Difference between revisions of "UKCA & UMUI Tutorial 8"

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==Adding Wet Deposition==
 
==Adding Wet Deposition==
   
The formulationn used in UKCA is described in Giannakopoulos (1999)[1]. This scheme uses the following formula to calculate the effective Henry's Law coefficient
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The formulation used in UKCA is described in Giannakopoulos (1999)[1]. This scheme uses the following formula to calculate the effective Henry's Law coefficient
   
 
<math>
 
<math>
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where <math>k\left(298\right)</math> is the rate constant at 298K.
 
where <math>k\left(298\right)</math> is the rate constant at 298K.
  +
  +
During this tutorial you will be tasked with adding the wet deposition of one of your new tracers.
   
 
'''References'''
 
'''References'''
# Giannakopoulos, C., M. P. Chipperfield, K. S. Law, and J. A. Pyle (1999), Validation and intercomparison of wet and dry deposition schemes using 210Pb in a global three-dimensional off-line chemical transport model, J. Geophys. Res., 104(D19), 23761–23784, doi:10.1029/1999JD900392.
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# Giannakopoulos, C., M. P. Chipperfield, K. S. Law, and J. A. Pyle (1999), Validation and intercomparison of wet and dry deposition schemes using 210Pb in a global three-dimensional off-line chemical transport model, J. Geophys. Res., 104(D19), 23761–23784, doi:10.1029/1999JD900392.
   
 
==Turning on Wet Deposition for a Species==
 
==Turning on Wet Deposition for a Species==
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{| border="1"
 
{| border="1"
| <math>\ k(298)\ </math> || <math>\ -{\Delta H}/R\ </math> || <math>\ k(298)</math> for the 1st dissociatation || <math>\ -{\Delta H}/R</math> for the 1st dissociatation || <math>\ k(298)</math> for the 2nd dissociatation || <math>\ -{\Delta H}/R</math> for the 2nd dissociatation
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| <math>\ k(298)\ </math> || <math>\ -\left({\Delta H}/R\right)\ </math> || <math>\ k(298)</math> for the 1st dissociation || <math>\ -\left({\Delta H}/R\right)</math> for the 1st dissociation || <math>\ k(298)</math> for the 2nd dissociation || <math>\ -\left({\Delta H}/R\right)</math> for the 2nd dissociation
 
|}
 
|}
   
Columns 3 and 4 are used if the species dissociates in the aqueous phase. In this case, <math>H_{eff}</math> is futher multiplied by a factor of
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Columns 3 and 4 are used if the species dissociates in the aqueous phase. In this case, <math>H_{eff}</math> is further multiplied by a factor of
   
 
<math>
 
<math>
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</math>
 
</math>
   
In this case, columns 3 and 4 contain the values of <math>k(298)</math> and <math>-{\Delta H}/R</math> used in the above formula. Similarly, if the dissasociates a second time then a further factor of <math>1+k(aq)/H^{+}</math>, where <math>k(aq)</math> is calculated from the values of <math>k(298)</math> and <math>-{\Delta H}/R</math> in columns 5 and 6.
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and column 3 contains the values of <math>k(298)</math> and column 4 contains the value of <math>-{\Delta H}/R</math>. Similarly, if the species dissociates a second time then a further factor of <math>1+k(aq)/H^{+}</math> is applied, where this value of <math>k(aq)</math> is calculated from the values of <math>k(298)</math> and <math>-{\Delta H}/R</math> in columns 5 and 6.
   
 
'''Note:''' As with the 2D dry deposition values in '''depvel_defs_<span style="color:blue">scheme</span>''', the order of '''henry_defs_<span style="color:blue">scheme</span>''' also assumes that the values are in the same order as the species (that wet deposit) in the '''chch_defs_<span style="color:blue">scheme</span>''' array.
 
'''Note:''' As with the 2D dry deposition values in '''depvel_defs_<span style="color:blue">scheme</span>''', the order of '''henry_defs_<span style="color:blue">scheme</span>''' also assumes that the values are in the same order as the species (that wet deposit) in the '''chch_defs_<span style="color:blue">scheme</span>''' array.
   
  +
Examples for this array are
! The following formula is used to calculate the effective Henry's Law coef,
 
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! which takes the affects of dissociation and complex formation on a species'
 
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0.2100E+06, 0.8700E+04, 0.2000E+02, 0.0000E+00, 0.0000E+00, 0.0000E+00,& ! 4 HONO2
! solubility (see Giannakopoulos, 1998)
 
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0.8300E+05, 0.7400E+04, 0.2400E-11,-0.3730E+04, 0.0000E+00, 0.0000E+00,& ! 5 H2O2
!
 
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! H(eff) = K(298)exp{[-deltaH/R]x[(1/T)-(1/298)]}
 
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===Increase the value of JPDW===
!
 
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! The data in columns 1 and 2 above give the data for this gas-aqueous transfer,
 
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Similar to when adding dry deposition of a species you will need to increase the size of the '''JPDW''' counter. This is done with a hand-edit, the value of '''JPDW''' being set in the '''CNTLATM''' file in your <tt>$HOME/umui_jobs/<span style="color:blue">jobid</span></tt> directory.
! Column 1 = K(298) [M/atm]
 
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! Column 2 = -deltaH/R [K-1]
 
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==Task 8.1: Add wet deposition of a species==
!
 
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! If the species dissociates in the aqueous phase the above term is multiplied by
 
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<span style="color:green">'''Task 8.1:''' Add in wet deposition for '''BOB''', using the following values:</span>
! another factor of 1+{K(aq)/[H+]}, where
 
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! K(aq) = K(298)exp{[-deltaH/R]x[(1/T)-(1/298)]}
 
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{| border="1"
! The data in columns 3 and 4 give the data for this aqueous-phase dissociation,
 
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! <math>\ k(298)\ </math> || <math>\ -\left({\Delta H}/R\right)\ </math> || <math>\ k(298)</math> for the 1st dissociation || <math>\ -\left({\Delta H}/R\right)</math> for the 1st dissociation || <math>\ k(298)</math> for the 2nd dissociation || <math>\ -\left({\Delta H}/R\right)</math> for the 2nd dissociation
! Column 3 = K(298) [M]
 
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|-
! Column 4 = -deltaH/R [K-1]
 
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| <math>\ 0.21 \times 10^{+06}\ </math> || <math>\ 0.87 \times 10^{+04}\ </math> || <math>\ 0.2 \times 10^{+02}\ </math> || <math>\ 0.0\ </math> || <math>\ 0.0\ </math> || <math>\ 0.0\ </math>
! The data in columns 5 and 6 give the data for a second dissociation,
 
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|}
! e.g for SO2, HSO3^{-}, and SO3^{2-}
 
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! Column 5 = K(298) [M]
 
  +
'''Note:''' If you were unable to successfully complete [[UKCA & UMUI Tutorial 7#Task 7.1: adding new dry deposition values|Task 7.1]], then please take a copy of the '''h''' job from the Tutorial experiment (''Tutorial: solution to Task 7.1 - add new dry deposition'') and work from there, as this will allow you to only make the changes required for this task.
! Column 6 = -deltaH/R [K-1]
 
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'''Remember:''' If you are using MONSooN you will need to delete/move any existing output files in your '''[[UKCA & UMUI Tutorials: Things to know before you start#Archiving|archive]]''' directory.
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[[Solution to UKCA & UMUI Tutorial 8 Task 8.1 | Solution]]
   
 
----
 
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Latest revision as of 16:37, 15 July 2013

Back to UKCA & UMUI Tutorials

Adding Wet Deposition

The formulation used in UKCA is described in Giannakopoulos (1999)[1]. This scheme uses the following formula to calculate the effective Henry's Law coefficient

where is the rate constant at 298K.

During this tutorial you will be tasked with adding the wet deposition of one of your new tracers.

References

  1. Giannakopoulos, C., M. P. Chipperfield, K. S. Law, and J. A. Pyle (1999), Validation and intercomparison of wet and dry deposition schemes using 210Pb in a global three-dimensional off-line chemical transport model, J. Geophys. Res., 104(D19), 23761–23784, doi:10.1029/1999JD900392.

Turning on Wet Deposition for a Species

Chemistry Scheme Specification

Within the UKCA code, whether a species is wet deposited or not is controlled in the ukca_chem_scheme.F90 file. In the chch_defs_scheme array there are lines like

chch_t( 10,'HONO2     ',  1,'TR        ','          ',  1,  1,  0),  & !  10 DD: 7,WD: 4,       
chch_t( 11,'H2O2      ',  1,'TR        ','          ',  1,  1,  0),  & !  11 DD: 8,WD: 5,  

Where the 1 in the 7th column turns on wet deposition of that species (being 0 otherwise). You will need to change the 0 to a 1 for the species that you wish to now wet deposit.

Setting Henry's Law values

In the ukca_chem_scheme.F90 the parameters required to calculate are held in the henry_defs_scheme array, and has format

for the 1st dissociation for the 1st dissociation for the 2nd dissociation for the 2nd dissociation

Columns 3 and 4 are used if the species dissociates in the aqueous phase. In this case, is further multiplied by a factor of

where

and column 3 contains the values of and column 4 contains the value of . Similarly, if the species dissociates a second time then a further factor of is applied, where this value of is calculated from the values of and in columns 5 and 6.

Note: As with the 2D dry deposition values in depvel_defs_scheme, the order of henry_defs_scheme also assumes that the values are in the same order as the species (that wet deposit) in the chch_defs_scheme array.

Examples for this array are

0.2100E+06, 0.8700E+04, 0.2000E+02, 0.0000E+00, 0.0000E+00, 0.0000E+00,&   !    4  HONO2
0.8300E+05, 0.7400E+04, 0.2400E-11,-0.3730E+04, 0.0000E+00, 0.0000E+00,&   !    5  H2O2

Increase the value of JPDW

Similar to when adding dry deposition of a species you will need to increase the size of the JPDW counter. This is done with a hand-edit, the value of JPDW being set in the CNTLATM file in your $HOME/umui_jobs/jobid directory.

Task 8.1: Add wet deposition of a species

Task 8.1: Add in wet deposition for BOB, using the following values:

for the 1st dissociation for the 1st dissociation for the 2nd dissociation for the 2nd dissociation

Note: If you were unable to successfully complete Task 7.1, then please take a copy of the h job from the Tutorial experiment (Tutorial: solution to Task 7.1 - add new dry deposition) and work from there, as this will allow you to only make the changes required for this task.

Remember: If you are using MONSooN you will need to delete/move any existing output files in your archive directory.

Solution


Written by Luke Abraham 2013