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    Volume 35 Issue 4
    Jul.  2010
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    LIU Dong-yan, LI Wei-ran, QIAO Yan-song, WANG Ling, PENG Sha-sha, 2010. The Periodicity of the Southwest Monsoon Revealed by the Magnetic Susceptibility of the Garzê A Loess-Paleosol Sequence Using EMD Method. Earth Science, 35(4): 533-541. doi: 10.3799/dqkx.2010.069
    Citation: LIU Dong-yan, LI Wei-ran, QIAO Yan-song, WANG Ling, PENG Sha-sha, 2010. The Periodicity of the Southwest Monsoon Revealed by the Magnetic Susceptibility of the Garzê A Loess-Paleosol Sequence Using EMD Method. Earth Science, 35(4): 533-541. doi: 10.3799/dqkx.2010.069

    The Periodicity of the Southwest Monsoon Revealed by the Magnetic Susceptibility of the Garzê A Loess-Paleosol Sequence Using EMD Method

    doi: 10.3799/dqkx.2010.069
    • Received Date: 2009-10-22
    • Publish Date: 2010-07-01
    • The magnetic susceptibility of loess as a proxy for the intensity of summer monsoon has be used to investigate the periodicity of paleoclimatic changes of aeolian deposits in China.However, previous studies focused most on the southeast monsoon areas. On the basis of magnetostratigraphic study of the Garzê A section on the southeastern margin of the Qinghai-Tibet Plateau, the magnetic susceptibility records during the past 1.16 Ma were subject to an empirical mode decomposition (EMD) to discuss the periodicity of the southwest monsoon evolution at various time scales. The results show that: (1) the significant orbital periodicities do exist including the eccentricity, obliquity and precession periods in our records, which indicates that the southwest monsoon is also controlled by the astronomical factors; (2) The beat frequency periods of the precession are detected, which shows the tropical climatic characteristics of the southwest monsoon; (3) the quasi-200 ka cycle is confirmed in existence but its forming mechanism needs further study; (4) the appearance of quasi-400 ka cycle fluctuation may correspond to quasi-400 ka eccentricity cycle. Therefore, the main forcing of Indian monsoon system may be the solar insolation at low latitude. As for the studies of paleoenvironment evolution of sedimentary records, EMD is superior and has more potentials than the traditional method of spectral analysis.

       

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