The causality between atmospheric circulation and thermohaline circulation (THC) is an open question in the field of air-sea interaction.

大气环流与热盐环流(THC)变化之间的因果关系，是海气相互作用研究领域的一个悬而未决的问题。

It is a highly controversial issue that there will be an abrupt and large climate change induced by the reorganization of the Atlantic thermohaline circulation in a warming climate.

未来是否会发生由大西洋热盐环流崩溃引起的气候突变是目前极富争议性的全球气候变化问题。

The dramatic slowing of the thermohaline circulation is anticipated by some ocean researchers, but the United States is not sufficiently prepared for its effects, timing, or intensity.

虽然已有海洋研究者预见到海洋环流会减缓，但美国方面对其影响、强度及发生时间都没有充足准备。

The effects of open boundary and different isopycnal diffusion coefficients on the circulation and thermohaline structure in the North Pacific are examined.

考察了开边界和不同等密面扩散系数对北太平洋环流和温盐结构的影响。