ice concentration meaning in Chinese
冰集中程度
冰浓度
覆冰量
海冰密集度
Examples
- ( 3 ) using the csim4 , the arctic sea ice equilibrium state was simulated reasonably . the simulated ice thickness distribution pattern very like that detected by submarine investigations . the simulated ice concentration and motion are similar to the observation
模拟的海冰厚度分布与潜艇探测的海冰厚度分布具有一致性；模拟的海冰密集度、海冰流速与观测相近，模拟的海冰气候态是合理的。 - Based on the arctic sea ice concentration data and the ncep / ncar reanalysis data , the contemporaneous relationship of the winter sea ice in the sea of okhotsk and its adjacent sea areas with the northern pacific storm track is investigated by statistical analysis methods
摘要利用北极海冰密集度资料和ncep / ncar再分析资料，运用统计方法讨论了冬季鄂霍次克海及其邻近海区海冰异常与同期北太平洋风暴轴的联系。 - Based on the ncep / ncar reanalysis products , the sea ice concentration data and the observation rainfall data in china , the seasonal , intraseasonal and interannual variations of the atmospheric circulation in the southern hemisphere ( sh ) are systematically analyzed together with their influences on east asian summer monsoon ( easm ) . the major conclusions are summarized as follows : ( 1 ) in the lower level of the troposphere , the semi - annual oscillation ( sao ) is most active along 40 s and 65 s in the extratropics of the sh . over these latitudes , the variance percentages of sao exceed 70 % , and the anti - phase variation of the sea level pressure ( slp ) between the two latitudes is primarily caused by their sao components
利用ncep ncar再分析资料、南半球海冰密度资料及中国台站降水资料，本文系统分析了南半球大气环流的季节、季节内和年际变化特征及其对东亚夏季风的影响，主要结论归纳如下： ( 1 )对南半球热带外大气环流而言， 40 s和65 s是低层大气准半年振荡最为显著的两个纬带，在这两个纬带上，半年波的贡献都超过了70 ，二者季节变化的反位相主要体现为半年波分量的反位相。 - Based on observed sea ice concentration data and simulated results , there has been noticeable downward trend in the extent of arctic sea ice during 1979 - 1998 . the model shows a substantial reduction of ice advection into the eastern arctic from the canada basin , and an increase of ice export through fram strait , both of which tend to deplete the sea ice of arctic
模拟结果表明北极海冰有很明显的季节变化和年际变化，实测的海冰密集度资料和模式模拟结果都证明1979 - 1998这20年间北极海冰的一个最明显的变化是海冰在不断减少。