J. Gratton et C. Vigo, SELF-SIMILAR GRAVITY CURRENTS WITH VARIABLE INFLOW REVISITED - PLANE CURRENTS, Journal of Fluid Mechanics, 258, 1994, pp. 77-104
We use shallow-water theory to study the self-similar gravity currents
that describe the intrusion of a heavy fluid below a lighter ambient
fluid. We consider in detail the case of currents with planar symmetry
produced by a source with variable inflow, such that the volume of th
e intruding fluid varies in time according to a power law of the type
t(alpha). The resistance of the ambient fluid is taken into account by
a boundary condition of the von Karman type, that depends on a parame
ter beta that is a function of the density ratio of the fluids. The fl
ow is characterized by beta,alpha and the Froude number F-0 near the s
ource. We find four kinds of self-similar solutions: subcritical conti
nuous solutions (Type I), continuous solutions with a supercritical-su
bcritical transition (Type II), discontinuous solutions (Type III) tha
t have a hydraulic jump, and discontinuous solutions having hydraulic
jumps and a subcritical-supercritical transition (Type IV). The curren
t is always subcritical near the front, but near the source it is subc
ritical (F-0 < 1) for Type I currents, and supercritical (F-0 > 1) for
Types II, III, and IV. Type I solutions have already been found by ot
her authors, but Type II, III, and IV currents are novel. We find the
intervals of parameters for which these solutions exist, and discuss t
heir properties. For constant-volume currents one obtains Type I solut
ions for any beta that, when beta > 2, have a 'dry' region near the or
igin. For steady inflow one finds Type I currents for 0 < beta < infin
ity and Type II and III currents for any beta, if F-0 is sufficiently
large.