based on the latitude you estimated, predict how much energy is transferred from the sun to the surface and then the air in your city
The amount of energy transferred from the sun to the surface and the air in a city is influenced by a variety of factors including the time of year, weather conditions, and atmospheric composition. However, based on a general estimation of latitude, we can assume that cities closer to the equator receive more direct sunlight and therefore more energy transfer compared to cities further away from the equator.
In general, cities located closer to the equator receive more intense sunlight and therefore experience higher levels of energy transfer from the sun to the surface and the air. This leads to higher temperatures and more energy available for various processes such as evaporation, convection, and wind formation.
On the other hand, cities located further away from the equator receive less intense sunlight and therefore experience lower levels of energy transfer from the sun. This results in lower temperatures and less energy available for atmospheric processes.
Overall, the estimated latitude of a city can provide a general indication of the amount of energy transferred from the sun to the surface and the air, but it is important to consider other factors as well in order to accurately predict energy transfer levels.