冬季东亚地区海陆热力对比大于观测，夏季海平面气压场整体模拟效果不如冬季；
The model can well capture the East Asia major trough and subtropical high over the western North Pacific at 500 hPa during winter and summer, in spite of larger than observation values.
本模式所求得的全球海平面气压场能与实况相比，结果并不差于高分辨率的复杂模式。
The obtained sea-level pressure fields of our simple model are as good as those computed by using the high resolution general circulation models with the complex physical processes.
海平面气压场表现为陆地上一致性的降低以及副热带海洋和南极洲边缘部分海域的升高。
The sea level pressure will decrease over lands, but increase over the subtropical oceans and parts of the oceans around the Antarctic.
冬季戴维斯海峡海冰在1981年发生突变，突变前后相应高度场、海平面气压场和流场等大气环流场均有显著差异。
There are remarkable differences in 500 hPa heights, SLP, stream fields before and after 1981, when the sea-ice area in Davis Strait abruptly changed.
四种积云对流参数化方案模拟的海平面气压场差别较大，其中GR方案较好地模拟出造成这次暴雨的高低压系统和中尺度气旋。
The simulative sea level pressure of four CPSs showed large difference, in which the GR scheme had better simulated the high, low systems and mesoscale cyclone.
根据新划分的1 90 0 ~ 1 998年东部夏季雨型序列，分析了与各类雨型相对应的北半球海平面气压场和海表温度距平场的特征。
Based on summer rain patterns of east China during 1900 ~ 1998, North Hemisphere SLP and SST anomaly fields for every rain patterns are studied by the use of statistic method.
根据新划分的1 90 0 ~ 1 998年东部夏季雨型序列，分析了与各类雨型相对应的北半球海平面气压场和海表温度距平场的特征。
Based on summer rain patterns of east China during 1900 ~ 1998, North Hemisphere SLP and SST anomaly fields for every rain patterns are studied by the use of statistic method.
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