Weather Prediction By Numerical Process
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1913, S. 55, said to be an important paper: I regret that I have not seen it; A. Friedmann, Met. Zeit. 1914 March; Hergesell (Lindenberg, xm Bd. ) reviewed in Met. Zeit. 1920 Aug.
t Compare E. Gold's analysis of surface observations, Q. J. R. Met. Soc. 1913 October.
OH. 6/5/2, 6/6 RADIATION IN THE STRATOSPHERE 135 Whence we conclude that " if a thin horizontal layer in the stratosphere has its temperature slightly raised above that which would be in equilibrium with its surround- ings, the dist...urbance will be decreased to e' 1 of itself, by radiation, in 8'3 days. " (1) Now seeing that cyclones often sweep past a given place in a time short in com- parison with 8 '3 days, it is difficult to see how the uniformity of temperature with height in the stratosphere can be maintained by radiation alone.
One is led to the conclusion that the distribution of velocities must be such, that the adiabatic changes of temperature are the same at all levels.
This conclusion might be avoided if the stratosphere contained a larger proportion than the lower layers of some constituent which absorbs long wave radiation ; for in calculating the absorptivity in Ch.
What to read after Weather Prediction By Numerical Process?
You can find similar books in the "Read Also" column, or choose other free books by Lewis Fry Richardson to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
1913, S. 55, said to be an important paper: I regret that I have not seen it; A. Friedmann, Met. Zeit. 1914 March; Hergesell (Lindenberg, xm Bd. ) reviewed in Met. Zeit. 1920 Aug.
t Compare E. Gold's analysis of surface observations, Q. J. R. Met. Soc. 1913 October.
OH. 6/5/2, 6/6 RADIATION IN THE STRATOSPHERE 135 Whence we conclude that " if a thin horizontal layer in the stratosphere has its temperature slightly raised above that which would be in equilibrium with its surround- ings, the dist...urbance will be decreased to e' 1 of itself, by radiation, in 8'3 days. " (1) Now seeing that cyclones often sweep past a given place in a time short in com- parison with 8 '3 days, it is difficult to see how the uniformity of temperature with height in the stratosphere can be maintained by radiation alone.
One is led to the conclusion that the distribution of velocities must be such, that the adiabatic changes of temperature are the same at all levels.
This conclusion might be avoided if the stratosphere contained a larger proportion than the lower layers of some constituent which absorbs long wave radiation ; for in calculating the absorptivity in Ch.
What to read after Weather Prediction By Numerical Process?
You can find similar books in the "Read Also" column, or choose other free books by Lewis Fry Richardson to read onlineMoreLess
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