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| 1 | A study of sea level variability and its long-term trend in the South China Sea显示文摘On the basis of the satellite maps of sea level anomaly(MSLA) data and in situ tidal gauge sea level data,correlation analysis and empirical mode decomposition(EMD) are employed to investigate the applicability of MSLA data,sea level correlation,long-term sea level variability(SLV) trend,sea level rise(SLR) rate and its geographic distribution in the South China Sea(SCS).The findings show that for Dongfang Station,Haikou Station,Shanwei Station and Zhapo Station,the minimum correlation coefficient between the closest MSLA grid point and tidal station is 0.61.This suggests that the satellite altimeter MSLA data are effective to observe the coastal SLV in the SCS.On the monthly scale,coastal SLV in the western and northern part of SCS are highly associated with coastal currents.On the seasonal scale,SLV of the coastal area in the western part of the SCS is still strongly influenced by the coastal current system in summer and winter.The Pacific change can affect the SCS mainly in winter rather than summer and the affected area mostly concentrated in the northeastern and eastern parts of the SCS.Overall,the average SLR in the SCS is 90.8 mm with a rising rate of(5.0±0.4) mm/a during1993–2010.The SLR rate from the southern Luzon Strait through the Huangyan Seamount area to the Xisha Islands area is higher than that of other areas of the SCS. | XU Ying LIN Mingsen ZHENG Quan'an SONG Qingtao YE Xiaomin | 2016 | Acta Oceanologica Sinica2016，35，9： | 1 |
| 2 | Extreme Sea Level Rise off the Northwest Coast of the South China Sea in 2012显示文摘Tide gauge data are used to investigate sea level variability off the northwest coast of the South China Sea(SCS) in 2012,and a significant sea level elevation with a magnitude approaching 79 mm is observed.Analysis suggests that an abnormal sea surface heat flux and freshwater flux may have contributed to this abnormal rise in sea level,together with the remote influence of an ENSO event.Further investigation shows that the event was dominated by the positive freshwater flux,where large volumes of water entered the ocean,and a maximum is centered to the south of Guangdong province,China.Simultaneously,a positive anomalous heat flux occurred in the northwestern part of the SCS,which is considered to have made a positive contribution to the high local sea level elevation.In addition to the heat flux,the ENSO event also had a significant effect on the event,where the La Ni?a-induced northwest Pacific cyclone contributed to sea level rise over the northwestern SCS through dynamic and thermodynamic interactions. | LIU Lin LI Juan TAN Wei WU Yue LIU Yanliang WANG Huiwu | 2018 | Journal of Ocean University of China2018，17，5： | 0 |
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