Information derived from sequence data is inherently static, and most interaction data sets are measured in a static way as well.
来源于序列数据的信息是固有地静态的，并大部分相互作用数据集也以一种静态的方式来测量。
Orographic static data needed in the gravity wave drag physics are recomputed and validated through comparing with the original static data from the ECMWF model.
重新计算了地形重力波过程需要的地形静态资料数据，并与原ecmWF模式的地形静态参数进行了对比分析，验证了模式地形参数的正确性。
Orographic static data needed in the gravity wave drag physics are recomputed and validated through comparing with the original static data from the ECMWF model.
重新计算了地形重力波过程需要的地形静态资料数据，并与原ecmWF模式的地形静态参数进行了对比分析，验证了模式地形参数的正确性。
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