change of ocean circulation pattern
We can provide proper circulation patterns and sufficient make up.
on the 500Hpa circulation pattern, one rainstorm is belongs to west-south airflow and the other belongs to west low-trough but the directness react system on 700Hpa is alike.
These swings trigger changes in atmospheric circulation patterns that, while most prominent in the tropics, also affect circulation patters at higher latitudes as well.
Results using routine surface meteorological variables show that we can get airmass categories each having distinct feature and circulation pattern by the methodology.
The connection between profile characteristics of the westerlies and seasonal characters of atmospheric circulation pattern are studied used observation data.
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