by the sun
Surface winds are slowed by friction caused by topography as well as the built environment.
True
hot, humid air with little or no wind
- Oceans - Latitude - Altitude - Topography - Earths Winds
"Weather" designates atmospheric conditions in a given geographic area for a given period. Hence, weather cannot be said to move at al. The above answer is quie true. However, earth surface winds in the northern hempishere that create local weather do generally tend to move west to east, opposite of the Earths rotation.
A primary cause for surface winds on the earth is the Earths Rotation.
high winds are normally caused by the unequal heating of the earths surface.
Surface winds and upper air winds differ in their speed, direction, and altitude. Surface winds are influenced by friction with the Earth's surface and tend to be slower and more variable in direction. Upper air winds, on the other hand, are faster, more consistent in direction, and are influenced by factors such as temperature gradients and pressure systems. These differences in wind patterns impact weather by affecting the movement of air masses, the formation of weather systems, and the distribution of heat and moisture in the atmosphere.
seasons
This caused by the rotation of the earth and is called the coriolis effect.
The equator is a calm area on Earth's surface where warm air rises due to the intense solar radiation it receives. This warm air creates low pressure and leads to the formation of the Inter-Tropical Convergence Zone (ITCZ), a region of converging winds and often thunderstorms.
Coriolis effect
No, there would not be winds if the earth's surface was the same temperature everywhere. The reason why is because during the day the land heats up faster than the water.
The answer is jet stream, answered by a sixth grader
The Jet Stream.
Local winds are winds that are influenced by local geographical features such as mountains, valleys, or bodies of water. They are usually short-lived and can vary in speed and direction, depending on the specific local conditions. Examples of local winds include sea breezes, valley breezes, and mountain winds.
Local winds are winds that blow over short distances caused by unequal heating of the earths surface in a small area.