Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1002/2017GL076574 |
Salinification in the South China Sea Since Late 2012: A Reversal of the Freshening Since the 1990s | |
Zeng, Lili1; Chassignet, Eric P.2; Schmitt, Raymond W.3; Xu, Xiaobiao2; Wang, Dongxiao1 | |
2018-03-28 | |
发表期刊 | GEOPHYSICAL RESEARCH LETTERS |
ISSN | 0094-8276 |
EISSN | 1944-8007 |
出版年 | 2018 |
卷号 | 45期号:6页码:2744-2751 |
文章类型 | Article |
语种 | 英语 |
国家 | Peoples R China; USA |
英文摘要 | Salinification has occurred in the South China Sea from late 2012 to the present, as shown by satellite Aquarius/Soil Moisture Active Passive data and Argo float data. This salinification follows a 20year freshening trend that started in 1993. The salinification signal is strongest near the surface and extends downward under the seasonal thermocline to a depth of 150m. The salinification occurs when the phase of the Pacific Decadal Oscillation switches from negative to positive. Diagnosis of the salinity budget suggests that an increasing net surface freshwater loss and the horizontal salt advection through the Luzon Strait driven by the South China Sea throughflow contributed to this ongoing salinification. In particular, a decrease in precipitation and enhanced Luzon Strait transport dominated the current intense salinification. Of particular interest is whether this salinification will continue until it reaches the previous maximum recorded in 1992. Plain Language Summary A significant salinification is taking place in the South China Sea starting from late 2012 to the present, as seen in satellite and Argo float data. The temperature, in contrast, exhibits no significant change. The salinification is mainly associated with switches in the Pacific Decadal Oscillation from negative to positive phase from late 2012 to the present. A decrease in precipitation and enhanced Luzon Strait transport dominated the current intense salinification. After a freshening period that lasted 20years, we are particularly interested in whether the salinification will continue in the future. |
英文关键词 | South China Sea salinification Argo floats Aquarius SMAP PDO |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000430106000022 |
WOS关键词 | PACIFIC DECADAL OSCILLATION ; OCEAN SALINITIES ; VARIABILITY ; TRENDS ; LEVEL ; MODEL |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
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/27377 |
专题 | 气候变化 |
作者单位 | 1.Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou, Guangdong, Peoples R China; 2.Florida State Univ, Ctr Ocean Atmospher Predict Studies, Tallahassee, FL 32306 USA; 3.Woods Hole Oceanog Inst, Dept Phys Oceanog, Woods Hole, MA 02543 USA |
推荐引用方式 GB/T 7714 | Zeng, Lili,Chassignet, Eric P.,Schmitt, Raymond W.,et al. Salinification in the South China Sea Since Late 2012: A Reversal of the Freshening Since the 1990s[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(6):2744-2751. |
APA | Zeng, Lili,Chassignet, Eric P.,Schmitt, Raymond W.,Xu, Xiaobiao,&Wang, Dongxiao.(2018).Salinification in the South China Sea Since Late 2012: A Reversal of the Freshening Since the 1990s.GEOPHYSICAL RESEARCH LETTERS,45(6),2744-2751. |
MLA | Zeng, Lili,et al."Salinification in the South China Sea Since Late 2012: A Reversal of the Freshening Since the 1990s".GEOPHYSICAL RESEARCH LETTERS 45.6(2018):2744-2751. |
条目包含的文件 | 条目无相关文件。 |
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。
修改评论