Those who keep a particularly vigilant eye on the weather might have noticed that on certain mornings, in all seasons, the lowest temperature is often recorded just after sunrise.
One of us had a morning paper route as a boy and was puzzled for years about this seemingly counterintuitive phenomenon. How could the temperature continue to fall for the few minutes after sunrise on a cold winter morning?
The answer lies in the fact that Earth and the sun radiate different kinds of energy and one needs to consider the budget of this energy to make sense of this recurring observation. But first a bit about measuring temperature. Atmospheric temperature is measured using thermometers placed in shaded enclosures at a height of about 5 to 6 feet above the ground.
On a clear, calm winter night, Earth’s surface radiates infrared energy upward towards space. With the sun already down, there is no shortwave solar radiation (and only a very little infrared energy from the overlying atmosphere) directed downward toward the surface. Consequently, with each passing second, the surface emits more energy than it receives and the surface temperature drops.
This continues all through the night with the accumulated loss of infrared energy from the surface accounting for the continued decrease in the surface temperature. When the sun finally rises above the horizon and spreads the first faint rays of solar energy across the surface, there is finally some incoming radiation. However, for several minutes the meager amount of incoming radiation is not sufficient to counter the amount of infrared energy still being emitted from the surface. As a result, the surface temperature continues to drop even in the face of the newly risen sun.
Steve Ackerman and Jonathan Martin, professors in the UW-Madison department of atmospheric and oceanic sciences, are guests on WHA radio (970 AM) at noon the last Monday of each month. send them your questions at stevea@ssec.wisc.edu or jemarti1@wisc. edu.





