Air pressure decreases as you move from the troposphere to the stratosphere. This is because the weight of the air above is less in the stratosphere, leading to lower air pressure at higher altitudes.
The temperature increases with altitude in the troposphere because of the absorption of solar radiation by the Earth's surface, which heats up the air closer to the surface. As you move higher in the troposphere, the air becomes thinner and less able to retain this heat, causing a decrease in temperature.
Wind currents flow faster at the poles than at the equator. This is due to the Coriolis effect, which causes the winds to be deflected as they move from high pressure to low pressure areas, creating stronger winds at higher latitudes. Additionally, temperature differences between the equator and the poles contribute to the strength of wind currents.
This wind is usually caused by convection currents (which are created by intense heating of the ground), and is usually strong enough to move entire sand dunes. Air is unstable when heated, and this instability in the air will cause the mixture of higher winds in the troposphere with winds in the lower atmosphere, producing strong surface winds.
This wind is usually caused by convection currents (which are created by intense heating of the ground), and is usually strong enough to move entire sand dunes. Air is unstable when heated, and this instability in the air will cause the mixture of higher winds in the troposphere with winds in the lower atmosphere, producing strong surface winds.
This wind is usually caused by convection currents (which are created by intense heating of the ground), and is usually strong enough to move entire sand dunes. Air is unstable when heated, and this instability in the air will cause the mixture of higher winds in the troposphere with winds in the lower atmosphere, producing strong surface winds.
This wind is usually caused by convection currents and is usually strong enough to move entire sand dunes. Air is unstable when heated, and this instability in the air will cause the mixture of higher winds in the troposphere with winds in the lower atmosphere, producing strong surface winds.
Winds are generally stronger during the day due to the differential heating of the Earth's surface by the sun. This causes air masses to move and create wind patterns. At night, the lack of heating leads to calmer conditions and lighter winds.
The temperature generally decreases as you move higher up in the troposphere, which is the lowest layer of Earth's atmosphere. This decrease in temperature is known as the lapse rate and is due to the lower pressure at higher altitudes.
Air pressure decreases as you move from the troposphere to the stratosphere. This is because the weight of the air above is less in the stratosphere, leading to lower air pressure at higher altitudes.
because the west winds were stronger then the east winds.
The temperature increases with altitude in the troposphere because of the absorption of solar radiation by the Earth's surface, which heats up the air closer to the surface. As you move higher in the troposphere, the air becomes thinner and less able to retain this heat, causing a decrease in temperature.
Some clouds move faster than others because of differences in wind speed and direction at different altitudes in the atmosphere. Stronger winds can push clouds along more quickly, while lighter winds may cause clouds to move more slowly.
Wind currents flow faster at the poles than at the equator. This is due to the Coriolis effect, which causes the winds to be deflected as they move from high pressure to low pressure areas, creating stronger winds at higher latitudes. Additionally, temperature differences between the equator and the poles contribute to the strength of wind currents.
The stronger metallic bonds have more delocalized electrons, which can move freely throughout the structure. This leads to increased electron density, stronger attraction between metal ions, and higher melting/boiling points.
Winds tend to move from opposite the directions that seagulls fly. Because seagulls tend to fly from low pressure cells to areas with higher atmospheric pressure, the direction of the wind generally flows against the flow of seagulls.
Winds near the surface are stronger and gustier in the afternoon because of solar heating. As the day progresses, the sun heats the Earth's surface unevenly, creating temperature differences that lead to air pressure variations. This causes air to move from high-pressure areas to low-pressure areas, resulting in stronger winds.