Ice-Volume Forcing of East Asian Winter Monsoon Variations in the Past 800,000 Years
Particle-size measurements of some typical loess-soil samples taken in different localities of the Chinese Loess Plateau demonstrate that the grain size ratio of <2 μm/>10 μm (%) can be used as an indicator of variations in intensity of the East Asian winter monsoon winds. Grain-size curves of...
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| Published in | Quaternary research Vol. 44; no. 2; pp. 149 - 159 |
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| Main Authors | , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
New York, USA
Cambridge University Press
01.09.1995
Elsevier Inc Elsevier |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Particle-size measurements of some typical loess-soil samples taken in different localities of the Chinese Loess Plateau demonstrate that the grain size ratio of <2 μm/>10 μm (%) can be used as an indicator of variations in intensity of the East Asian winter monsoon winds. Grain-size curves of the Baoji and Weinan sections show that this proxy indicator is very sensitive to loess-soil alterations. Analytical results also suggest that during soil-forming periods, eolian dust accumulation was still substantial and, hence, loess deposition can be regarded as a nearly continuous process during the Quaternary period. In this study we compared the Baoji grain-size time series with the SPECMAP marine isotope record with the objective of elucidating the dynamic linkage between changes in global ice volume and the winter monsoon circulation. Both records show good agreement at both time and frequency domains. In particular, the winter monsoon variations are also dominated by a 100,000 yr period over the past 800,000 yr. It is thus inferred that direct local insolation forcing could be less important in driving the East Asian winter monsoon variability, and, alternatively, variations in glacial-age boundary conditions may have played a key role in modulating and pacing its strength and timing. |
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| AbstractList | Abstract
Particle-size measurements of some typical loess-soil samples taken in different localities of the Chinese Loess Plateau demonstrate that the grain size ratio of <2 μm/>10 μm (%) can be used as an indicator of variations in intensity of the East Asian winter monsoon winds. Grain-size curves of the Baoji and Weinan sections show that this proxy indicator is very sensitive to loess-soil alterations. Analytical results also suggest that during soil-forming periods, eolian dust accumulation was still substantial and, hence, loess deposition can be regarded as a nearly continuous process during the Quaternary period. In this study we compared the Baoji grain-size time series with the SPECMAP marine isotope record with the objective of elucidating the dynamic linkage between changes in global ice volume and the winter monsoon circulation. Both records show good agreement at both time and frequency domains. In particular, the winter monsoon variations are also dominated by a 100,000 yr period over the past 800,000 yr. It is thus inferred that direct local insolation forcing could be less important in driving the East Asian winter monsoon variability, and, alternatively, variations in glacial-age boundary conditions may have played a key role in modulating and pacing its strength and timing. Particle-size measurements of some typical loess-soil samples taken in different localities of the Chinese Loess Plateau demonstrate that the grain size ratio of <2 μm/>10 μm (%) can be used as an indicator of variations in intensity of the East Asian winter monsoon winds. Grain-size curves of the Baoji and Weinan sections show that this proxy indicator is very sensitive to loess-soil alterations. Analytical results also suggest that during soil-forming periods, eolian dust accumulation was still substantial and, hence, loess deposition can be regarded as a nearly continuous process during the Quaternary period. In this study we compared the Baoji grain-size time series with the SPECMAP marine isotope record with the objective of elucidating the dynamic linkage between changes in global ice volume and the winter monsoon circulation. Both records show good agreement at both time and frequency domains. In particular, the winter monsoon variations are also dominated by a 100,000 yr period over the past 800,000 yr. It is thus inferred that direct local insolation forcing could be less important in driving the East Asian winter monsoon variability, and, alternatively, variations in glacial-age boundary conditions may have played a key role in modulating and pacing its strength and timing. |
| Author | Ding, Zhongli Yu, Zhiwei Zhu, Rixiang Rutter, Nat W. Guo, Zhengtang Liu, Tungsheng |
| Author_xml | – sequence: 1 givenname: Zhongli surname: Ding fullname: Ding, Zhongli organization: Institute of Geology, Chinese Academy of Sciences, Beijing 100029, China – sequence: 2 givenname: Tungsheng surname: Liu fullname: Liu, Tungsheng organization: Institute of Geology, Chinese Academy of Sciences, Beijing 100029, China – sequence: 3 givenname: Nat W. surname: Rutter fullname: Rutter, Nat W. organization: Department of Geology, University of Alberta, Edmonton, Canada T6G 2E3 – sequence: 4 givenname: Zhiwei surname: Yu fullname: Yu, Zhiwei organization: Department of Geology, China Mining and Technology University, Xuzhou 221008, China – sequence: 5 givenname: Zhengtang surname: Guo fullname: Guo, Zhengtang organization: Institute of Geology, Chinese Academy of Sciences, Beijing 100029, China – sequence: 6 givenname: Rixiang surname: Zhu fullname: Zhu, Rixiang organization: Institute of Geophysics, Chinese Academy of Sciences, Beijing 100101, China |
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| Cites_doi | 10.1007/978-94-017-4841-4_13 10.1016/0277-3791(93)90024-G 10.1007/978-94-017-4841-4_14 |
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| Copyright | University of Washington 1995 Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 1996 |
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| DocumentTitleAlternate | EAST ASIAN WINTER MONSOON VARIATIONS DING ET AL. |
| EISSN | 1096-0287 |
| EndPage | 159 |
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| Issue | 2 |
| Keywords | Loess Atmospheric circulation Inland ice Plateau Oxygen 18 Quaternary Monsoon Grain size distribution Winter Global change Climatic variation Isotope analysis Palaeoclimatology Deglaciation |
| Language | English |
| License | CC BY 4.0 |
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| References | Shackleton (S0033589400024340_ref045) 1990 Liu (S0033589400024340_ref033) 1985 S0033589400024340_ref040 Liu (S0033589400024340_ref031) 1965 S0033589400024340_ref044 Rutter (S0033589400024340_ref043) 1990 S0033589400024340_ref008 Duplessy (S0033589400024340_ref020) 1988 Kukla (S0033589400024340_ref027) 1987 (S0033589400024340_ref014) 1984 Berger (S0033589400024340_ref007) 1991 Ding (S0033589400024340_ref017) 1992 (S0033589400024340_ref013) 1976 Ding (S0033589400024340_ref018) 1993 Zhang (S0033589400024340_ref054) 1982 Berger (S0033589400024340_ref006) 1984 An (S0033589400024340_ref002) 1991b Zhang (S0033589400024340_ref056) 1987 Liu (S0033589400024340_ref032) 1966 Kukla (S0033589400024340_ref028) 1989 Manabe (S0033589400024340_ref037) 1985 Chang (S0033589400024340_ref009) 1980 Hays (S0033589400024340_ref021) 1978 Liu (S0033589400024340_ref034) 1981 Imbrie (S0033589400024340_ref024) 1993 Clemens (S0033589400024340_ref012) 1991 Trewartha (S0033589400024340_ref050) 1981 Trewartha (S0033589400024340_ref051) 1980 Lambeck (S0033589400024340_ref030) 1995 Ding (S0033589400024340_ref019) 1994 Tauxe (S0033589400024340_ref048) 1992 Liu (S0033589400024340_ref035) 1982 Milankovitch (S0033589400024340_ref038) 1941 Baksi (S0033589400024340_ref003) 1992 Kutzbach (S0033589400024340_ref029) 1985 Ruddiman (S0033589400024340_ref042) 1989b Stuiver (S0033589400024340_ref046) 1981 Berger (S0033589400024340_ref005) 1978 Ruddiman (S0033589400024340_ref041) 1989a Denton (S0033589400024340_ref016) 1981 Tao (S0033589400024340_ref047) 1957 Chu (S0033589400024340_ref011) 1984 Imbrie (S0033589400024340_ref025) 1992 Imbrie (S0033589400024340_ref026) 1984 Xiao (S0033589400024340_ref053) 1995 Hays (S0033589400024340_ref022) 1976 An (S0033589400024340_ref001) 1991a Chen (S0033589400024340_ref010) 1991 (S0033589400024340_ref015) 1988 Liu (S0033589400024340_ref036) 1989 Ruddiman (S0033589400024340_ref039) 1991 Howard (S0033589400024340_ref023) 1984 Williams (S0033589400024340_ref052) 1993 Zhang (S0033589400024340_ref055) 1984 Thierstein (S0033589400024340_ref049) 1977 Bartholomew (S0033589400024340_ref004) 1980 |
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| Snippet | Particle-size measurements of some typical loess-soil samples taken in different localities of the Chinese Loess Plateau demonstrate that the grain size ratio... Abstract Particle-size measurements of some typical loess-soil samples taken in different localities of the Chinese Loess Plateau demonstrate that the grain... |
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| SubjectTerms | Bgi / Prodig Climatic oscillations. Historical climates. Palaeoclimates Climatology Physical geography |
| Title | Ice-Volume Forcing of East Asian Winter Monsoon Variations in the Past 800,000 Years |
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