evaporation-precipitation changes in the eastern Arabian Sea for the last 68 ka: implications on monsoon variability. Paleoceanography 25. doi:10.1029/2008PA001687
Gupta AK, Anderson DM, Overpeck JT (2003) Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean. Nature 421:354–357
Gupta AK, Das M, Anderson DM (2005) Solar influence on the Indian summer monsoon during the Holocene. Geophys Res Lett 32:L17703
Guptha MVS, Curry WB, Ittekkot V, Murlinath AS (1997) Seasonal variation in the flux of planktic foraminifera: sediment trap results from the Bay of Bengal, Northern Indian Ocean. J Foramin Res 27:5–19
Kroopnick PM (1985) The distribution of 13C of ΣCO2 in the world oceans. Deep-Sea Res 32:75–84
Luckge A, Rolinski AD, Khan AA, Schulz H, von Rad U (2001) Monsoonal variability in the northeastern Arabian Sea during the past 5000 years: geochemical evidence from laminated sediments. Palaeogeogr Palaeoclimatol Palaeoecol 167:273–286
McCreary JP, Kundu PK, Molinari RL (1993) A numerical investigation of dynamics, thermodynamics and mixed layer processes in the Indian Ocean. Prog Oceanogr 31:181–224
Naidu PD, Malmgren BA, Bornmalm L (1993) Quaternary history of the calcium carbonate fluctuations in the western equatorial Indian Ocean (Somali basin). Palaeogeog Palaeoclimatol Palaeoecol 103:21–30
Nair RR, Ittekkot V, Ramaswamy SJ, Haake B, Degens ET, Desai BN, Honjo S (1989) Increased particle flux to the deep ocean related to monsoons. Nature 338:749–751
Reichart GJ, Schenau SJ, de Lange GJ, Zachariasse WJ (2002) Synchroneity of oxygen minimum zone intensity on the Oman and Pakistan margins at sub-Milankovitch time scales. Mar Geol 185:403–415
Rostek F, Ruhland G, Bassinot FC, Muller PJ, Labeyrie LD, Lancelot Y, Bard E (1993) Reconstructing sea surface temperature and salinity using δ18O and alkenone records. Nature 364:319–321
Saher MH, Jung SJA, Elderfield H, Greaves MJ, Kroon D (2007) Sea surface temperatures of the western Arabian Sea during the last deglaciation. Paleoceanography 22:PA2208
Sarkar A, Ramesh R, Somayajulu BLK, Agnihotri R, Jull AJT, Burr GS (2000) High resolution Holocene monsoon record from the eastern Arabian Sea. Earth Planet Sci Lett 177:209–218
Shackleton NJ (1967) Oxygen isotope analyses and Pleistocene temperatures reassessed. Nature 215:15–17
Shankar D, Shetye SR (1997) On the dynamics of the Lakshadweep high and low in the southeastern Arabian Sea. J Geophys Res 102:12551–12562
Shetye SR (1984) Seasonal variability of the temperature field off the southwest coast of India. Proc Indian Acad Sci 93(4):399–411
Sirocko F, Sarnthein M, Erlenkreuser H, Lange H, Arnold M, Duplessy JC (1993) Century scale events in monsoon climate over the past 24,000 years. Nature 364:322–324
Southon J, Kashgarian M, Fontugne M, Metivier B, Wyss Yim W-S (2002) Marine reservoir corrections for the Indian Ocean and Southeast Asia. Radiocarbon 44:167–180
Staubwasser M, Sirocko F, Grootes PM, Segl M (2003) Climate change at the 4.2 ka BP termination of the Indus valley civilization and Holocene south Asian monsoon variability. Geophys Res Lett 30:1425–1428
Stuiver M, Reimer PJ, Bard E, Beck JW, Burr GS, Hughen KA, Kromer B, McCormac G, van der Plicht J, Spurk M (1998) INTCAL98 radiocarbon age calibration, 24,000–0 cal BP. Radiocarbon 40:1041–1083
Thamban M, Rao VP, Schneider RR, Grootes PM (2001) Glacial to Holocene fluctuations in hydrography and productivity along the southwestern continental margin of India. Palaeogeog Palaeoclimatol Palaeoecol 165:113–127
Tiwari M, Ramesh R, Somayajulu BLK, Jull AJT, Burr GS (2006) Paleomonsoon precipitation deduced from a sediment core from the equatorial Indian Ocean. Geo-Mar Lett 26:23–30
Tiwari M, Ramesh R, Bhushan R, Sheshshayee MS, Somayajulu BLK, Jull AJT, Burr GS (2010) Did the Indo-Asian summer monsoon decrease during the Holocene following insolation? J Quat Sci 25:1179–1188. doi:10.1002/jqs.1398
von Rad U, Schaaf M, Michels KH, Schulz H, Berger WH, Sirocko F (1999) A 5000-yr record of climate change in varved sediments from the oxygen minimum zone off Pakistan, Northeastern Arabian Sea. Quat Res 51:39–53
Yadava MG, Ramesh R (2005) Monsoon reconstruction from radiocarbon dated tropical Indian speleothems. Holocene 15:50–62
Zonneveld KAF, Ganssen G, Troelstra S, Verstheegh GJM, Visscher H (1997) Mechanisms forcing abrupt fluctuations of the Indian Ocean summer monsoon during the last deglaciation. Quat Sci Rev 16:187–201
Acknowledgement
MT thanks ISRO-GBP for funding and Sri Rasik Ravindra, Director-NCAOR for support; this is NCAOR Contribution no. 015/2011.
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Tiwari, M. (2013). High Resolution Southwest Monsoon Reconstruction for the Past ~2,800 Years: Wind Versus Precipitation. In: Sinha, R., Ravindra, R. (eds) Earth System Processes and Disaster Management. Society of Earth Scientists Series. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-28845-6_8
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