globalchange  > 过去全球变化的重建
DOI: 10.1016/j.palaeo.2015.03.007
论文题名:
A high resolution record of sea surface temperature in southern Okinawa Trough for the past 15,000years
作者: Ruan J.; Xu Y.; Ding S.; Wang Y.; Zhang X.
刊名: Palaeogeography, Palaeoclimatology, Palaeoecology
ISSN: 0031-0182
出版年: 2015
卷: 426
起始页码: 209
结束页码: 215
语种: 英语
英文关键词: Alkenone ; Holocene ; Kuroshio Current ; Monsoon ; Okinawa Trough ; Sea surface temperature
英文摘要: The study of long-chain alkenones in the Ocean Drilling Program (ODP) core 1202B reveals a sub-centennial resolution record of sea surface temperature (SST) in the southern Okinawa Trough for the past 15. thousand. years (kyr). From the Deglaciation to Holocene, SST varied from 21.1 to 26.5. °C. The presence of Bølling (15.0-14.2. kyr. BP) and Allerød (13.7-13.4. kyr. BP) warming phases, Older Dryas (14.2-13.7. kyr. BP) and Younger Dryas (12.8-11.6. kyr. BP) cold periods reflects a tight teleconnection of climate between the Okinawa Trough and the North Atlantic region in the last Deglaciation. After rapidly increased and reached the maximum at ~. 7.4. kyr. BP, SST in the southern OT gradually decreased, corresponding with the lowering of northern hemisphere summer solar insolation. However, a series of abrupt SST drops were identified at ca. 8.6-8.1, 5.8-4.8, 4.1-3.9, 3.0-2.5, 1.6-1.3 and 0.6-0.5. kyr. BP, which cannot be explained by solar insolation changes alone, and instead are mediated by a complex sun-ocean-atmosphere coupling. © 2015 Elsevier B.V.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/68962
Appears in Collections:过去全球变化的重建

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作者单位: MOE Key Laboratory for Earth Surface Process, College of Urban and Environmental Sciences, Peking University, Beijing, China; Qingdao Collaborative Innovation Center of Marine Science and Technology, Qingdao, China

Recommended Citation:
Ruan J.,Xu Y.,Ding S.,et al. A high resolution record of sea surface temperature in southern Okinawa Trough for the past 15,000years[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2015-01-01,426
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