Trickle-Down and Trickle-Up Boundary Conditions in Eolian Dune-Field Pattern Formation

Author(s):  
Gary Kocurek ◽  
Ryan C. Ewing
Geomorphology ◽  
2010 ◽  
Vol 114 (3) ◽  
pp. 175-187 ◽  
Author(s):  
R.C. Ewing ◽  
G. Kocurek

Author(s):  
Michael D. Stubna ◽  
Richard H. Rand

Abstract We investigate the dynamics of the parametrically-excited P.D.E.(1)∂2u∂t2-c2(∂2u∂x2+∂2u∂y2)+εβ∂u∂t+(∂+εγcos⁡t)u=εαu3 with Neumann boundary conditions on a rectangular region:∂u∂x=0forx=0,π and ∂u∂y=0fory=0,πμ where 0 < μ ≤ 1. Our approach involves expanding u(x, y, t) in a 3-term Fourier series truncation:(2)u=f0(t)+f1(t)cos⁡x+f2(t)cos⁡μy By substituting (2) into (1) we obtain a system of 3 coupled nonlinear Mathieu equations which we analyze using averaging in the neighborhood of 2 : 1 resonance. By varying the parameters c and δ we obtain bifurcation curves which divide the cδ-plane into more than forty regions, each containing a distinct slow flow. Individual regions are found to differ from one another with respect to such features as the number and character of slow flow equilibria, and the presence or absence of a limit cycle. When interpreted in the original variable u, these regions account for a variety of patterns which may be classified as stationary, traveling or rotating. This type of behavior is comparable to various experimental observations made by other investigators on vertically driven fluids or sand.


Sedimentology ◽  
2011 ◽  
Vol 58 (6) ◽  
pp. 1391-1406 ◽  
Author(s):  
ERIN EASTWOOD ◽  
JOANNA NIELD ◽  
ANDREAS BAAS ◽  
GARY KOCUREK
Keyword(s):  

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