what's the answer
The ocean zone characterized by high water pressure, low temperatures, and no sunlight is the hadal zone. This zone extends from depths of 19,685 to 36,100 feet (6,000 to 11,000 meters) and is found in deep ocean trenches. Organisms living in this zone must adapt to extreme conditions, such as lack of sunlight and high pressure.
The zone is called a front. There are a few types of fronts. They are: cold front, warm front, occluded front & stationary front.
No, the Intertropical Convergence Zone (ITCZ) is a region near the equator where the trade winds converge, creating low pressure. As warm, moist air rises in this zone, it can lead to the formation of thunderstorms and heavy rainfall.
Wind moves from high pressure to low pressure. Air always moves from areas of high pressure to areas of low pressure in an attempt to equalize pressure differences.
abyssal zone
what's the answer
abyssal zone
The ocean zone characterized by high water pressure, low temperatures, and no sunlight is the hadal zone. This zone extends from depths of 19,685 to 36,100 feet (6,000 to 11,000 meters) and is found in deep ocean trenches. Organisms living in this zone must adapt to extreme conditions, such as lack of sunlight and high pressure.
It means that one or more of the gauges is out of the safe zone. It could be oil pressure low, voltage high or low, or an engine overheat.It means that one or more of the gauges is out of the safe zone. It could be oil pressure low, voltage high or low, or an engine overheat.
The zone is called a front. There are a few types of fronts. They are: cold front, warm front, occluded front & stationary front.
No, the Intertropical Convergence Zone (ITCZ) is a region near the equator where the trade winds converge, creating low pressure. As warm, moist air rises in this zone, it can lead to the formation of thunderstorms and heavy rainfall.
The convection cells radiate heat.
The boundary layer of air next to the skin gets dragged around with the spinning ball, on one side its away from the direction of motion creating low pressure zone, on the other side its against the direction of motion, building a high pressure zone, the pressure difference pushes the ball from the high pressure to the low pressure zone.
The bands of high pressure are called subtropical high-pressure belts, while the bands of low pressure are known as the intertropical convergence zone (ITCZ) or the equatorial low-pressure belt. These belts play a significant role in global atmospheric circulation.
Wind moves from high pressure to low pressure. Air always moves from areas of high pressure to areas of low pressure in an attempt to equalize pressure differences.
Low pressure is a counter-clockwise spin (in the northern hemisphere) of rising air. Rising air causes precipitation and therefore you typically find rain with low pressure systems. High pressure systems have sinking air which tends to prevent rain in most cases.