the general surface wind circulation associated with the high-pressure center (h) is most likely
High-pressure area Winds within high-pressure areas flow outward from the higher pressure areas near their centers towards the lower pressure areas further from their centers. Gravity adds to the forces causing this general movement, because the higher pressure compresses the column of air near the center of the area into greater density â€“ and so greater weight compared to lower pressure, lower density, and lower weight of the air outside the center.
Mistral (wind) The mistral (Catalan: Mestral, Greek: Μαΐστρος, Italian: Maestrale, Corsican: Maestral) is a strong, cold, northwesterly wind that blows from southern France into the Gulf of Lion in the northern Mediterranean, with sustained winds often exceeding 66 km/h (41 mph), sometimes reaching 185 km/h (115 mph).[1] It is most common in the winter and spring, and strongest in the transition between the two seasons. Periods of the wind exceeding 30 km/h (19 mph) for more than sixty-five hours have been reported.[2]