The lapse rate is the rate at which the temperature Tdecreases in the atmosphere with respect to ncreasing altitude z It is typically reported in units of °C/km and is defined by dT dz Vhen the lapse rate rises above 7°C/km in a certain layer of the atmosphere, it indicates favorable onditions for thunderstorm and tornado formation, provided other atmospheric conditions are also present. Suppose the temperature at z = 2.9km is T = 7.6°C and the temperature at z = 5.26km s T = -14.3°C. Assume also that the temperat ure function is continuous and differentiable at all ltitudes of interest. What can a meteorologist conclude from these data?

Functions and Change: A Modeling Approach to College Algebra (MindTap Course List)
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Author:Bruce Crauder, Benny Evans, Alan Noell
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Chapter1: Functions
Section1.2: Functions Given By Tables
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The lapse rate is the rate at which the temperature Tdecreases in the atmosphere with respect to
increasing altitude z It is typically reported in units of °C/km and is defined by
dT
dz
When the lapse rate rises above 7°C/km in a certain layer of the atmosphere, it indicates favorable
conditions for thunderstorm and tornado formation, provided other atmospheric conditions are also
present. Suppose the temperature at z = 2.9km is T = 7.6°C and the temperature at z = 5.26km
is T = –14.3°C. Assume also that the temperature function is continuous and differentiable at all
altitudes of interest. What can a meteorologist conclude from these data?
Transcribed Image Text:The lapse rate is the rate at which the temperature Tdecreases in the atmosphere with respect to increasing altitude z It is typically reported in units of °C/km and is defined by dT dz When the lapse rate rises above 7°C/km in a certain layer of the atmosphere, it indicates favorable conditions for thunderstorm and tornado formation, provided other atmospheric conditions are also present. Suppose the temperature at z = 2.9km is T = 7.6°C and the temperature at z = 5.26km is T = –14.3°C. Assume also that the temperature function is continuous and differentiable at all altitudes of interest. What can a meteorologist conclude from these data?
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