Triple oxygen isotope reveals insolation-forced tropical moisture cycles
(2024) In Science Advances 10(37).- Abstract
Tropical oceans are the main global water vapor and latent heat sources, but their responses to radiative forcing remain unclear. Here, we investigate oceanic moisture dynamics of the western tropical Pacific (WTP) over the past 210,000 years through an approach of planktonic foraminiferal triple oxygen isotope (Δ′17O). The Δ′17O record is dominated by the precession cycles (~23,000 years), with lower values reflecting higher humidity in concert with higher Northern Hemisphere summer insolation. Our empirical and modeling results, combined with other geological archives, suggest that the enhanced moisture convergence over the WTP largely intensifies changes in the meridional and zonal hydrological cycles, affecting... (More)
Tropical oceans are the main global water vapor and latent heat sources, but their responses to radiative forcing remain unclear. Here, we investigate oceanic moisture dynamics of the western tropical Pacific (WTP) over the past 210,000 years through an approach of planktonic foraminiferal triple oxygen isotope (Δ′17O). The Δ′17O record is dominated by the precession cycles (~23,000 years), with lower values reflecting higher humidity in concert with higher Northern Hemisphere summer insolation. Our empirical and modeling results, combined with other geological archives, suggest that the enhanced moisture convergence over the WTP largely intensifies changes in the meridional and zonal hydrological cycles, affecting rainfall patterns in East Asia and northern South America. We propose that the insolation-driven WTP moisture dynamics play a pivotal role in regulating tropical hydroclimate.
(Less)
- author
- organization
- publishing date
- 2024-09
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Science Advances
- volume
- 10
- issue
- 37
- article number
- eadp7855
- publisher
- American Association for the Advancement of Science (AAAS)
- external identifiers
-
- pmid:39259794
- scopus:85204167567
- ISSN
- 2375-2548
- DOI
- 10.1126/sciadv.adp7855
- language
- English
- LU publication?
- yes
- id
- 2c09037d-6c7a-41ae-b2b5-a4d20e532f5f
- date added to LUP
- 2024-11-22 09:29:20
- date last changed
- 2025-07-05 05:12:31
@article{2c09037d-6c7a-41ae-b2b5-a4d20e532f5f, abstract = {{<p>Tropical oceans are the main global water vapor and latent heat sources, but their responses to radiative forcing remain unclear. Here, we investigate oceanic moisture dynamics of the western tropical Pacific (WTP) over the past 210,000 years through an approach of planktonic foraminiferal triple oxygen isotope (Δ′<sup>17</sup>O). The Δ′<sup>17</sup>O record is dominated by the precession cycles (~23,000 years), with lower values reflecting higher humidity in concert with higher Northern Hemisphere summer insolation. Our empirical and modeling results, combined with other geological archives, suggest that the enhanced moisture convergence over the WTP largely intensifies changes in the meridional and zonal hydrological cycles, affecting rainfall patterns in East Asia and northern South America. We propose that the insolation-driven WTP moisture dynamics play a pivotal role in regulating tropical hydroclimate.</p>}}, author = {{Sha, Lijuan and Dang, Haowen and Wang, Yue and Wassenburg, Jasper A. and Baker, Jonathan L. and Li, Hanying and Sinha, Ashish and Brahim, Yassine Ait and Wu, Nanping and Lu, Zhengyao and Yang, Ce and Dong, Xiyu and Lu, Jiayu and Zhang, Haiwei and Mahata, Sasadhar and Cai, Yanjun and Jian, Zhimin and Cheng, Hai}}, issn = {{2375-2548}}, language = {{eng}}, number = {{37}}, publisher = {{American Association for the Advancement of Science (AAAS)}}, series = {{Science Advances}}, title = {{Triple oxygen isotope reveals insolation-forced tropical moisture cycles}}, url = {{http://dx.doi.org/10.1126/sciadv.adp7855}}, doi = {{10.1126/sciadv.adp7855}}, volume = {{10}}, year = {{2024}}, }