09.04.2013 Views

Observations and Modelling of Fronts and Frontogenesis

Observations and Modelling of Fronts and Frontogenesis

Observations and Modelling of Fronts and Frontogenesis

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

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)

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!