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.
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