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âCoupledâ Subduction Model Oceanic Corner ï¬ïïu ï« ïp ï½ 0 ï¯ï ï u ï½ 0 ï¯ï¯ ïu ï½ 0 ï¯ï³ ï n ï½ 0 ï¯ ï¯ï®ï³ ï n ï½ p ext ï n with ï ï ° in ï in ï on ï1 on ï 2 on ï 3 uï½b uï½b ï³ ïn ï½ 0 2 p ext ï½ pressure at boundary computed from the oceanic corner With this natural boundary condition the weak form becomes (ïv,ïu)ï ï (divv, p)ï ï (q, divu)ï ï½ (v, f )ï ï« (v, p ext ï n)ï 3 . Arc Corner uï½0 ï³ ïn ï½ 0 ï³ ï n ï½ p ext ï n ï³ ïn ï½ 0
