The Cold Pool Below the Orchard

Written by Studio AM.

On a clear, calm night, a hollow at the foot of a slope may frost while trees higher up remain untouched. The difference can appear backward, since air is often colder at greater height. That broad rule describes much of the atmosphere, but the last few meters above the ground can behave differently.

After sunset, the land releases heat toward the open sky. The ground cools, then chills the thin layer of air touching it. Cooler air is usually denser than warmer air nearby, so gravity draws it downslope like a slow, shallow flow. When that air reaches a basin or meets a hedge, it can collect in a cold pool. Plants inside the pool may reach the frost point even when a thermometer on the upper slope stays above it.

Clouds and wind can interrupt the pattern. Clouds reduce the ground's heat loss, while a steady breeze mixes the cold layer with warmer air above. Soil moisture, plant cover, and the exact shape of the land also affect the result. Growers learned to notice these frost pockets through repeated observation, sometimes placing sensitive blossoms higher on a slope. A white patch below green leaves is not random; it can be a map of how air moved during the night.

Questions

Choose an answer. The explanation appears after you answer.

  1. Question 1 of 4

    What is the main idea of this passage?

  2. Question 2 of 4

    Which night would most likely weaken a cold pool in the hollow?

  3. Question 3 of 4

    What is a "basin" in the explanation of cold air?

  4. Question 4 of 4

    What first cools the thin layer of air near the ground?

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