Synchronous climate anomalies in the western North Pacific and North Atlantic regions during the last 14,000 years

Hong, Youwei; Hong, Bin; Lin, Qinhao; Shibata, Yasuyuki; Zhu, Yuxin; Leng, X.T.; Wang, Y.

doi:10.1016/j.quascirev.2008.11.011

Cited by 78 publications

(55 citation statements)

References 72 publications

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“…The high-resolution records of an alternation of the NW Pacific events with lower/higher productivity related to climate cooling/warming demonstrate that centennial-scale climate events during the EH were similar between the N Atlantic and NW Pacific, possibly because of the close linkages of sun, ocean and climate, consistent with earlier conclusions (Bond et al, 2001;Hong et al, 2009;Hu et al, 2003).…”

Section: Centennial Variations In Productivity During the Ehsupporting

confidence: 86%

“…Furthermore, the timing and pattern of variability during the early Holocene (EH) regional climate changes are still under debate. In particular, though the EH climate has started from a strong warming in most cases, a Hani peat δ 18 O record from NE China instead suggest a centennial cooling event which is primarily superimposed on a long-term warming trend during the Holocene (Hong et al, 2009). …”

Section: Introductionmentioning

confidence: 99%

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Centennial to millennial climate variability in the far northwestern Pacific (off Kamchatka) and its linkage to the East Asian monsoon and North Atlantic from the Last Glacial Maximum to the early Holocene

Gorbarenko¹,

Shi²,

Malakhova³

et al. 2017

Clim. Past

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Abstract. High-resolution reconstructions based on productivity proxies and magnetic properties of core LV63-41-2 (off Kamchatka) reveal prevailing centennial productivity/climate variability in the northwestern (NW) Pacific from the Last Glacial Maximum (LGM) to the early Holocene (EH). The age model of the core is established by AMS 14 C dating and by projections of AMS 14 C data of the nearby core SO-201-12KL through correlation of the productivity proxies and relative paleomagnetic intensity. The resulting sequence of centennial productivity increases/climate warming events in the NW Pacific occurred synchronously with the East Asian summer monsoon (EASM) sub-interstadials during the LGM (four events), Heinrich Event 1 (HE1) (four events), Bølling-Allerød (B/A) warming (four events), and over the EH (four events). Remarkable similarity of the sequence of the NW Pacific increased-productivity events with the EASM sub-interstadials over the LGM-HE1 implies that the Siberian High is a strong and common driver. The comparison with the δ 18 O record from Antarctica suggests that another mechanism associated with the temperature gradient in the Southern Hemisphere may also be responsible for the EASM/NW Pacific centennial events over the LGM-HE1. During the B/A warming and resumption of the Atlantic Meridional Overturning Circulation (AMOC), clear synchronicity between the NW Pacific, EASM and Greenland sub-interstadials was mainly controlled by changes in the atmospheric circulation. During the EH the linkages between solar forcing, ocean circulation, and climate changes likely control the synchronicity of abrupt climate changes in the NW Pacific and North Atlantic. The sequence of centennial events recorded in this study is a persistent regional feature during the LGM-EH, which may serve as a template in high-resolution paleoceanography and sediment stratigraphy in the NW Pacific.

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Section: Centennial Variations In Productivity During the Ehsupporting

confidence: 86%

Section: Introductionmentioning

confidence: 99%

Centennial to millennial climate variability in the far northwestern Pacific (off Kamchatka) and its linkage to the East Asian monsoon and North Atlantic from the Last Glacial Maximum to the early Holocene

Gorbarenko¹,

Shi²,

Malakhova³

et al. 2017

Clim. Past

View full text Add to dashboard Cite

show abstract

“…Recent studies have led to significant advances in understanding of Asian Monsoon (AM) dynamics during the Holocene [1][2][3][4][5][6][7][8][9][10][11][12][13][14][15][16][17][18]. However, the timing, duration and transition of the Holocene Optimum are still under debate.…”

mentioning

confidence: 99%

Stalagmite-inferred Holocene precipitation in northern Guizhou Province, China, and asynchronous termination of the Climatic Optimum in the Asian monsoon territory

Jiang

Shen³

et al. 2011

Chin. Sci. Bull.

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“…Some studies suggest that the inverse phase relationship between the EASM and the ISM on millennial timescales is linked to the occurrence of El Niña-like conditions in the tropical Pacific during the Holocene (Hong et al, 2005(Hong et al, , 2009, although evidence remains limited. Additional sensitive proxies, high-resolution records, and detailed modeling simulations are needed to fully understand the mechanism that underpinned the inverse phase relationship between the two monsoon systems during the last glacial.…”

Section: Synchronous Long-term Changes In Ism and Easm And Abrupt CLmentioning

confidence: 99%

Evolution of the Indian summer monsoon during the interval 32.7–11.4cal. ka BP: Evidence from the Baoxiu peat, Yunnan, southwest China

Huang

Wei

et al. 2016

Journal of Asian Earth Sciences

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Synchronous climate anomalies in the western North Pacific and North Atlantic regions during the last 14,000 years

Cited by 78 publications

References 72 publications

Centennial to millennial climate variability in the far northwestern Pacific (off Kamchatka) and its linkage to the East Asian monsoon and North Atlantic from the Last Glacial Maximum to the early Holocene

Centennial to millennial climate variability in the far northwestern Pacific (off Kamchatka) and its linkage to the East Asian monsoon and North Atlantic from the Last Glacial Maximum to the early Holocene

Stalagmite-inferred Holocene precipitation in northern Guizhou Province, China, and asynchronous termination of the Climatic Optimum in the Asian monsoon territory

Evolution of the Indian summer monsoon during the interval 32.7–11.4cal. ka BP: Evidence from the Baoxiu peat, Yunnan, southwest China

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