Observations and Modelling of Fronts and Frontogenesis
Observations and Modelling of Fronts and Frontogenesis
Observations and Modelling of Fronts and Frontogenesis
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solution exist in the neighborhood <strong>of</strong> such a point. In order<br />
to remove the singular solution, we impose the regularity<br />
condition,<br />
g(pf)(p3 - p2)[2h2v2 + h2v2 + (h1v1)I<br />
- (f u2y)v2 + (f - u3y)v3 = 0. (25)<br />
This may be derived either by power series solution <strong>of</strong> (16)<br />
or by inspection <strong>of</strong> (24), requiring that v2 be bounded at<br />
Y Y2-<br />
The three conditions (20), (23), <strong>and</strong> (25), applied at<br />
any juncture <strong>of</strong> two- <strong>and</strong> three-layer subdomains, close the<br />
problem for the equations (16), with the boundary conditions<br />
(17), when layer 2 vanishes in any portion <strong>of</strong> the domain.<br />
III .2 . c Nondimensionalization<br />
We nondimensionalize the equations by dimensional<br />
quantities related to the forcing. In this subsection,<br />
primes will denote nondimensional variables. Typical<br />
dimensional values will be given in brackets. The basic<br />
scales are the friction velocity u* [1 cm s] <strong>and</strong> the<br />
heating Q* [75 W m2], in terms <strong>of</strong> which the forcing may be<br />
written,<br />
= pou*2r' [0.1 N m2], Q = Q*Q'.<br />
The nondimensional variables <strong>and</strong> dimensional scales (with<br />
0.5 (Davis et al., l981a, l981b), P0 = l0 kg m3,<br />
g = 9.8 m 2, = i0 sfl-, specific heat <strong>of</strong> water at<br />
(26a)