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The East Asian Winter Monsoon Variability in Response to Precession During the Past 150 000 Yr : Volume 9, Issue 6 (13/12/2013)

By Yamamoto, M.

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Book Id: WPLBN0004006588
Format Type: PDF Article :
File Size: Pages 12
Reproduction Date: 2015

Title: The East Asian Winter Monsoon Variability in Response to Precession During the Past 150 000 Yr : Volume 9, Issue 6 (13/12/2013)  
Author: Yamamoto, M.
Volume: Vol. 9, Issue 6
Language: English
Subject: Science, Climate, Past
Collections: Periodicals: Journal and Magazine Collection, Copernicus GmbH
Historic
Publication Date:
2013
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications

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Chen, M., Sai, H., Zhao, M., & Yamamoto, M. (2013). The East Asian Winter Monsoon Variability in Response to Precession During the Past 150 000 Yr : Volume 9, Issue 6 (13/12/2013). Retrieved from http://www.ebooklibrary.org/


Description
Description: Faculty of Environmental Earth Science, Hokkaido University, Kita-10, Nishi-5, Kita-ku, Sapporo 060-0810, Japan. The response of the East Asian winter monsoon variability to orbital forcing is still unclear, and hypotheses are controversial. We present a 150 000 yr record of sea surface temperature difference (ΔSST) between the South China Sea and other Western Pacific Warm Pool regions as a proxy for the intensity of the Asian winter monsoon, because the winter cooling of the South China Sea is caused by the cooling of surface water at the northern margin and the southward advection of cooled water due to winter monsoon winds. The ΔSST showed dominant precession cycles during the past 150 000 yr. The ΔSST varies at precessional band and supports the hypothesis that monsoon is regulated by insolation changes at low-latitudes (Kutzbach, 1981), but contradicts previous suggestions based on marine and loess records that eccentricity controls variability on glacial–interglacial timescales. Maximum winter monsoon intensity corresponds to the May perihelion at precessional band, which is not fully consistent with the Kutzbach model of maximum winter monsoon at the June perihelion. Variation in the East Asian winter monsoon was anti-phased with the Indian summer monsoon, suggesting a linkage of dynamics between these two monsoon systems on an orbital timescale.

Summary
The East Asian winter monsoon variability in response to precession during the past 150 000 yr

Excerpt
Chen, M.-T. and Huang, C.-Y.: Ice-volume forcing of winter monsoon climate in the South China Sea, Paleoceanography, 13, 622–633, 1998.; Caley, T., Malaizé, B., Zaragosi, S., Rossignol, L., Bourget, J., Eynaud, F., Martinez, P., Giraudeau, J., Charlier, K., and Ellouz-Zimmermann, N.: New Arabian Sea records help decipher orbital timing of Indo-Asian monsoon, Earth Planet. Sci. Lett., 308, 433–444, 2011.; Chen, M.-T., Beaufort, L., and the Shipboard Scientific Party of the IMAGES III/MD106-IPHIS Cruise (Leg II): Exploring Quaternary variability of the East Asian monsoon, Kuroshio Current, and the Western Pacific warm pool systems: high-resolution investigations of paleoceanography from the IMAGES III/MD106-IPHIS cruise, Terrest. Atmos. Ocean. Sci., 9, 129–142, 1998.; Chen, M.-T., Shiau, L.-J., Yu, P.-S., Chiu, T.-C., Chen, Y.-G., and Wei, K.-Y.: 500 000-Year records of carbonate, organic carbon, and foraminiferal sea surface temperature from the southeastern South China Sea (near Palawan Island), Palaeogeogr. Palaeocli. Palaeoecol., 197, 113–131, 2003.; Clemens, S. C. and Prell, W. L.: A 350,000 year summer-monsoon multi-proxy stack from the Own Ridge, Northern Arabian Sea, Mar. Geol., 201, 35–51, 2003.; Clemens, S. C., Prell, W. L., and Sun, Y.: Orbital-scale timing and mechanisms driving Late Pleistocene Indo-Asian summer monsoons: Reinterpreting cave speleothem δ18O, Paleoceanography, 25, 1–19, 2010.; de Garidel-Thoron, T., Beaufort, L., Linsley, B. K., and Dannenmann, S.: Millennial-scale dynamics of the East Asian winter monsoon during the last 200,000 years, Paleoceanography, 16, 491–502, 2001.; de Garidel-Thoron, T., Rosenthal, Y., Bassinot, F., and Beaufort, L.: Stable sea surface temperatures in the western Pacific warm pool over the past 1.75 million years, Nature, 433, 294–298, 2005.; Ding, Z., Liu, T., Putter, N. W., Yu, Z., Guo, Z., and Zhu, R.: Ice-volume forcing of East Asian winter monsoon variations in the past 800,000 years, Quaternary Res., 44, 149–159, 1995.; Feldman, G. C., Kuring, N., Ng, C., Esaias, W., McClain, C., Elrod, J., Maynard, N., and Endres, D.: Ocean color–availability of the global data set. Eos, Transactions, Am. Geophys. Union, 70, 634–641, 1989.; Hopmans, E. C., Schouten, S., Pancost, R., van der Meer, M. T. J., and Sinninghe Damsté, J. S.: Analysis of intact tetraether lipids in archaeal cell material and sediments by high performance liquid chromatography/atmospheric pressure chemical ionization mass spectrometry, Rapid Commun. Mass Spectrom., 14, 585–589, 2000.; Hopmans, E. C., Weijers, J. W. H., Schefuß, E., Herfort, L., Sinninghe Damsté, J. S., and Schouten, S.: A novel proxy for terrestrial organic matter in sediments normalized on branched and isoprenoid tetraether lipids, Earth Planet. Sci. Lett., 224, 107–116, 2004.; Hu, J., Kawamura, H., Hong, H., and Qi, Y.: A review on the currents in the South China Sea: Seasonal circulation, South China Sea Warm Current and Kuroshio Intrusion, J. Oceanogr., 56, 607–624, 2000.; Huang, C.-Y., Liew, P.-M., Zhao, M., Chang, T.-C., Kuo, C.-M., Chen, M.-T., Wang, C.-H., and Zheng, L.: Deep sea and lake records of the Southeast Asian paleomonsoons for the last 25 kyrs, Earth Planet. Sci. Lett., 146, 59–72, 1997a.; Huang, C.-Y., Wu, S.-F., Zhao, M., Chen, M.-T., Wang, C.-H., Tu, X., and Yuan, P. B.: Surface ocean and monsoon climate variability in the South China Sea since last glaciation, Mar. Micropaleontol., 32, 71–94, 1997b.; Huang, C. Y., Wang, C. C., and Zhao, M.: High-resolution carbonate stratigraphy of IMAGES core MD972151 from the South China Sea, Terrest. Atmos. Ocean. Sci., 10, 225–238, 1999.; Huang, C.-C., Chen, M.-T., Lee, M.-Y., Wei, K.-Y., and Huang, C.-Y.: Planktic foraminifer faunal sea surface temperature records of the past two glacial terminations in the South China Sea near Wan-An shallow (IMAGES core MD972151), West. Pacific Earth Sci., 2, 1–14, 2002.; Huang, E., Tian, J., and Steinke, S.: Millennial-scal

 

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