SMOS 捕捉到厄尔尼诺和拉尼娜期间 SSS 锋面的变化

IF 2.5 4区 环境科学与生态学 Q3 ENVIRONMENTAL SCIENCES
Jiahao Li and Ling Du
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引用次数: 0

摘要

土壤水分和海洋盐度(SMOS)卫星的发射促进了对海面盐度(SSS)和盐度锋面(SF)的研究。太平洋中部的盐度锋受厄尔尼诺和拉尼娜现象的影响,其中涉及的物理过程非常复杂。在这项研究中,我们用一种简单直观的方法评估了巴塞罗那专家中心(BEC)的 SMOS 产品检索 SF 的能力。此外,本研究还调查了 SF 的季节变化及其对厄尔尼诺和拉尼娜事件的响应。SMOS BEC L4 SSS 的精度足以研究 SF。通过选择合理的SF阈值并分析其位置和强度,在赤道太平洋中部,SF可分为两种:北部和南部SF。北部 SF 的变化主要受热带辐合带(ITCZ)移动的影响,而淡水通量和盐分平流是南部 SF 的主要因素。它们通过淡水通量和盐分平流与厄尔尼诺和拉尼娜事件相对应。这些发现可为基于卫星数据的 SF 研究提供信息,并加深我们对厄尔尼诺南方涛动(ENSO)动力学的理解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
SMOS captures variations in SSS fronts during El Niño and La Niña
The launch of the Soil Moisture and Ocean Salinity (SMOS) satellite has promoted research on sea surface salinity (SSS) and salinity fronts (SF). The SF in the central Pacific Ocean is influenced by El Niño and La Niña events, and the physical processes involved are complex. In this study, we evaluated the ability of the SMOS product from the Barcelona Expert Centre (BEC) to retrieve SF using a simple and intuitive method. Furthermore, this study investigated seasonal variations in the SF and its response to El Niño and La Niña events. The accuracy of the SMOS BEC L4 SSS is sufficient for studying SF. By selecting reasonable SF thresholds and analyzing its locations and intensities, in the central equatorial Pacific Ocean, SF can be divided into two: northern and southern SF. The variability in the northern SF is primarily influenced by the migration of the intertropical convergence zone (ITCZ), whereas both freshwater flux and salt advection are the primary factors in the southern SF. They correspond to El Niño and La Niña events through freshwater flux and salt advection. These findings can provide information for the study of the SF based on satellite data and enhance our understanding of El Niño Southern Oscillation (ENSO) dynamics.
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来源期刊
Environmental Research Communications
Environmental Research Communications ENVIRONMENTAL SCIENCES-
CiteScore
3.50
自引率
0.00%
发文量
136
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