Menu
×
West Ashley Library
Closed
Phone: (843) 766-6635
Wando Mount Pleasant Library
Closed
Phone: (843) 805-6888
Village Library
Closed
Phone: (843) 884-9741
St. Paul's/Hollywood Library
Closed
Phone: (843) 889-3300
Otranto Road Library
Closed
Phone: (843) 572-4094
Mt. Pleasant Library
Closed
Phone: (843) 849-6161
McClellanville Library
Closed
Phone: (843) 887-3699
Keith Summey North Charleston Library
Closed
Phone: (843) 744-2489
John's Island Library
Closed
Phone: (843) 559-1945
Hurd/St. Andrews Library
Closed
Phone: (843) 766-2546
Folly Beach Library
Closed
Phone: (843) 588-2001
Edisto Island Library
Closed
Phone: (843) 869-2355
Dorchester Road Library
Closed
Phone: (843) 552-6466
John L. Dart Library
Closed
Phone: (843) 722-7550
Baxter-Patrick James Island
Closed
Phone: (843) 795-6679
Main Library
2 p.m. – 5 p.m.
Phone: (843) 805-6930
Bees Ferry West Ashley Library
Closed
Phone: (843) 805-6892
Edgar Allan Poe/Sullivan's Island Library
Closed for renovations
Phone: (843) 883-3914
Mobile Library
Closed
Phone: (843) 805-6909
Today's Hours
West Ashley Library
Closed
Phone: (843) 766-6635
Wando Mount Pleasant Library
Closed
Phone: (843) 805-6888
Village Library
Closed
Phone: (843) 884-9741
St. Paul's/Hollywood Library
Closed
Phone: (843) 889-3300
Otranto Road Library
Closed
Phone: (843) 572-4094
Mt. Pleasant Library
Closed
Phone: (843) 849-6161
McClellanville Library
Closed
Phone: (843) 887-3699
Keith Summey North Charleston Library
Closed
Phone: (843) 744-2489
John's Island Library
Closed
Phone: (843) 559-1945
Hurd/St. Andrews Library
Closed
Phone: (843) 766-2546
Folly Beach Library
Closed
Phone: (843) 588-2001
Edisto Island Library
Closed
Phone: (843) 869-2355
Dorchester Road Library
Closed
Phone: (843) 552-6466
John L. Dart Library
Closed
Phone: (843) 722-7550
Baxter-Patrick James Island
Closed
Phone: (843) 795-6679
Main Library
2 p.m. – 5 p.m.
Phone: (843) 805-6930
Bees Ferry West Ashley Library
Closed
Phone: (843) 805-6892
Edgar Allan Poe/Sullivan's Island Library
Closed for renovations
Phone: (843) 883-3914
Mobile Library
Closed
Phone: (843) 805-6909
Patron Login
menu
Item request has been placed!
×
Item request cannot be made.
×
Processing Request
Winter Insolation Modulates Boreal Tropical Monsoonal Temperatures in the Late Pleistocene.
Item request has been placed!
×
Item request cannot be made.
×
Processing Request
- Author(s): Dai, Gaowen1 (AUTHOR); Zhang, Zhongshi2,3 (AUTHOR) ; Otterå, Odd Helge4,5 (AUTHOR); Langebroek, Petra M.4 (AUTHOR); Yan, Qing6 (AUTHOR); Zhang, Ran7 (AUTHOR); Zhu, Zongmin1 (AUTHOR)
- Source:
Journal of Geophysical Research. Atmospheres. Apr2024, Vol. 129 Issue 8, p1-13. 13p.- Subject Terms:
- Source:
- Additional Information
- Subject Terms:
- Abstract: During past glacial‐interglacial cycles, the boreal summer insolation is the most crucial external forcing for climate change. However, the question of whether summer insolation is a key forcing on temperatures in the boreal tropics remains under debate, hampering our understanding of climate change at low latitudes. To shed further light on this issue, we performed a series of equilibrium simulations with the NorESM‐L model over the past 425 ka. Our simulations show that in the boreal tropical monsoon region, the simulated annual temperature is anti‐phased towards the boreal summer insolation. This antiphase relation is also supported by some available geological data. Additional diagnostic analyses reveal that the tropical warmth throughout the year is more reliant on winter temperatures than on summer temperatures. This stands in contrast to the situation in middle to high latitudes, particularly in the Mediterranean region. Further correlation analysis and spectrum analysis suggest that the annual temperature in boreal tropics is highly linked to local winter insolation. Our results highlight complex hydrothermal configurations in the boreal tropics, suggesting a decoupling of temperature and precipitation. Specifically, variations in annual temperature and precipitation in the boreal tropics are driven by distinct patterns of seasonal insolation. We deduce that the unique hydrothermal configurations in North Africa may have influenced the dispersal of early humans out of Africa. Plain Language Summary: On the orbital timescale, whether the temperature in boreal tropics is driven by boreal summer insolation still remains unclear. In this study, we conduct a comprehensive analysis of simulated results spanning the 425 ka. Our findings indicate that the annual temperature in boreal tropics is anti‐phased to the local summer insolation. Specifically, when local summer insolation is high (low), overall cooling (warming) occurs in the North African and South Asian monsoon regions. Some available paleo‐temperature records from the tropics also provide partial support for our simulation results. The temperature pattern in the boreal tropics is linked to the strong internal feedback in the summer from the unique climate background of the tropics, which results in relatively slight summer cooling at high boreal summer insolation, while the annual temperature is largely dependent on winter temperatures driven by local winter insolation. Our simulations reveal highly complex hydrothermal configurations in the boreal tropics on the orbital timescale, suggesting a decoupling of temperature and precipitation, with the former influenced by winter insolation and the latter forced by summer insolation. Key Points: The temperature in boreal tropical monsoon regions is anti‐phased to the boreal summer insolationThe annual temperature in boreal tropics is more dependent on the winter than summer temperaturesThe key role of local winter insolation in regulating the boreal tropical temperature is closely linked to its unique climatic background [ABSTRACT FROM AUTHOR]
- Abstract: Copyright of Journal of Geophysical Research. Atmospheres is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
Contact CCPL
Copyright 2022 Charleston County Public Library Powered By EBSCO Stacks 3.3.0 [350.3] | Staff Login
No Comments.