Factors that determine climate are:ALatitude and elevationBLongitude and seasonsCProximity to water or mountainsDBoth 1 and 3
Question
Factors that determine climate are:ALatitude and elevationBLongitude and seasonsCProximity to water or mountainsDBoth 1 and 3
Solution 1
The factors that determine climate are both 1 and 3. This means that climate is determined by latitude and elevation, as well as proximity to water or mountains.
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Latitude and Elevation: The closer a place is to the equator (0° latitude), the warmer its climate is. This is because the sun's rays are most direct at the equator. As for elevation, the higher a place is above sea level, the cooler its climate is. This is due to the fact that as altitude increases, the air becomes thinner and less able to absorb and retain heat.
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Proximity to Water or Mountains: Large bodies of water like oceans and large lakes can affect the climate of an area. Water heats up and cools down more slowly than land, so coastal regions tend to have more moderate temperatures than inland areas. Mountains can also affect climate. As air rises over a mountain, it cools and precipitation occurs on the windward side. The leeward side of the mountain is often much drier.
Solution 2
The factors that determine climate are both 1 and 3. This means that climate is determined by latitude and elevation, as well as proximity to water or mountains.
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Latitude and Elevation: The closer a place is to the equator (0° latitude), the warmer its climate is. This is because the sun's rays are most direct at the equator. As for elevation, the higher a place is above sea level, the cooler its climate is. This is due to the fact that as altitude increases, the air becomes thinner and less able to absorb and retain heat.
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Proximity to Water or Mountains: Large bodies of water like oceans and large lakes can affect the climate of an area. Water heats up and cools down more slowly than land, so coastal regions tend to have more moderate temperatures than inland areas. Mountains can also affect climate. As air rises over a mountain, it cools and precipitation occurs on the windward side. The leeward side of the mountain is often much drier.
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