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Adaptivity with moving grids

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16 C. J. Budd, W. Huang and R. D. Russell<br />

then given by<br />

s = max |λ i|<br />

min |λ j | . (2.6)<br />

Other measures of mesh skewness are also referred to as shape or quality<br />

measures. Liu and Joe (1994) investigate several shape measures for<br />

tetrahedra and show that they are equivalent to each other. Denote the<br />

four vertices of a tetrahedron τP e by a 0,...,a 3 , and define the so-called edge<br />

matrix as E =[a 1 − a 0 ,a 2 − a 0 ,a 3 − a 0 ]. Let ê be a regular tetrahedron<br />

having the same volume as τP e . Denote the corresponding vertices and the<br />

edge matrix of ê by â 0 ,...,â 3 and Ê, respectively. Then one of the shape<br />

measures for τP e is defined by<br />

η(τP e )= 3[ det((EÊ−1 ) T (EÊ−1 )) ] 1 3<br />

trace((EÊ−1 ) T (EÊ−1 )) .<br />

Notice that the η(τP e )rangesfrom0to1,<strong>with</strong>η(τ P e ) = 1 for a regular<br />

tetrahedron and η(τP e ) = 0 for a flat tetrahedron. A geometric quality measure<br />

is introduced by Huang (2005a) for measuring the shape of a simplicial<br />

element in any dimension. Let τP e be a simplicial element in n dimensions<br />

and let ˆK be an n-simplex <strong>with</strong> unit edge length. There exists a unique<br />

invertible affine mapping<br />

F e : ˆK → τ e P ,<br />

τ e P = F e ( ˆK).<br />

Denote the Jacobian matrix of F e by F e. ′ Then the geometric measure is<br />

defined by<br />

Q geo (τP e )= trace((F e) ′ T F e)<br />

′ .<br />

d[det((F e) ′ T F e)] ′ 1 d<br />

Notice that Q geo (τP e ) ranges from 1 to ∞, <strong>with</strong>Q geo(τP e ) = 1 for a regular n-<br />

simplex and Q geo (τP e )=∞ for a flat d-simplex. Interestingly, for tetrahedra<br />

these two shape measures have the relation Q geo (τP e )=1/η(τ P e ). To see this,<br />

we first notice that ˆK and ê are similar. Thus, the mapping G e :ê → τP e is<br />

related to F e by<br />

G e = cF e , G ′ e = cF e<br />

′<br />

for some positive constant c. Then the edge matrices E and Ê are related by<br />

E = G ′ ′<br />

eÊ = cF eÊ.<br />

Using this relation we can rewrite η(τ e P )as<br />

η(τ e P )= 3[ det((F ′ e) T F ′ e) ] 1 3<br />

trace((F ′ e) T F ′ e)<br />

=<br />

1<br />

Q geo (τ e P ).

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