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In the lower troposphere, such clouds are called stratus.
Figure 4-19 illustrates how solar heating generates an unstable mixed layer in the lower troposphere.
Analysis of satellite measurements of the lower troposphere also had 2014 in the top ten warmest years.
The lower troposphere was divided into two stratified air layers with contrasted BC vertical distributions.
Upwelling creates areas of cold coastal surface waters that stabilize the lower troposphere and reduce the chances for convection.
The lower troposphere over these warmer oceanic areas tends to be a region of relative low pressure.
The values attained during this event exceeded the 99th percentile values for the midwinter period throughout the lower troposphere.
A more plausible explanation for the discrepancy between a cooling lower troposphere and a warming surface is incomplete knowledge.
Can these "downdraft" motions lead to rapid vertical transport of air from the upper to the lower troposphere?
Possible mechanisms of solar influence on the lower troposphere are discussed.
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This alters the calculation needed to derive the lower-troposphere temperature.
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