Thin Layers of Low TI Material

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(Created page with "=Description= Running KRC cases with layering (see Material Properties and Regolith Layering for more information on layering), scenarios can be encountered where thin la...")
 
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=Description=
 
=Description=
  
Running KRC cases with layering (see [[Material Properties and Regolith Layering]] for more information on layering), scenarios can be encountered where thin layers are desired. When sufficiently thin layers are encountered, the timestep requirement can raise beyond 1 step per second and KRC will not run. In order to bypass this  
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Running KRC cases with layering (see [[Material Properties and Regolith Layering]] for more information on layering), scenarios can be encountered where thin layers are desired. When sufficiently thin layers are encountered, the time step requirement can be very small and KRC will fail to run. In order to bypass this, we can enforce a smaller time step using the 'N2' field.
  
 
The below examples are relevant to the case found in the '''thin.pdf''' (page 10) within directory /doc.
 
The below examples are relevant to the case found in the '''thin.pdf''' (page 10) within directory /doc.
  
 
=Examples=
 
=Examples=
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For the following examples, we consider a case where a lower-TI "dust-like" layer (50 J m^-2 K^-1 s^-1/2) overlies a higher-TI layer (250 J m^-2 K^-1 s^-1/2).
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  krc(lat=0.,lon=0.,INERTIA=50.,INERTIA2=250.,thick=32.E-6,LKofT="T",ALBEDO=0.2,N2=393216)
 
  krc(lat=0.,lon=0.,INERTIA=50.,INERTIA2=250.,thick=32.E-6,LKofT="T",ALBEDO=0.2,N2=393216)

Revision as of 18:17, 11 January 2021

Description

Running KRC cases with layering (see Material Properties and Regolith Layering for more information on layering), scenarios can be encountered where thin layers are desired. When sufficiently thin layers are encountered, the time step requirement can be very small and KRC will fail to run. In order to bypass this, we can enforce a smaller time step using the 'N2' field.

The below examples are relevant to the case found in the thin.pdf (page 10) within directory /doc.

Examples

For the following examples, we consider a case where a lower-TI "dust-like" layer (50 J m^-2 K^-1 s^-1/2) overlies a higher-TI layer (250 J m^-2 K^-1 s^-1/2).


krc(lat=0.,lon=0.,INERTIA=50.,INERTIA2=250.,thick=32.E-6,LKofT="T",ALBEDO=0.2,N2=393216)
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