中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Climatological seasonal variation of the upper ocean salinity

文献类型:期刊论文

作者Liu, Yuanxin1,2,3; Cheng, Lijing3,4,5; Pan, Yuying3,4,5; Abraham, John6; Zhang, Bin4,7; Zhu, Jiang3,4,5; Song, Junqiang1,2
刊名INTERNATIONAL JOURNAL OF CLIMATOLOGY
出版日期2021-11-13
页码22
ISSN号0899-8418
关键词evaporation precipitation salinity seasonal cycle upper ocean
DOI10.1002/joc.7428
通讯作者Cheng, Lijing(chenglij@mail.iap.ac.cn)
英文摘要Salinity plays a vital role in regulating ocean density, stratification and circulation, and is an indicator of the coupling between the ocean, atmosphere and land through the water cycle. This study provides a spatially complete look of the seasonal variation of the upper 2,000 m ocean salinity from regional to global scales, and assesses the robustness of the signals. The potential drivers of this variation are also investigated by comparing salinity changes with surface precipitation and evaporation. New observations show a robust seasonal variation in global ocean salinity from the surface down to 350 m depth that exceeds the observational uncertainty, and in some regions, the variation can be detected at 2,000 m. Regions with a seasonal variation of sea surface salinity (SSS) larger than 0.6 g.kg(-1) include the Northwest Pacific, Northwest Atlantic, tropical oceans and the northeast Indian Ocean. From 5 degrees N to 30 degrees N (20 degrees N to 5 degrees N), the sea surface is fresher (saltier) in the first half of the year and gets saltier (fresher) in the second half of the year, because of surface precipitation and evaporation changes associated with monsoons and the seasonal changes in atmospheric circulation. In the middle and high latitudes, the evaporation-minus-precipitation is mismatched with local salinity changes, suggesting that river runoff, sea ice change and ocean dynamics have a controlling role. On zonal average, the subsurface (50-160 m) generally shows salinity anomalies with an opposite sign to those of the near surface regions (0-50 m), indicating the importance of ocean dynamics. There are notable differences in global SSS variation between Argo-only products and datasets that merge all observations, revealing the insufficiency of Argo network in shallow oceans and polar regions. To overcome this, an integrated ocean observational network is strongly recommended.
资助项目Key Deployment Project of Centre for Ocean Mega-Research of Science, CAS[COMS2019Q01] ; National Key R&D Program of China[2017YFA0603202]
WOS研究方向Meteorology & Atmospheric Sciences
语种英语
出版者WILEY
WOS记录号WOS:000718013200001
源URL[http://ir.qdio.ac.cn/handle/337002/177224]  
专题中国科学院海洋研究所
通讯作者Cheng, Lijing
作者单位1.Natl Univ Def Technol, Coll Meteorol & Oceanog, Changsha, Peoples R China
2.Natl Univ Def Technol, Coll Comp Sci & Technol, Changsha, Peoples R China
3.Chinese Acad Sci, Int Ctr Climate & Environm Sci, Inst Atmospher Phys, Beijing 100029, Peoples R China
4.Chinese Acad Sci, Ctr Ocean Megasci, Qingdao, Peoples R China
5.Univ Chinese Acad Sci, Beijing, Peoples R China
6.Univ St Thomas, Sch Engn, St Paul, MN USA
7.Chinese Acad Sci, Marine Sci Data Ctr, Inst Oceanol, Qingdao, Peoples R China
推荐引用方式
GB/T 7714
Liu, Yuanxin,Cheng, Lijing,Pan, Yuying,et al. Climatological seasonal variation of the upper ocean salinity[J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY,2021:22.
APA Liu, Yuanxin.,Cheng, Lijing.,Pan, Yuying.,Abraham, John.,Zhang, Bin.,...&Song, Junqiang.(2021).Climatological seasonal variation of the upper ocean salinity.INTERNATIONAL JOURNAL OF CLIMATOLOGY,22.
MLA Liu, Yuanxin,et al."Climatological seasonal variation of the upper ocean salinity".INTERNATIONAL JOURNAL OF CLIMATOLOGY (2021):22.

入库方式: OAI收割

来源:海洋研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。