Answer:
Because at those latitudes the jet stream, which is a very high altitude wind, always blows from the West to the East. The planes moving at a constant air speed thus go faster in the West-East direction when they are moving with the wind than in the opposite direction.
Explanation:
Answer : B. dissipation.
The third stage in the development of a full tropical cyclone is the dissipation stage together with the formative and mature stage. In the formative stage, moist air moves upward causing rainfall and the circulation of the air. The cyclonic rotation is produced as more moist air are lifted. The mature stage is characterized by the increased wind speed and the sudden drop of the pressure while in the dissipation stage, the cyclone has gone weaker.
Physical geography is the branch of geography dealing with the natural features and the processes
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