The places near the equator are warmer than the places which are far away from it. This is because the rays of the sun fall vertical on the equator and slanting in the temperate and polar regions. The vertical rays are concentrated over a small area than the slanting one. Because the angle of radiation varies depending on the latitude, surface temperatures on average are warmer at lower latitudes and cooler at higher latitudes (even though higher latitudes have more hours of daylight during the summer months). The distance from the equator affects the climate of a place. At the poles, energy from the sun reaches the Earth's surface at lower angles and passes through a thicker layer of atmosphere than at the equator. This means the climate is cooler further from the Equator. Tropic of cancer is the most important latitude of India i.e. 23.30 ′N. As it divides the Earth into 2 equal parts. The second important latitude is the standard meridian of India i.e. 82 30′E passing through Mirzapur. As it covers the difference of 2 hours and gives India a standard time.
Latitude affects climate primarily because of differences in the amount and angle of solar radiation received by different parts of the Earth's surface. At the equator, the sun's rays hit the Earth's surface more directly, causing more intense heating and warmer temperatures. As you move away from the equator towards the poles, the angle at which the sun's rays hit the Earth's surface becomes more oblique, causing less intense heating and cooler temperatures.
At low latitudes, which are close to the equator, the climate is generally hot and humid, with high temperatures and high levels of precipitation. This is because the intense heating causes warm air to rise, creating low pressure and drawing in moisture from the surrounding areas. These conditions are ideal for the growth of lush tropical rainforests and other vegetation.
At high latitudes, which are closer to the poles, the climate is generally cold and dry, with low temperatures and low levels of precipitation. This is because the oblique angle of the sun's rays causes less intense heating, which results in less moisture and less plant growth. In addition, the cold temperatures at high latitudes cause water to freeze, creating ice caps and glaciers that reflect sunlight back into space, further reducing the amount of solar radiation absorbed by the Earth's surface.
Overall, the differences in climate between low and high latitudes are primarily due to differences in solar radiation and temperature, which in turn affect the amount of precipitation, vegetation growth, and other climatic factors.
Many factors influence the climate of a region. The most important factor is latitude because different latitudes receive different amounts of solar radiation. The maximum annual temperature of the Earth, showing a roughly gradual temperature gradient from the low to the high latitudes. Because the angle of radiation varies depending on the latitude, surface temperatures on average are warmer at lower latitudes and cooler at higher latitudes (even though higher latitudes have more hours of daylight during the summer months). The distance from the equator affects the climate of a place. Low latitudes are those locations found between the Equator (0 degrees N/S) and 30 degrees N/S. The middle latitudes are found between 30 degrees N/S and 60 degrees N/S. And the high latitudes are found between 60 degrees N/S and the poles (90 degrees N/S). There is a relationship between latitude and temperature around the world, as temperatures are typically warmer approaching the Equator and cooler approaching the Poles. There are variations, though, as other factors such as elevation, ocean currents, and precipitation affect climate patterns. In the lower latitudes, such as the tropics, temperatures are the highest. This is because the sun's rays travel a shorter distance to the Equator (hitting the earth at less of an angle) and are therefore more concentrated, resulting in higher temperatures. High-altitude locations are usually much colder than areas closer to sea level. This is due to the low air pressure. Air expands as it rises, and the fewer gas molecules including nitrogen, oxygen, and carbon dioxide have fewer chances to bump into each other.There is a relationship between latitude and temperature around the world, as temperatures are typically warmer approaching the Equator and cooler approaching the Poles. There are variations, though, as other factors such as elevation, ocean currents, and precipitation affect climate patterns.