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DOI | 10.1175/JCLI-D-19-0056.1 |
Interannual to Decadal Variability of Upper-Ocean Salinity in the Southern Indian Ocean and the Role of the Indonesian Throughflow | |
Hu, Shijian1,2,3,4; Zhang, Ying5,6,7; Feng, Ming7,8; Du, Yan5,6; Sprintall, Janet9; Wang, Fan1,3; Hu, Dunxin1,3; Xie, Qiang5,10; Chai, Fei2 | |
2019-10-01 | |
发表期刊 | JOURNAL OF CLIMATE |
ISSN | 0894-8755 |
EISSN | 1520-0442 |
出版年 | 2019 |
卷号 | 32期号:19页码:6403-6421 |
文章类型 | Article |
语种 | 英语 |
国家 | Peoples R China; Australia; USA |
英文摘要 | Variability of oceanic salinity, an indicator of the global hydrological cycle, plays an important role in the basin-scale ocean circulation. In this study, interannual to decadal variability of salinity in the upper layer of the Indian Ocean is investigated using Argo observations since 2004 and data assimilating model outputs (1992-2015). The southeastern Indian Ocean shows the strongest interannual to decadal variability of upper-ocean salinity in the Indian Ocean. Westward propagation of salinity anomalies along isopycnal surfaces is detected in the southern Indian Ocean and attributed to zonal salinity advection anomalies associated with the Indonesian Throughflow and the South Equatorial Current. Composite and salinity budget analyses show that horizontal advection is a major contributor to the interannual to decadal salinity variability of the southern Indian Ocean, and the local air-sea freshwater flux plays a secondary role. The Pacific decadal oscillation (PDO) and El Nino-Southern Oscillation (ENSO) modulate the salinity variability in the southeastern Indian Ocean, with low salinity anomalies occurring during the negative phases of the PDO and ENSO and high salinity anomalies during their positive phases. The Indonesian Throughflow plays an essential role in transmitting the PDO- and ENSO-related salinity signals into the Indian Ocean. A statistical model is proposed based on the PDO index, which successfully predicts the southeastern Indian Ocean salinity variability with a lead time of 10 months. |
英文关键词 | Indian Ocean Advection Atmosphere-ocean interaction ENSO Ocean circulation Thermocline |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000484615400001 |
WOS关键词 | BARRIER-LAYER THICKNESS ; SEA-SURFACE SALINITY ; MIXED-LAYER ; SOIL-MOISTURE ; PACIFIC ; DIPOLE ; SCALE ; AQUARIUS ; IMPACT ; BUDGET |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/187424 |
专题 | 气候变化 |
作者单位 | 1.Chinese Acad Sci, Ctr Ocean Mega Sci, Inst Oceanol, Key Lab Ocean Circulat & Waves, Qingdao, Shandong, Peoples R China; 2.State Ocean Adm, Inst Oceanog 2, State Key Lab Satellite Ocean Environm Dynam, Hangzhou, Zhejiang, Peoples R China; 3.Pilot Natl Lab Marine Sci & Technol Qingdao, Qingdao, Shandong, Peoples R China; 4.Univ Chinese Acad Sci, Coll Marine Sci, Qingdao, Shandong, Peoples R China; 5.Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou, Guangdong, Peoples R China; 6.Univ Chinese Acad Sci, Beijing, Peoples R China; 7.CSIRO Oceans & Atmosphere, Crawley, WA, Australia; 8.CSIRO Oceans & Atmosphere, Ctr Southern Hemisphere Oceans Res, Hobart, Tas, Australia; 9.Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA; 10.Chinese Acad Sci, Inst Deep Sea Sci & Engn, Sanya, Peoples R China |
推荐引用方式 GB/T 7714 | Hu, Shijian,Zhang, Ying,Feng, Ming,et al. Interannual to Decadal Variability of Upper-Ocean Salinity in the Southern Indian Ocean and the Role of the Indonesian Throughflow[J]. JOURNAL OF CLIMATE,2019,32(19):6403-6421. |
APA | Hu, Shijian.,Zhang, Ying.,Feng, Ming.,Du, Yan.,Sprintall, Janet.,...&Chai, Fei.(2019).Interannual to Decadal Variability of Upper-Ocean Salinity in the Southern Indian Ocean and the Role of the Indonesian Throughflow.JOURNAL OF CLIMATE,32(19),6403-6421. |
MLA | Hu, Shijian,et al."Interannual to Decadal Variability of Upper-Ocean Salinity in the Southern Indian Ocean and the Role of the Indonesian Throughflow".JOURNAL OF CLIMATE 32.19(2019):6403-6421. |
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