2013/2014年中国第30次南极考察长城站温盐数据

2014年2月份对长城站附近的长城湾、阿德雷湾10个站位分层采集样品，进行了温盐剖面测定。温盐就是温度和盐度。全球气候变暖所致海水在空间上存在着的温度和盐度的差异使密度发生变化进而导致深层海水的缓慢运动称之为温盐海流。温盐环流是一个大尺度的海洋环流，由温度及含盐度的差异所致。

In February 2014, stratified sampling was conducted at 10 stations in Great Wall Bay and Ardley Bay near the Great Wall Station, followed by temperature-salinity profile measurements. Temperature-salinity refers to both water temperature and salinity. Thermohaline currents are defined as the slow movements of deep seawater driven by changes in seawater density, which stem from spatial differences in water temperature and salinity caused by global climate warming. Thermohaline circulation is a large-scale ocean circulation driven by differences in water temperature and salinity.