| 1. | Only differences in enthalpy are of practical engineering interest .
在实际工程上有意义的只是热含量之差。 |
| 2. | The heat content of the earth is very high in comparison to the heat loss of the earth .
与地球的热损耗相比，地球的热含量是很高的。 |
| 3. | The result is generally consistent with that from the world ocean atlas 2001 ( woao1 )
这一计算结果与基于气候态温盐资料计算的热含量季节变化具有很好的一致性。 |
| 4. | Furthermore , the heat storage anomaly of december in the scs can be used as a predictor for the onset of the scs summer monsoon
进一步分析还发现，南海12月份热含量异常可以作为南海夏季风爆发的一种预报指标。 |
| 5. | The interannual and decadal variability of precipitation for yunnan province in rainy season and its relationship with tropical upper layer heat content
云南省雨季降水的年际年代际变化特征及其与热带上层海洋热含量分布的关系 |
| 6. | With the harmonic analysis method , we can find that the heat storage anomaly in the scs has about 0 . 5 , 1 . 5 , 2 . 4 , 4 and 6 years period oscillations besides annual change
对此时间序列进行谐波分析可以看出，南海热含量异常除了具有显著的年变化周期外，还存在明显的0 . 5 、 1 . 5 、 2 . 4 、 4年和6年的变化周期。 |
| 7. | Based on the linear relationship between the sea level variability and heat storage anomaly , the heat storage anomaly in the south china sea ( scs ) is estimated by using merged altimetric data from 1992 to 2004
摘要本文从海面高度异常与海洋热含量变化的线性关系出发，利用1992 ~ 2004年多颗卫星融合海面高度资料，对南海海域的热含量异常进行了计算。 |
| 8. | The correlation analysi s between sst and sea surface height , heat content and depth of thermocline also shows the important role of ocean dynamic processes in some regions , besides the influence of heat exchange between air and sea
Sst与海表面高度、热含量、温跃层深度等的相关分析也表明，在某些区域，除受海洋-大气之间热交换的影响外，海洋动力过程对sst的影响也占重要地位。 |
| 9. | Using monthly temperature and rainfall data of 160 stations in china and global sea surface temperature and heat content data , diagnostic analysis is performed by means of harmonic analysis , correlation analysis , svd and corresponding statistical significance test methods
利用全球海温、热含量、中国160站月平均气温和降水资料，通过周期分析、相关分析和奇异值分解( svd )以及相应的统计学显著性检验方法，分析比较了全球海洋热状况与气候异常的相关联系。 |
| 10. | The result also shows that the heat storage anomaly in the scs has an obvious long - term variability which is a stable interannual variability from 1992 to 1998 , an abrupt change to a high stage in 1998 continuing till 2001 , and a tendency to reduce after 2002
本文得到的结果还显示南海热含量异常具有明显的长周期变化，表现为： 1992 ~ 1998年基本保持比较稳定的年际变化特征， 1998年之后，热含量出现明显的跃变，这一跃变一直维持到2001年，在2002年开始出现热含量的递减趋势。 |
