On a map of average annual temperature why are the lower latitudes so much warmer than the higher latitudes?
Hurricanes form in warm tropical waters and the conditions aren't right in higher northern latitudes because the temperature of the water is cold.
Elevation and latitude both affect temperature because they can impact the amount of sunlight received. Higher elevations generally have cooler temperatures due to decreased air pressure and thinner atmosphere. Areas at higher latitudes receive less direct sunlight, leading to cooler temperatures compared to lower latitudes.
The excess heat in tropical latitudes is transported to middle and high latitudes through a process called atmospheric circulation. This circulation is driven by temperature differences between the equator and the poles, leading to the movement of warm air toward higher latitudes and the transfer of heat energy across the globe.
The average kinetic energy of the atoms and molecules in a substance is directly proportional to its temperature. It is a measure of the average motion of particles within the substance. The higher the temperature, the higher the average kinetic energy.
The average temperature in the Olympic Rainforest is around 50-60°F (10-15°C) with cooler temperatures at higher elevations. The area receives an average annual rainfall of 140-170 inches (350-430 cm), making it one of the wettest areas in the United States.
The average temperature decreases as the distance from the equator increases because sunlight is spread out over a larger area at higher latitudes, resulting in less concentrated heat. Additionally, the angle at which sunlight strikes the Earth's surface becomes more oblique at higher latitudes, leading to less heating.
The largest annual temperature ranges occur towards higher latitudes in the interior of continents because these areas are more distant from the moderating effects of large bodies of water. Water has a high specific heat capacity, which means it can absorb and release heat more slowly than land. As a result, areas closer to oceans experience less extreme temperature fluctuations compared to inland regions.
Hurricanes form in warm tropical waters and the conditions aren't right in higher northern latitudes because the temperature of the water is cold.
A graph that shows the general trend between differences in elevation above sea level and the average annual temperature within the troposphere would depict a decrease in temperature with increasing elevation. As you go higher in the troposphere, the temperature generally decreases due to the lapse rate, which results in cooler temperatures at higher elevations.
The latitude that experiences the largest change in day length throughout the year (typically higher latitudes) would exhibit the greatest decrease in average daily insolation on a graph. This is due to the larger variation in the number of daylight hours between seasons at higher latitudes compared to lower latitudes.
Temperature refers to the average kinetic energy of a suubstance. The higher the average kinetic energy, the higher the temperature.
Elevation and latitude both affect temperature because they can impact the amount of sunlight received. Higher elevations generally have cooler temperatures due to decreased air pressure and thinner atmosphere. Areas at higher latitudes receive less direct sunlight, leading to cooler temperatures compared to lower latitudes.
The temperature differences between low and high latitudes are primarily due to variations in the angle of sunlight. At low latitudes, near the equator, sunlight is more direct and concentrated, leading to higher temperatures. In contrast, at high latitudes, sunlight is more spread out and less intense, resulting in cooler temperatures.
Seattle
Density variations of seawater with latitude are very similar to those for temperature variations with latitude. Because of the influence of temperature on seawater density, low latitudes exhibit lower densities at the surface that rapidly increase with depth. Higher latitudes exhibit little or no difference in density owing to the lack of a thermocline. Such a rapid change in density with depth is called a pycnocline, and like a thermocline is absent at higher latitudes.
It could be that Mumbai is nearer to the equator.
The excess heat in tropical latitudes is transported to middle and high latitudes through a process called atmospheric circulation. This circulation is driven by temperature differences between the equator and the poles, leading to the movement of warm air toward higher latitudes and the transfer of heat energy across the globe.