They indicate that atmospheric instability is occurring on the higher altitudes of the troposphere.
2.
That requires the detection of the spectral signatures of atmospheric instability and high mass loss.
3.
By the time the thunderstorms started developing, J / kg, indicating moderate atmospheric instability.
4.
Castellanus clouds are evidence of mid-atmospheric instability and a high mid-altitude lapse rate.
5.
Cooling aloft, in conjunction with the approaching storm system, led to atmospheric instability, resulting in thunderstorms.
6.
Elevated sea surface temperatures, contrasting with cold atmospheric air, encourage atmospheric instability, especially within the troposphere.
7.
Atmospheric instability, hot temperatures, and a severe drought fueled the fire, making it difficult to suppress.
8.
Such storms are rarely severe and are a result of local atmospheric instability; hence the term " air mass thunderstorm ".
9.
These indices, as well as atmospheric instability itself, involve temperature changes through the troposphere with height, or lapse rate.
10.
Effects of atmospheric instability in moist atmospheres include thunderstorm development, which over warm oceans can lead to tropical cyclogenesis, and turbulence.
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