Custom Query (964 matches)
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Ticket | Owner | Reporter | Resolution | Summary |
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#930 | Done | Minor Miscelaneous Update | ||
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#931 | Fixed | VERY IMPORTANT: corrected bug in ATM_PRESS term for shallow-water applications | ||
Description |
There is a sign error when adding the ATM_PRESS term in step2d for shallow-water applications (SOLVE3D off). So we need to have the following code instead: #if defined ATM_PRESS && !defined SOLVE3D rhs_ubar(i,j)=rhs_ubar(i,j)- & & fac3*on_u(i,j)* & & (h(i-1,j)+h(i,j)+ & & gzeta(i-1,j)+gzeta(i,j))* & & (Pair(i,j)-Pair(i-1,j)) #endif ... #if defined ATM_PRESS && !defined SOLVE3D rhs_vbar(i,j)=rhs_vbar(i,j)- & & fac3*om_v(i,j)* & & (h(i,j-1)+h(i,j)+ & & gzeta(i,j-1)+gzeta(i,j))* & & (Pair(i,j)-Pair(i,j-1)) #endif We need to use a minus sign for the contribution—many thanks to Shunpei Matsuo for reporting this bug. I noticed the sign issue when coding the adjacent term for the TIDE_GENERATING_FORCES option in step2d_LF_AM3.h for a similar shallow water configuration. I was supposed to set a test case for the air pressure forcing inverted barometer effect in the barotropic pressure gradient. But it was low on my long priority list. So, I forgot. Thus, Shunpei Matsuo's cyclone application is suitable for testing the ATM_PRESS this term. A cyclone rotates counterclockwise around a center of low atmospheric pressure in the northern hemisphere. Consequently, the inverted barometer effect causes the water level to rise to form a dome around the low-pressure center, as shown below: Notice that the opposite would happen over a cell of high air pressure causing the water level to drop. Above Figure is taken from the SWELLNET, which is used by surfers. |
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#932 | Fixed | IMPORTANT: Update arguments to intrisic function PACK | ||
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