It is the time delay between a maximum or minimum insolation and maximum or minimum air temperature
Temperature lag is when the month/time of day when insolation is longest does not match up with when surface temperature is greatest. This is because it takes a while for the sunlight to pass through Earth's atmosphere.
The duration of insolation on March 21 is 12 hours daylight. The duration of insolation is dependent on temperature, season and latitude.
increases
The angle of insolation into a surface is largest when the surface directly faces the Sun. That coincides with the temperature rising. So the angle of insolation goes up as the temperature goes up.
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Temperature lag is when the month/time of day when insolation is longest does not match up with when surface temperature is greatest. This is because it takes a while for the sunlight to pass through Earth's atmosphere.
increases
The duration of insolation on March 21 is 12 hours daylight. The duration of insolation is dependent on temperature, season and latitude.
The angle of insolation into a surface is largest when the surface directly faces the Sun. That coincides with the temperature rising. So the angle of insolation goes up as the temperature goes up.
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Since they are at the same latitude it is most likely that something else is making the temperature different than the intensity of insolation affecting the temperature in both areas.
Direct and diffused insolation.
temperature swing
Insolation is a measurement of the solar radiation received by a surface over a unit time. Polar regions have the lowest insolation.
System overshoot is the room temperature that is way over the set room temperature from residual heat from the exchanger into the room after it has shut off. System lag is when the temperature drops below the set point on the thermostat.
The climate of Latin America is influenced by a variety of factors, including its proximity to the equator, ocean currents, elevation, and the presence of mountain ranges that affect precipitation patterns. The region's diverse topography also plays a role in shaping different climate zones, from tropical rainforests to deserts. Human activities, such as deforestation and urbanization, can also impact the climate through changes in land use and greenhouse gas emissions.
Insolation