The change in the density of a liquid undergoing a temperature change, e.g. alcohol or mercury, allows for the making of a liquid glass tube thermometer.
Other thermometers are based on the changing of electrical properties (resistance, current, and voltage) with temperature, sensing infrared radiation, and bending bimetallic strips.
The maximum temperature typically occurs around 4PM local time.
The minimum temperature typically occurs around sunrise.
At the maximum and minimum temperature times of the day, incoming solar and IR radiation and outgoing IR radiation at surface are nearly the same.
The outgoing IR surface radiation will reveal when the max and min temperatures are reached during a day. Maximumoutgoing surface IR corresponds to the maximumsurface temperature and the minimumoutgoing surface IR corresponds to the minimumsurface temperature
Surface air responds to changes in surface temperature through IR absorption, conduction (direct contact of air), convection (mixing of air), and latent heat (change of state of water vapor).
Conditions most favorable for nighttime cooling of surface air are dry air, clear skies, and calm winds
Radiational cooling of the ground with moist surface air can lead to condensational heating at the ground (dew forms) which lessens the cooling of the ground and surface air
Conditions most favorable for daytime warming of surface air are clear skies and a dry ground.
Material factors at the earth’s surface affecting surface temperature include heat capacity, water content (evaporation and heat capacity), transparency, and conduction from below (insulation)
A fresh snow covered surface (insulates the ground) is quite favorable for nighttime cooling of surface air.
Dry sand with air between the grains acts as an insulator from the ground underneath and will warm quickly with solar radiation.
The surface of the ground responds quickly in temperature when absorbing solar radiation while water responds slowly in temperature when absorbing solar radiation.
Radiation is absorbed by water within a thick layer and water has a high heat capacity
Radiation is absorbed by the ground in a very thin layer right at its surface
The daily temperature range is smaller over a water body than over land
The meteorological daily mean temperature is the average of the maximum and minimum temperature.
The daily temperature range is the difference between the maximum and minimum temperature
The mean monthly temperature is the average of the mean daily temperatures over a month
The annual temperature range is the difference between the mean month maximum and minimum temperatures over a year
The largest annual temperature ranges are typically found at high latitudes over continents
The least annual temperature ranges are typically found over oceans at low latitudes (tropics)
The wind chill temperature is a relative temperature to how one feels in the wind.
The largest daily temperature ranges during the summer are typically found over deserts.