Intensification of Decadal Variability in Sea Surface Salinity in the Western Tropical Pacific

Abstract The decadal variability of sea surface salinity (SSS) is crucial for the global water cycle and the climate system. Previous studies have indicated that the SSS in the western tropical Pacific (WTP) Ocean exhibits significant decadal variability, which plays an important role in shaping tropical climate. Here we find that the amplitude of SSS decadal variability in the WTP has been intensified significantly since the early 1950s. A comprehensive analysis of the salinity budget indicates that the amplifying of SSS decadal variability in the WTP is primarily attributed to changes in both the freshwater flux and ocean dynamics. During the past decades, surface currents in the WTP get stronger and result in enhanced salinity advection. In addition, the amplitude of decadal variability of freshwater flux is increased as well due to anomalous atmospheric circulation associated with the Victoria mode.

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Publication Details

Journal
Geophysical Research Letters
Published
2025-02-28
DOI
https://doi.org/10.1029/2024gl113453
Primary Topic
Climate variability and models
Type
article
Field-Weighted Citation Impact
0.00

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article

Intensification of Decadal Variability in Sea Surface Salinity in the Western Tropical Pacific

Shijian Hu, Guanghui Zhou, Yue Wu
Geophysical Research Letters
Climate variability and models
article

Intensification of Decadal Variability in Sea Surface Salinity in the Western Tropical Pacific

Shijian Hu, Guanghui Zhou, Yue Wu
article en

Abstract

Abstract The decadal variability of sea surface salinity (SSS) is crucial for the global water cycle and the climate system. Previous studies have indicated that the SSS in the western tropical Pacific (WTP) Ocean exhibits significant decadal variability, which plays an important role in shaping tropical climate. Here we find that the amplitude of SSS decadal variability in the WTP has been intensified significantly since the early 1950s. A comprehensive analysis of the salinity budget indicates that the amplifying of SSS decadal variability in the WTP is primarily attributed to changes in both the freshwater flux and ocean dynamics. During the past decades, surface currents in the WTP get stronger and result in enhanced salinity advection. In addition, the amplitude of decadal variability of freshwater flux is increased as well due to anomalous atmospheric circulation associated with the Victoria mode.

Geophysical Research LettersVol. 52(5)
Shaoxing University (CN), Institute of Oceanology (CN), Shenyang Environmental Protection Bureau (CN), Qingdao National Laboratory for Marine Science and Technology (CN), University of Chinese Academy of Sciences (CN)
Qingdao Postdoctoral Science Foundation, Youth Innovation Promotion Association
Openalex Percentile: Top 97%
Climate variability and models
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