{"title":"Understanding climate modes’ impact on the Indian Ocean decadal upwelling variability","authors":"Xiaolin Zhang","doi":"10.18686/jaoe.v11i1.9466","DOIUrl":null,"url":null,"abstract":"<p align=\"justify\">This study explores the spatial pattern and climate modes’ impact on the Indian Ocean decadal upwelling variability by using observational dataset, Static Linear Regression Model (SLM) and Bayesian Dynamic Linear Model (BDLM). Our analysis shows that the Indian Ocean decadal upwellings averaged in the Eastern and Western Indian Ocean (EIO and WIO) regions are positively correlated. Moreover, the BDLM that represents the temporal modulations of the El Niño and Southern Ocean (ENSO) and Indian Ocean Dipole (IOD) impacts, reproduces the time series of the EIO and WIO upwellings more realistically than a conventional SLM does. BD<span style=\"font-family: 'Times New Roman';\">L</span>M simulations further suggest that in both EIO and WIO, IOD is more important than ENSO impact. The time-varying regression coefficients in BDLM indicate that the observed shift of the IOD impact on the EIO upwelling around 1985 is mainly associated with the changes of <span style=\"font-family: 'Times New Roman';\">alongshore </span>wind stress forcing <span style=\"font-family: 'Times New Roman';\">and </span>the sensitivity of the upper <span style=\"font-family: 'Times New Roman';\">ocean </span>temperature <span style=\"font-family: 'Times New Roman';\">in the </span>E<span style=\"font-family: 'Times New Roman';\">IO</span> through the surface warming tendency and the enhanced ocean stratification. This suggests that climate models need to consider the time-varying impact of different climate modes in order to simulate the Indian Ocean dynamics correctly.<strong></strong></p>","PeriodicalId":484200,"journal":{"name":"J of Atmosphere and Oceanography Environment","volume":"30 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2023-10-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"J of Atmosphere and Oceanography Environment","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.18686/jaoe.v11i1.9466","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
This study explores the spatial pattern and climate modes’ impact on the Indian Ocean decadal upwelling variability by using observational dataset, Static Linear Regression Model (SLM) and Bayesian Dynamic Linear Model (BDLM). Our analysis shows that the Indian Ocean decadal upwellings averaged in the Eastern and Western Indian Ocean (EIO and WIO) regions are positively correlated. Moreover, the BDLM that represents the temporal modulations of the El Niño and Southern Ocean (ENSO) and Indian Ocean Dipole (IOD) impacts, reproduces the time series of the EIO and WIO upwellings more realistically than a conventional SLM does. BDLM simulations further suggest that in both EIO and WIO, IOD is more important than ENSO impact. The time-varying regression coefficients in BDLM indicate that the observed shift of the IOD impact on the EIO upwelling around 1985 is mainly associated with the changes of alongshore wind stress forcing and the sensitivity of the upper ocean temperature in the EIO through the surface warming tendency and the enhanced ocean stratification. This suggests that climate models need to consider the time-varying impact of different climate modes in order to simulate the Indian Ocean dynamics correctly.
<p align="justify">利用观测数据、静态线性回归模型(SLM)和贝叶斯动态线性模型(BDLM),探讨了空间格局和气候模式对印度洋年代际上升流变率的影响。分析表明,东印度洋和西印度洋(EIO和WIO)区域的年代际平均上升流是正相关的。此外,BDLM代表了El Niño和南大洋(ENSO)以及印度洋偶极子(IOD)影响的时间调制,比传统的SLM更真实地再现了EIO和WIO上升流的时间序列。BD<span style="font-family: 'Times New Roman';">L</span>M模拟进一步表明,在EIO和WIO中,IOD的影响比ENSO的影响更重要。BDLM的时变回归系数表明,1985年前后观测到的IOD对EIO上升流影响的变化主要与<span style="font-family: 'Times New Roman'; >沿岸</span>风应力作用<span style="font-family: 'Times New Roman';">和</span>上部<span style="font-family: 'Times New Roman';">海洋</span>温度<span style="font-family: 'Times New Roman';"font-family:宋体";" font-family:宋体";通过地表变暖趋势和海洋分层增强。这表明,为了正确地模拟印度洋动力学,气候模型需要考虑不同气候模式的时变影响。