[HTML][HTML] Equilibration of two-dimensional double-diffusive intrusions
J Simeonov, ME Stern - Journal of Physical Oceanography, 2007 - journals.ametsoc.org
J Simeonov, ME Stern
Journal of Physical Oceanography, 2007•journals.ametsoc.org… The ξ-independent intrusion signal appears as one fresh and one salty band of salt
fingers. The axes are labeled with the number of grid nodes. The strongest fingers appear in
the region of maximum shear where the vertical T–S gradients are also the largest. … (b)
The ratio of the rms intrusion velocity and temperature as a function of a. This ratio is
approximately 50% of the linear theory constant U 0 /T 0 = 0.85 (see discussion in text). …
The ξ-independent intrusion signal appears as one fresh and one salty band of salt fingers …
fingers. The axes are labeled with the number of grid nodes. The strongest fingers appear in
the region of maximum shear where the vertical T–S gradients are also the largest. … (b)
The ratio of the rms intrusion velocity and temperature as a function of a. This ratio is
approximately 50% of the linear theory constant U 0 /T 0 = 0.85 (see discussion in text). …
The ξ-independent intrusion signal appears as one fresh and one salty band of salt fingers …
Özgökmen, TM, OE Esenkov, and DB Olson, 1998: A numerical study of layer formation due to fingers in double-diffusive convection in a vertically-bounded domain. J. Mar. Res., 56, 463–487.
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