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cEstimate the convective overshooting as the level
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c where the [aafac * cloud work function] becomes zero,
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c which is the final cloud top
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c which is the final cloud top.
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c
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!> - Continue calculating the cloud work function past the point of neutral buoyancy to represent overshooting according to Han and Pan (2011) \cite han_and_pan_2011 . Convective overshooting stops when \f$ cA_u < 0\f$ where \f$c\f$ is currently 10%, or when 10% of the updraft cloud work function has been consumed by the stable buoyancy force.
Copy file name to clipboardExpand all lines: physics/CONV/SAS/sascnvn.F
+3-3Lines changed: 3 additions & 3 deletions
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@@ -974,9 +974,9 @@ subroutine sascnvn_run(
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if(totflg) return
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!!
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!
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! estimate the onvective overshooting as the level
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! Estimate the convective overshooting as the level
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! where the [aafac * cloud work function] becomes zero,
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! which is the final cloud top
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! which is the final cloud top.
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!
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!> - Continue calculating the cloud work function past the point of neutral buoyancy to represent overshooting according to Han and Pan (2011) \cite han_and_pan_2011 . Convective overshooting stops when \f$ cA_u < 0\f$ where \f$c\f$ is currently 10%, or when 10% of the updraft cloud work function has been consumed by the stable buoyancy force.
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do i = 1, im
@@ -1001,7 +1001,7 @@ subroutine sascnvn_run(
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& dz1 * (g / (cp * to(i,k)))
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& * dbyo(i,k) / (1. + gamma)
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& * rfact
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!NRL MNM: Limit overshooting not to be deeper than the actual cloud
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!NRL MNM: Limit overshooting not to be deeper than half the actual cloud
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