Holocene forcing of East Asian hydroclimate recorded in a subtropical peatland from southeastern China
Abstract The Holocene hydroclimate evolution and underlying mechanisms modulating the East Asian summer monsoon (EASM) remains controversial, especially in south eastern China. Here we present a multiproxy peat record of monsoon evolution from southeastern China covering the last 14 ka. Our new reco...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Huang, Xianyu [verfasserIn] |
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| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2022 |
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| Schlagwörter: |
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| Anmerkung: |
© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 |
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| Übergeordnetes Werk: |
Enthalten in: Climate dynamics - Springer Berlin Heidelberg, 1986, 60(2022), 3-4 vom: 17. Juni, Seite 981-993 |
|---|---|
| Übergeordnetes Werk: |
volume:60 ; year:2022 ; number:3-4 ; day:17 ; month:06 ; pages:981-993 |
| Links: |
|---|
| DOI / URN: |
10.1007/s00382-022-06333-x |
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| Katalog-ID: |
OLC2133853235 |
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| 520 | |a Abstract The Holocene hydroclimate evolution and underlying mechanisms modulating the East Asian summer monsoon (EASM) remains controversial, especially in south eastern China. Here we present a multiproxy peat record of monsoon evolution from southeastern China covering the last 14 ka. Our new records show a relatively weaker EASM but wetter hydroclimate during the early (10 to 8 ka) and late Holocene (after 5.4 ka), while a stronger EASM and overall drier climate during the mid-Holocene (8 to 5.4 ka). In line with nearby speleothem records, our results reveal a dominant control of the northern-latitude ice-sheet meltwater forcing on millennial-scale East Asian hydroclimate variability during the last deglaciation and early Holocene. This dominant influence, however, likely waned once the global sea level had stabilized during the mid-to-late Holocene, giving way to other drivers of the monsoon and hydroclimate, including a combination of summer insolation and teleconnection patterns associated with vegetation-dust feedbacks. | ||
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10.1007/s00382-022-06333-x doi (DE-627)OLC2133853235 (DE-He213)s00382-022-06333-x-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Huang, Xianyu verfasserin aut Holocene forcing of East Asian hydroclimate recorded in a subtropical peatland from southeastern China 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract The Holocene hydroclimate evolution and underlying mechanisms modulating the East Asian summer monsoon (EASM) remains controversial, especially in south eastern China. Here we present a multiproxy peat record of monsoon evolution from southeastern China covering the last 14 ka. Our new records show a relatively weaker EASM but wetter hydroclimate during the early (10 to 8 ka) and late Holocene (after 5.4 ka), while a stronger EASM and overall drier climate during the mid-Holocene (8 to 5.4 ka). In line with nearby speleothem records, our results reveal a dominant control of the northern-latitude ice-sheet meltwater forcing on millennial-scale East Asian hydroclimate variability during the last deglaciation and early Holocene. This dominant influence, however, likely waned once the global sea level had stabilized during the mid-to-late Holocene, giving way to other drivers of the monsoon and hydroclimate, including a combination of summer insolation and teleconnection patterns associated with vegetation-dust feedbacks. Hydroclimate Southeastern China Holocene Lipids Ocean-atmospheric teleconnection Zhang, Hongbin (orcid)0000-0001-6999-3352 aut Griffiths, Michael L. aut Zhao, Bingyan aut Pausata, Francesco S. R. aut Tabor, Clay aut Shu, Junwu aut Xie, Shucheng aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 60(2022), 3-4 vom: 17. Juni, Seite 981-993 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:60 year:2022 number:3-4 day:17 month:06 pages:981-993 https://doi.org/10.1007/s00382-022-06333-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 60 2022 3-4 17 06 981-993 |
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10.1007/s00382-022-06333-x doi (DE-627)OLC2133853235 (DE-He213)s00382-022-06333-x-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Huang, Xianyu verfasserin aut Holocene forcing of East Asian hydroclimate recorded in a subtropical peatland from southeastern China 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract The Holocene hydroclimate evolution and underlying mechanisms modulating the East Asian summer monsoon (EASM) remains controversial, especially in south eastern China. Here we present a multiproxy peat record of monsoon evolution from southeastern China covering the last 14 ka. Our new records show a relatively weaker EASM but wetter hydroclimate during the early (10 to 8 ka) and late Holocene (after 5.4 ka), while a stronger EASM and overall drier climate during the mid-Holocene (8 to 5.4 ka). In line with nearby speleothem records, our results reveal a dominant control of the northern-latitude ice-sheet meltwater forcing on millennial-scale East Asian hydroclimate variability during the last deglaciation and early Holocene. This dominant influence, however, likely waned once the global sea level had stabilized during the mid-to-late Holocene, giving way to other drivers of the monsoon and hydroclimate, including a combination of summer insolation and teleconnection patterns associated with vegetation-dust feedbacks. Hydroclimate Southeastern China Holocene Lipids Ocean-atmospheric teleconnection Zhang, Hongbin (orcid)0000-0001-6999-3352 aut Griffiths, Michael L. aut Zhao, Bingyan aut Pausata, Francesco S. R. aut Tabor, Clay aut Shu, Junwu aut Xie, Shucheng aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 60(2022), 3-4 vom: 17. Juni, Seite 981-993 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:60 year:2022 number:3-4 day:17 month:06 pages:981-993 https://doi.org/10.1007/s00382-022-06333-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 60 2022 3-4 17 06 981-993 |
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10.1007/s00382-022-06333-x doi (DE-627)OLC2133853235 (DE-He213)s00382-022-06333-x-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Huang, Xianyu verfasserin aut Holocene forcing of East Asian hydroclimate recorded in a subtropical peatland from southeastern China 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract The Holocene hydroclimate evolution and underlying mechanisms modulating the East Asian summer monsoon (EASM) remains controversial, especially in south eastern China. Here we present a multiproxy peat record of monsoon evolution from southeastern China covering the last 14 ka. Our new records show a relatively weaker EASM but wetter hydroclimate during the early (10 to 8 ka) and late Holocene (after 5.4 ka), while a stronger EASM and overall drier climate during the mid-Holocene (8 to 5.4 ka). In line with nearby speleothem records, our results reveal a dominant control of the northern-latitude ice-sheet meltwater forcing on millennial-scale East Asian hydroclimate variability during the last deglaciation and early Holocene. This dominant influence, however, likely waned once the global sea level had stabilized during the mid-to-late Holocene, giving way to other drivers of the monsoon and hydroclimate, including a combination of summer insolation and teleconnection patterns associated with vegetation-dust feedbacks. Hydroclimate Southeastern China Holocene Lipids Ocean-atmospheric teleconnection Zhang, Hongbin (orcid)0000-0001-6999-3352 aut Griffiths, Michael L. aut Zhao, Bingyan aut Pausata, Francesco S. R. aut Tabor, Clay aut Shu, Junwu aut Xie, Shucheng aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 60(2022), 3-4 vom: 17. Juni, Seite 981-993 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:60 year:2022 number:3-4 day:17 month:06 pages:981-993 https://doi.org/10.1007/s00382-022-06333-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 60 2022 3-4 17 06 981-993 |
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10.1007/s00382-022-06333-x doi (DE-627)OLC2133853235 (DE-He213)s00382-022-06333-x-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Huang, Xianyu verfasserin aut Holocene forcing of East Asian hydroclimate recorded in a subtropical peatland from southeastern China 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract The Holocene hydroclimate evolution and underlying mechanisms modulating the East Asian summer monsoon (EASM) remains controversial, especially in south eastern China. Here we present a multiproxy peat record of monsoon evolution from southeastern China covering the last 14 ka. Our new records show a relatively weaker EASM but wetter hydroclimate during the early (10 to 8 ka) and late Holocene (after 5.4 ka), while a stronger EASM and overall drier climate during the mid-Holocene (8 to 5.4 ka). In line with nearby speleothem records, our results reveal a dominant control of the northern-latitude ice-sheet meltwater forcing on millennial-scale East Asian hydroclimate variability during the last deglaciation and early Holocene. This dominant influence, however, likely waned once the global sea level had stabilized during the mid-to-late Holocene, giving way to other drivers of the monsoon and hydroclimate, including a combination of summer insolation and teleconnection patterns associated with vegetation-dust feedbacks. Hydroclimate Southeastern China Holocene Lipids Ocean-atmospheric teleconnection Zhang, Hongbin (orcid)0000-0001-6999-3352 aut Griffiths, Michael L. aut Zhao, Bingyan aut Pausata, Francesco S. R. aut Tabor, Clay aut Shu, Junwu aut Xie, Shucheng aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 60(2022), 3-4 vom: 17. Juni, Seite 981-993 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:60 year:2022 number:3-4 day:17 month:06 pages:981-993 https://doi.org/10.1007/s00382-022-06333-x lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 60 2022 3-4 17 06 981-993 |
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Holocene forcing of East Asian hydroclimate recorded in a subtropical peatland from southeastern China |
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Holocene forcing of East Asian hydroclimate recorded in a subtropical peatland from southeastern China |
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Huang, Xianyu Zhang, Hongbin Griffiths, Michael L. Zhao, Bingyan Pausata, Francesco S. R. Tabor, Clay Shu, Junwu Xie, Shucheng |
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holocene forcing of east asian hydroclimate recorded in a subtropical peatland from southeastern china |
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Holocene forcing of East Asian hydroclimate recorded in a subtropical peatland from southeastern China |
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Abstract The Holocene hydroclimate evolution and underlying mechanisms modulating the East Asian summer monsoon (EASM) remains controversial, especially in south eastern China. Here we present a multiproxy peat record of monsoon evolution from southeastern China covering the last 14 ka. Our new records show a relatively weaker EASM but wetter hydroclimate during the early (10 to 8 ka) and late Holocene (after 5.4 ka), while a stronger EASM and overall drier climate during the mid-Holocene (8 to 5.4 ka). In line with nearby speleothem records, our results reveal a dominant control of the northern-latitude ice-sheet meltwater forcing on millennial-scale East Asian hydroclimate variability during the last deglaciation and early Holocene. This dominant influence, however, likely waned once the global sea level had stabilized during the mid-to-late Holocene, giving way to other drivers of the monsoon and hydroclimate, including a combination of summer insolation and teleconnection patterns associated with vegetation-dust feedbacks. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 |
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Abstract The Holocene hydroclimate evolution and underlying mechanisms modulating the East Asian summer monsoon (EASM) remains controversial, especially in south eastern China. Here we present a multiproxy peat record of monsoon evolution from southeastern China covering the last 14 ka. Our new records show a relatively weaker EASM but wetter hydroclimate during the early (10 to 8 ka) and late Holocene (after 5.4 ka), while a stronger EASM and overall drier climate during the mid-Holocene (8 to 5.4 ka). In line with nearby speleothem records, our results reveal a dominant control of the northern-latitude ice-sheet meltwater forcing on millennial-scale East Asian hydroclimate variability during the last deglaciation and early Holocene. This dominant influence, however, likely waned once the global sea level had stabilized during the mid-to-late Holocene, giving way to other drivers of the monsoon and hydroclimate, including a combination of summer insolation and teleconnection patterns associated with vegetation-dust feedbacks. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 |
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Abstract The Holocene hydroclimate evolution and underlying mechanisms modulating the East Asian summer monsoon (EASM) remains controversial, especially in south eastern China. Here we present a multiproxy peat record of monsoon evolution from southeastern China covering the last 14 ka. Our new records show a relatively weaker EASM but wetter hydroclimate during the early (10 to 8 ka) and late Holocene (after 5.4 ka), while a stronger EASM and overall drier climate during the mid-Holocene (8 to 5.4 ka). In line with nearby speleothem records, our results reveal a dominant control of the northern-latitude ice-sheet meltwater forcing on millennial-scale East Asian hydroclimate variability during the last deglaciation and early Holocene. This dominant influence, however, likely waned once the global sea level had stabilized during the mid-to-late Holocene, giving way to other drivers of the monsoon and hydroclimate, including a combination of summer insolation and teleconnection patterns associated with vegetation-dust feedbacks. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 |
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