The observational sea surface temperature(SST)data from 1960 to 2017 of the Chengshantou marine station has been adjusted by the Penalized Maximal Test(PMT)developed by the Climate Research Center of the Environment M...The observational sea surface temperature(SST)data from 1960 to 2017 of the Chengshantou marine station has been adjusted by the Penalized Maximal Test(PMT)developed by the Climate Research Center of the Environment Ministry of Canada,based on the metadata archive.In this study,the homogenous surface air temperature(SAT)data from neighboring meteorological observation stations are used to construct the reference series by correlation coefficient weighted averaged method.The climate change characteristics of the Chengshantou SST were analyzed using the homogenized data.Results show that the annual average SST trend has changed significantly before and after the homogenization.The warming trend increased from 0.04℃/10 a before revision to 0.15℃/10 a.The warmest five years occurred mostly after 1980,that is,1973,1989,2002,2007 and 2017.SST generally showed a significant upward trend and significant inter-decadal fluctuations.From the 1960s to the end of the 1980s,it was a colder stage,and then began to warm up.It was a warmer period from the 1990s to the present.From 1960 to 2017,the jump point occurred in 1987,which is very consistent with the temperature characteristics of China's mainland.展开更多
The climate distribution and variation characteristics of temperature and salinity i n the upper surface layer of Sulawesi Sea(117-127°E,0-8°N)were analyzed using Argo T/S profiles of 0-1500 m and XBT temper...The climate distribution and variation characteristics of temperature and salinity i n the upper surface layer of Sulawesi Sea(117-127°E,0-8°N)were analyzed using Argo T/S profiles of 0-1500 m and XBT temperature profiles obtained by Chinese Antarctic scientific investigation.The results show that the temperature and salinity are respectively about 2.5℃-30℃ and 33.2‰-35.1‰ in the Sulawesi sea.Compared with the vertical changes,the T/S horizontal gradients are smaller.The temperatures gradually reduce with the in crease of the depth.The sali nities increase firstly,then decrease,and increase finally with the increase of depth.The salinity has two lower and one higher salinity areas.The whole sea surface shows the characteristics of high temperature and low salinity.T he subsurface temperature is slightly lower with salinity increasing.Middle depths are characterized by high temperature and high salinity.At the depth of 500 m,the temperature and salinity tend to be uniform.And at the bottom,T/S represent lower temperature with higher salinity.Moreover,an obvious thermocline exists at the depth of 50 m-150 m.The thermocline depth in summer is less than 90 m and is about 110 m in winter.The thermocline exists in the deeper depth in April than that of November by XBT observation sections.In the central of Sulawesi Sea,the thermocline is also relatively deeper.展开更多
文摘The observational sea surface temperature(SST)data from 1960 to 2017 of the Chengshantou marine station has been adjusted by the Penalized Maximal Test(PMT)developed by the Climate Research Center of the Environment Ministry of Canada,based on the metadata archive.In this study,the homogenous surface air temperature(SAT)data from neighboring meteorological observation stations are used to construct the reference series by correlation coefficient weighted averaged method.The climate change characteristics of the Chengshantou SST were analyzed using the homogenized data.Results show that the annual average SST trend has changed significantly before and after the homogenization.The warming trend increased from 0.04℃/10 a before revision to 0.15℃/10 a.The warmest five years occurred mostly after 1980,that is,1973,1989,2002,2007 and 2017.SST generally showed a significant upward trend and significant inter-decadal fluctuations.From the 1960s to the end of the 1980s,it was a colder stage,and then began to warm up.It was a warmer period from the 1990s to the present.From 1960 to 2017,the jump point occurred in 1987,which is very consistent with the temperature characteristics of China's mainland.
文摘The climate distribution and variation characteristics of temperature and salinity i n the upper surface layer of Sulawesi Sea(117-127°E,0-8°N)were analyzed using Argo T/S profiles of 0-1500 m and XBT temperature profiles obtained by Chinese Antarctic scientific investigation.The results show that the temperature and salinity are respectively about 2.5℃-30℃ and 33.2‰-35.1‰ in the Sulawesi sea.Compared with the vertical changes,the T/S horizontal gradients are smaller.The temperatures gradually reduce with the in crease of the depth.The sali nities increase firstly,then decrease,and increase finally with the increase of depth.The salinity has two lower and one higher salinity areas.The whole sea surface shows the characteristics of high temperature and low salinity.T he subsurface temperature is slightly lower with salinity increasing.Middle depths are characterized by high temperature and high salinity.At the depth of 500 m,the temperature and salinity tend to be uniform.And at the bottom,T/S represent lower temperature with higher salinity.Moreover,an obvious thermocline exists at the depth of 50 m-150 m.The thermocline depth in summer is less than 90 m and is about 110 m in winter.The thermocline exists in the deeper depth in April than that of November by XBT observation sections.In the central of Sulawesi Sea,the thermocline is also relatively deeper.
