单位质量的物质从0°C加热到T°C所需的热量称为该物质在T°C时的热含量。
In addition, the upper heat storage and the thermocline in the tropical Pacific also contain the westward signals of 10-year period.
另外，热带太平洋上层热含量和温跃层还存在准10年际的西行信号。
参考来源 - 太平洋年代际变化及其非线性作用机制初探Compared with the early onset monsoon years,the features of the winter-spring heat content over the SCS holds the opposite polarity during the late onset years.
季风爆发早、晚年的冬春季,南海中南部热含量呈反位相变化。
参考来源 - 南海夏季风爆发与冬春季南海上层海洋热含量关系的初探·2,447,543篇论文数据，部分数据来源于NoteExpress
在实际工程上有意义的只是热含量之差。
Only differences in enthalpy are of practical engineering interest.
热带西北太平洋西部热含量增加时，副热带高压脊点偏西，移入南海的热带气旋频数增加，反之减少。
When heat content increased, the ridge point of subtropical high moved more westly, and frequency of tropical cyclone moving from Pacific into South China Sea increased, otherwise it decreased;
模拟的ENSO位相转换机制与 “充电—放电” 概念模型相符合， 赤道太平洋热含量的变化是维持ENSO振荡的机制。
The negative feedback of ENSO is explained by the "Recharge-Discharge Oscillator" theory, in which the change of the equatorial Pacific Ocean heat content acts as an important transitioner for ENSO.
应用推荐