manus_continuum_granular1

commit 6e2b194b7883bda23cc821870911dedd1d82d3a0
parent 467972b534028b29ca6e500a7b8bdc66621fe2df
Author: Anders Damsgaard <anders@adamsgaard.dk>
Date:   Tue,  3 Dec 2019 16:24:24 +0100

Update reference

Diffstat:
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continuum-granular-manuscript1.tex
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2
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1 file changed, 1 insertion(+), 1 deletion(-)
diff --git a/continuum-granular-manuscript1.tex b/continuum-granular-manuscript1.tex
@@ -317,7 +317,7 @@ With all other physical conditions being equal, our results indicate that shear-
 Topography of non-planar ice-bed interfaces (proto-drumlins, ribbed moraines, etc.) may be transported and modulated through this spatially variable transport capacity, unless stress differences are overprinted by variations in water pressure \cite<e.g.,>[] {Sergienko2013, McCracken2016, Iverson2017b, Hermanowski2019b}.
 
 At depth, the water pressure variations display exponential decay in amplitude and increasing lag.
-As long as fluid and diffusion properties are constant and the layer is sufficiently thick, an analytical solution to skin depth $d_\mathrm{s}$ [m] in our system follows the form (after Eq.~4.90 in \citeA{Turcotte2002}),
+As long as fluid and diffusion properties are constant and the layer is sufficiently thick, an analytical solution to skin depth $d_\mathrm{s}$ [m] in our system follows the form \cite<e.g.,>[] {Turcotte2002},
 \begin{linenomath*}
 \begin{equation}
 	d_\mathrm{s}