In areas near the equator

Trade creation abbreviations create favorable conditions. , celestial winds are caused by interference between the two hemispherescreating upward drifting convection currents of air. Therefore, celestial winds are usually quiet or blowing very lightly at the surface. This forms the Sagittarius or a region called the Intertropical Convergence Zone. Tianfeng wind originates from the high pressure center in the Pacific Ocean and blows towards the equator from there. The sign is white which originates from high pressure areas at horse latitudes blowing into low letter and pressure areas around the equator. Tianfeng wind is a true subtropical high pressure belt generated by the two hemispheres.



Generated pedicle abbreviation. The origin of the Tianfeng wind The origin of the Tianfeng wind is at the equator. The Tianfeng wind blows from two half-way license plate balls and merges here to form a highly rising convection. Therefore the effect of wind is weaker and quieter closer to the surface. In the northern hemisphere, the wind direction is mainly Job Function Email List or southwest, while in the southern hemisphere, the wind direction is southeast or northwest due to the influence of the Coriolis force. When the celestial wind appears, it is white and usually blows eastward in the summer and is kilometers above the equator. On the upper floorsthe wind is blowing against the sky and to the west. This is compliance with the spin.






Rotational motility Abbreviation Consequences of the law of conservation of momentum. Characteristics of Tianfang Wind Tianfeng wind has obvious characteristics that affect the climate of the area it passes through. First, the Tianfeng wind blows from the sea bringing a cool breeze. When this wind moves inland it creates some special climate characteristicsespecially in the northern delta and coastal areas. Characteristics of Tianfangfeng Characteristics of Tianfangfeng The number of Tianfengfeng is white, which originates from the Pacific high pressure center. The air pressure in this area is higher than that of surrounding areas. So the wind starts moving from there. With the production of high pressure.