与 «TEPHIGRAM»相关的英语书籍
在以下的参考文献中发现
tephigram的用法。与
tephigram相关的书籍以及同一来源的简短摘要提供其在 英语文献中的使用情境。
1
The Physics of Atmospheres
3.3 The tephigram The tephigram is a thermodynamic diagram particularly
suitable for representing atmospheric processes. The name derives from T-i/i-
gram since it is a temperature-entropy plot, the symbol 0 sometimes being used
for ...
John Theodore Houghton,
1977
2
An Introduction to Atmospheric Physics
One such diagram is the tephigram shown in Figure 2.10. This uses the
temperature T andentropy perunitmass S asorthogonalcoordinates.11 The lines
of constant S are labelled with the corresponding values of the potential
temperature θ ...
3
Atmospheric Thermodynamics
Tdlnp sin a (31) which coincides with £,e except for the constant proportionality
factor sin a. Within this approximation, we can therefore work with the tephigram
as if it were an ema- gram, and apply the same methods as described before.
Julio V. Iribarne, W.L. Godson,
1981
4
Physical and Dynamical Meteorology
The tephigram in effect takes account only of the density of the dry air, though it
takes account of the effect of the presence of water-vapour on the temperature
changes which are produced by the ascent of the moist air. Strictly speaking ...
5
The Physics of Atmospheres
... ignores the compensating motions, is in general a good approximation and is
used in general forecasting analysis. 3.3 The tephigram The tephigram is a
thermodynamic diagram particularly suitable for representing atmospheric
processes.
6
Fundamentals of Physics and Chemistry of the Atmosphere
This diagram is also known as a tephigram and it is very instructive because it
permits us to visualize concepts we will use often when dealing with
thermodynamic transformations in the presence of water vapor. The state of an
air mass can be ...
7
Principles of Meteorological Analysis
Although the chart has had little use in recent years, its principle is still a useful
one which we can incorporate in the tephigram. The Rossby diagram has
coordinates log 6d as ordinate and r as abscissa. Isopleths of 6E are also found
in the ...
8
Atmosphere, Weather and Climate
Experimentation with a tephigram shows that both the convective and the lifting
condensation levels rise as the surface temperature increases, with little change
of dew-point. This is commonly observed in the early afternoon, when the base of
...
Roger G. Barry, Richard J Chorley,
2009
Such an area lying above the tephigram is said to be a positive area, for it
represents positive energy available for the production of convective instability. If
the tephigram had followed a course above the saturation adiabat the area would
have ...
10
Bulletin of the National Research Council
Such an area lying above the tephigram is said to be a positive area, for it
represents positive energy available for the production of convective instability. If
the tephigram had followed a course above the saturation adiabat the area would
have ...