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Warming of higher levels of the atmosphere leads to increased atmospheric water vapour, which in turn absorbs some of the sun's energy before it reaches the surface.
If so, that's probably because it's quite dry in the lower levels of the atmosphere.
Evaporation is rapid in dry air but much slower when the lowest levels of the atmosphere are close to saturation.
The chamber was designed to simulate some physical conditions in high levels of the atmosphere, particularly pressure, temperature and humidity.
In the middle and upper levels of the atmosphere, a pronounced dip in the jet stream, called a trough, overspread vigorous winds that changed direction with altitude.
In reality, as lead author Steve Sherwood explains in the video below, scientists observe water vapor being pulled away from those higher cloud-forming levels of the atmosphere.
Frozen precipitation, falling to levels of the atmosphere that are much warmer than 0 °C, often melts and reaches the ground as rain.
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When it occurs, very fast winds from the mid-levels of the atmosphere can descend to ground-level.
A look at the upper-levels of the atmosphere over the past week shows a weather pattern on pause.
After attaining hurricane status, Audrey began to slowly move northward in response troughing in the upper-levels of the atmosphere.
Initially fairly disorganized with little deep convection, dry air in the mid- to-upper-levels of the atmosphere prevented immediate intensification.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com