Publication Date:
2022-05-26
Description:
A. On the maintenance of the westerlies south of the polar front. B. Technique and examples of isentropic analysis. C. Isentropic analysis of a case of anticyclogenesis.
Description:
This paper constitutes Part I of a report on certain investigations which have been in
progress at the Massachusetts Institute of Technology during the past few years and
which have been supported in part with funds provided by the Weather Bureau of the
U. S. Department of Agriculture under the Bankhead-Jones Special Research Fund. The
ultimate purpose of these investigations is to develop a sound physical model of the general
circulation of the atmosphere, in the hope that an improved understanding of this
process eventually may furnish valuable clues as to how the time range of our present
daily weather forecasts may be extended and their quality be improved.
In the past, the interpretation of the large-scale circulations of the atmosphere with
the aid of the tools of classical hydrodynamics has suffered from the fact that these tools
were designed for the study of thermodynamically inactive fluids, in which, furthermore,
viscous or eddy stresses could be neglected. Through the work of V. Bjerknes and his
students a good start has now been made towards the development of a science of hydrodynamics
applicable also to thermodynamically active fluids, in which density changes
are taking place as a result of non-adiabatic temperature changes. The removal of the
second restriction-i.e., the development of hydrodynamic tools adapted to the study of
fluids in which eddy stresses playa dominant role-has been accomplished mainly
through the investigations of the Göttingen school of fluid mechanics.
As yet, no synthesis of these two modern developments has been accomplished, although
it is becoming increasingly clear that such a synthesis is needed before any headway
can be made with the interpretation of the behaviour of the atmosphere. There has
been a tendency on the part of meteorologists to assume that the effects of eddy stresses
are restricted to a layer near the ground, and that the atmosphere above this layer behaves
approximately as an ideal fluid. Even fairly elementary considerations show that
a real understanding of atmospheric circulations becomes absolutely impossible on the
basis of this assumption.
A modest first attempt towards such a synthesis of the Norwegian and German developments
will be attempted in these reports. It will be shown that the movements in
the free atmosphere above the ground friction layer are affected by large-scale lateral
mixing processes which produce shearing stresses acting across vertical planes, and one
or two examples will be given to demonstrate that reasonable steady state solutions for
the atmosphere can be obtained by taking this internal stress distribution into account.
It will be shown, moreover, that the distribution of cold sources and heat sources in
the free atmosphere is at least in part controlled by the stress distribution, which regúlates
the location of ascending and descending movements.
Keywords:
Atmospheric circulation
Repository Name:
Woods Hole Open Access Server
Type:
Book
Format:
8947371 bytes
Format:
application/pdf
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