Latitude and Longitude

The controls of weather and climate include latitude, distribution of land and water, general circulation of the atmosphere, general circulation of the oceans, altitude, topographic barriers and storms.
Latitude is one of the main controls of weather and climate because it helps one figure out the amount of circulation going on in the atmosphere. It helps determine the time and day in its weather form such as sunlight is barley shown to be up not very excessively high in the sky when the months of june to september arrive because of how much radiation is in the atmosphere and earth’s surface. The way latitude controls the climate is by when the latitude is increased the climate weather starts to decrease meaning if one is next to the equator it is most likely going to be piping hot and excruciating but the further apart you are from it, it gets colder. Depending on how much heat there is in the atmosphere, the latitude will manage how the conditions in degrees should be.
Distribution of land and water are related to the climate because an area or releam can increase in temperature rapidly no matter what the condition may be. Between land and water, the energy of the heat source going out depends on its sensation point. Energy is both used in land and water to help the with the distribution for the climate. Temperatures near the water/ocean is usually lower than land. It tends to be colder than what the climate on land is. Since waters vitality comes from sunlight, it makes the surface more adaptable and it helps circulate on land. Patterns from how land and water operate with energy show an increase and decrease in its weather conditions. Depending on the size of the land it can support the different weather climates going on in the atmosphere.

General circulation of the atmosphere is used to help bring energy into the earth’s surface and atmosphere. The heat mixed in with chilly weather starts to reduce the condensation of the force between the energy and temperature of both conditions. When the atmosphere has high forceful pushes, it reduces the temperature near the equator. The south and north differentiate on how the climate and weather of the atmosphere will be.
The positions of the latitude and longitude is what controls what the temperature and energy using of the atmosphere can possibly become. Air in the atmosphere goes through an increase or decrease depending on the weather condition to help populate how much energy is being used. Near the poles, energy is used to help create winds and a high altitudes to get the atmospheric pressure decreased. Samples are taken of the air force in the atmosphere and earth’s surface to help determine the latitude of the consistency of how much energy is being used up near the poles.

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