Development of Fast-JX in GEOS-Chem: Difference between revisions
(New page: This page describes the implementation of Fast-JX in GEOS-Chem. ==A few things about Fast-JX== I implemented Fast-JX (v6.2) into GEOS-Chem v8-01-02. This version of Fast-JX includes 18 bi...) |
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==A few things about Fast-JX== | ==A few things about Fast-JX== | ||
I implemented Fast-JX (v6.2) into GEOS-Chem v8-01-02. This version of Fast-JX includes 18 bins of wavelengths. A few | I implemented Fast-JX (v6.2) into GEOS-Chem v8-01-02. This version of Fast-JX includes 18 bins of wavelengths. A few good things for this new version: | ||
* This version can be used for stratospheric chemistry with 11 wavelength bins in UV. | * This version can be used for stratospheric chemistry with 11 wavelength bins in UV. | ||
* This version of Fast-JX handles thick clouds much better, because it uses a log-spacing to add sub-layers for thick clouds or aerosol layers. | * This version of Fast-JX handles thick clouds much better, because it uses a log-spacing to add sub-layers for thick clouds or aerosol layers. We had some problems in the standard version when cloud or aerosols are too thick (the old Fast-J uses linear spacing to ad sub-layers). See [[Photolysis_mechanism#Too_many_levels_in_photolysis_code|Too many levels in photolysis_code]]. | ||
* This version of Fast-JX is supposed to do a better job over polar region. | * This version of Fast-JX is supposed to do a better job over polar region,where solar zenith angle gets close to 90. | ||
* I combined most files into one module: fast_jx_mod.f. This will provide a much better platform to get updates from newer version of Fast-JX. | * I combined most files into one module: fast_jx_mod.f. This will provide a much better platform to get updates from newer version of Fast-JX for future development. | ||
* Fast-JX takes into account the photolysis of O2, which will make a little bit more ozone in upper troposphere. | * Fast-JX takes into account the photolysis of O2, which will make a little bit more ozone in upper troposphere. | ||
If you need the source code, please contact [mailto:Jingqiu.Mao@noaa.gov Jingqiu Mao] on this. | If you need the source code, please contact [mailto:Jingqiu.Mao@noaa.gov Jingqiu Mao] on this. |
Revision as of 21:00, 15 November 2011
This page describes the implementation of Fast-JX in GEOS-Chem.
A few things about Fast-JX
I implemented Fast-JX (v6.2) into GEOS-Chem v8-01-02. This version of Fast-JX includes 18 bins of wavelengths. A few good things for this new version:
- This version can be used for stratospheric chemistry with 11 wavelength bins in UV.
- This version of Fast-JX handles thick clouds much better, because it uses a log-spacing to add sub-layers for thick clouds or aerosol layers. We had some problems in the standard version when cloud or aerosols are too thick (the old Fast-J uses linear spacing to ad sub-layers). See Too many levels in photolysis_code.
- This version of Fast-JX is supposed to do a better job over polar region,where solar zenith angle gets close to 90.
- I combined most files into one module: fast_jx_mod.f. This will provide a much better platform to get updates from newer version of Fast-JX for future development.
- Fast-JX takes into account the photolysis of O2, which will make a little bit more ozone in upper troposphere.
If you need the source code, please contact Jingqiu Mao on this.
How does the new Fast-JX work?
Fast-JX calculates scattering at five wavelength 200nm, 300nm, 400nm, 600nm and 999nm. Fast-J calculates at four wavelength 300nm, 400nm, 600nm and 999nm (without 200nm).
- In chemdr.f, Fast-JX is initialized (call INPHOT(LLTROP, NPHOT)).
- In chemdr.f, Fast-JX is calculated by calling FAST_J( SUNCOS, OPTD, UVALBEDO).
- In fast_j.f, it was first determined which cloud overlap scheme (linear, random,or maximum) to be used. Then send single column properties to PHOTOJ for calculation, including:
- pressure profile
- temperature profile
- surface albedo
- Aerosol OD profile
- Mineral dust OD profile
- Cloud OD profile
- In calcrate.f, send J-values to smvgear by calling fjfunc.f.
Modules in fast_jx_mod.f
- INPHOT
- Read in labels of photolysis (call RD_JS)
- Match Fast-JX species with Harvard species (call JV_INDEX)
- Read in Fast-JX X-sections (spectral data) (call RD_XXX)
- Read in T & O3 climatology (call RD_PROF)
- Select aerosol/cloud types to be used (call SET_AER)
- PHOTOJ
- Set up Air, O3, BC profiles on GEOS-Chem vertical levels (call set_prof.f), this is the same as the old fast-j.
- calculate air mass factors by calling sphere2. This is different from the old fast-j: the new AMF2 does each of the half-layers of the CTM separately, whereas the original, based on the pratmo code did the whole layers and thus calculated the ray-path to the CTM layer edges, NOT the middle.
- add sub-layers (JXTRA) to thick cloud/aerosol layers by calling EXTRAL. This version sets up log-spaced sub-layers of increasing thickness ATAU. Given the aerosol+cloud OD/layer in visible (600 nm) calculate how to add additonal levels at top of clouds (now uses log spacing). This was linear spacing in Fast-J, so caused lots of problems for thick clouds.
- For each wavelength bin, call OPMIE to calculate the mean actinic flux in each layer (AVGF), then save the flux into FFF (1:LPAR).
- call JRATET to convert FFF to J-values for all species.
How does the current Fast-J work in GEOS-Chem?
Step 1: inphot.f
Require input files (cmn_fj.h, jv_cmn.h, ratj.d, jv_spec.dat, jv_atms.dat)
- Error check # of layers (call ERROR_STOP)
- Read in labels of photolysis rates required (call RD_JS.f)
- translate between GEOS-Chem species nomenclature and Fast-J species nomenclature(call JV_INDEX.f)
- Read in JPL spectral data set (e.g. X-sections, quantum yields) (call RD_TJPL.f)
- Read in T & O3 climatology (cf. Nagatani/92 and McPeters/91) (call RD_PROF.f)
- Select Aerosol/Cloud types to be used (call SET_AER.f)
Step 2: fast_j.f
For each (NLON,NLAT) location, call subroutine PHOTOJ (in a parallel loop to compute J-values for the entire column. J-values will be stored in the common-block variable ZPJ, and will be later accessed via function FJFUNC).
- Read TOMS O3 columns if it's a new month(call READ_TOMSO3 from "toms_mod.f“).
- Cloud overlap options
- Linear Approximation (used up to v7-04-12)->call photoj.f
- Approximate Random Overlap (default)->call photoj.f
- Maximum Random Overlap (MRAN, computation intensive)->call photoj.f+mmran_16.f
Step 3: photoj.f
- Set up Air, O3, BC profiles on GEOS-Chem vertical levels (call set_prof.f)
- Set up cloud and surface properties (Call CLDSRF.f).
- Set up pressure levels for O3/T climatology.
- Select appropriate monthly and latitudinal profiles
- Apportion O3 and T on supplied climatology z* levels onto CTM levels with mass (pressure) weighting, assuming constant mixing ratio and temperature half a layer on either side of the point supplied.
- Calculate effective altitudes using scale height at each level
- Add aerosol column - include aerosol types here. Currently use soot water and ice; assume black carbon x-section of 10 m2/g, independent of wavelength; assume limiting temperature for ice of -40 deg C.
- Calculate column quantities for FAST-J: monthly mean air column and monthly mean O3 column.
- Weight the O3 column by the observed monthly mean TOMS data.
- Interpolate O3 column to current day (TOMS data is half month time resolution). Scale monthly O3 profile to the daily O3 profile.
- Compute actinic flux at each GEOS-CHEM vertical level (call JVALUE.f). In which, calculate air mass factors for each layer (call sphere.f). Loop over all wavelength bins to call OPMIE.f:
- Pick nearest Mie wavelength, no interpolation.
- For Mie code scale extinction at 1000 nm to wavelength WAVEL (QXMIE)
- Set up total optical depth over each CTM level, DTAUX
- Fractional extinction for Rayleigh scattering and each aerosol type
- Define the scattering phase fn. with mix of Rayleigh(1) & Mie(MIEDX), No. of quadrature pts fixed at 4 (M__), expansion of phase fn @ 8
- Calculate attenuated incident beam EXP(-TTAU/U0) and flux on surface
- Take optical properties on CTM layers and convert to a photolysis level grid corresponding to layer centres and boundaries
- Calculate cumulative total and define levels we want J-values at. Sum upwards for levels, and then downwards for Mie code readjustments.
- SET UP FOR MIE CODE. Transpose the ascending TTAU grid to a descending ZTAU grid. This is required so that J-values can be calculated for the centre of CTM layers; the index of these layers is kept in the jndlev array.
- Insert new levels, working downwards from the top of the atmosphere to the surface (down in 'j', up in 'k').
- call MIESCT.f
- (1) fix scattering to 4 Gauss pts = 8-stream(CALL GAUSSP.f)
- (2) solve eqn of R.T. only for first-order M=1(call LEGND0.f)
- (3) call BLKSLV.f to solve the block tri-diagonal system.
- (4) call GEN.f and MATIN4.f.
- Calculate J-values for all species(call JRATET.f)
- Scale actinic flux (FFF) by Solar distance factor (SOLF)
- With model temperature, call XSECO2.f(FLINT.f); call XSECO3.f(FLINT.f); call XSEC1D.f(FLINT.f)
- Calculate Jvalues for O2,O3,O1D
- Calculate remaining J-values with T-dep X-sections
Step 4: fjfunc.f
supplies J-values to SMVGEAR solver
Implementation of Fast-JX
New input files
- spec2008.dat: fast-J X-sections (spectral data)
- atmos_std.dat: T & O3 climatology data
- chemJ2008.d: this is a tranfer map from the J's automatically calculated in fast-JX onto the names and order in the users chemistry code.
Major changes
- Aerosol_mod.f
old | new |
---|---|
# include "cmn_fj.h" # include "jv_cmn.h" | # include "fj2008.h" |
RW(R) = RAA(4,IND(N)+R-1) | RW(R) = RAA(5,IND(N)+R-1) |
QW(R) = QAA(4,IND(N)+R-1)*FWET + QAA(4,IND(N))*(1.d0-FWET) | QW(R) = QAA(5,IND(N)+R-1)*FWET + QAA(5,IND(N))*(1.d0-FWET) |
WAERSL(I,J,L,N) * QAA(4,IND(N)) | WAERSL(I,J,L,N) * QAA(5,IND(N)) |
DAERSL(I,J,L,N-1) * QAA(4,IND(N)) | DAERSL(I,J,L,N-1) * QAA(5,IND(N)) |
REFF = 1.0D-4 * RAA(4,IND(N)) | REFF = 1.0D-4 * RAA(5,IND(N)) |
QAA(2,IND(N)+R-1) / QAA(4,IND(N)+R-1) | QAA(3,IND(N)+R-1) / QAA(5,IND(N)+R-1) |
All these are because there is one more wavelength bin for mie scattering(200nm), so RAA (effective radius) and QAA(aerosol extinction coefficient) all need to be changed accordingly.
- dust_mod.f
old | new |
---|---|
# include "cmn_fj.h" # include "jv_cmn.h" | # include "fj2008.h" |
DUST(I,J,L,N) * QAA(4,14+N)/ ( MSDENS(N) * RAA(4,14+N) * 1.0D-6 ) | DUST(I,J,L,N) * QAA(5,14+N)/ ( MSDENS(N) * RAA(5,14+N) * 1.0D-6 ) |
ERADIUS(JLOOP,N) = RAA(4,14+N) * 1.0D-4 | ERADIUS(JLOOP,N) = RAA(5,14+N) * 1.0D-4 |
( ODMDUST(I,J,L,N) * QAA(2,14+N) / QAA(4,14+N) ) | ( ODMDUST(I,J,L,N) * QAA(3,14+N) / QAA(5,14+N) ) |
DUST(I,J,L,N) * QAA(4,14+N) / ( MSDENS(N) * RAA(4,14+N) * 1.0D-6 ) | DUST(I,J,L,N) * QAA(5,14+N)/ ( MSDENS(N) * RAA(5,14+N) * 1.0D-6 ) |
ERADIUS(JLOOP,N) = RAA(4,14+N) * 1.0D-4 | ERADIUS(JLOOP,N) = RAA(5,14+N) * 1.0D-4 |
( ODMDUST(I,J,L,N) * QAA(2,14+N) / QAA(4,14+N) ) | ( ODMDUST(I,J,L,N) * QAA(3,14+N) / QAA(5,14+N) ) |
- fast_j.f, fjfunc.f, fjfunc.f
USE FAST_JX_MOD, ONLY : PHOTOJ | |
# include "cmn_fj.h" # include "jv_cmn.h" | # include "fj2008.h" |
- fast_jx_mod.f- this is a new file and it is the main file for Fast-J.
- planeflight_mod.f
old | new |
---|---|
# include "cmn_fj.h" # include "jv_cmn.h" | # include "fj2008.h" |
S400nm = QAA(2,IND(N)+RH-1) / & QAA(4,IND(N)+RH-1) | S400nm = QAA(3,IND(N)+RH-1) / & QAA(5,IND(N)+RH-1) |
S400nm = QAA(2,IND(N)+RH-1) / & QAA(4,IND(N)+RH-1) | S400nm = QAA(3,IND(N)+RH-1) / & QAA(5,IND(N)+RH-1) |
- ch3i_mod.f
add this line at the beginning; “USE FAST_JX_MOD” Because ch3i_mod.f needs fast_j to calculate something for ch3i simulations.
- Chemdr.f
Add this line: “USE FAST_JX_MOD, ONLY : INPHOT” Because inphot.f is now merged into fast_jx_mod.f
- chemistry_mod.f
Add this line: USE FAST_JX_MOD
- diag48_mod.f, diag49_mod.f, diag50_mod.f, diag51_mod.f
old | new |
---|---|
USE FAST_JX_MOD, ONLY : PHOTOJ | |
# include "cmn_fj.h" # include "jv_cmn.h" | # include "fj2008.h" |
Files removed from v8-01-02
Filename | Notes |
---|---|
BLKSLV.f | Merged into “fastjx_mod.f” |
CLDSRF.f | Merged into “fastjx_mod.f” |
cmn_fj.h | Input files, now merged into “fj2008.h”. |
EFOLD.f | Removed, not even used in fast-j |
FLINT.f | Merged into “fastjx_mod.f” (Three-point linear interpolation function) |
GAUSSP.f | Merged into “fastjx_mod.f” |
GEN.f | Merged into “fastjx_mod.f” |
inphot.f | Merged into “fastjx_mod.f” |
JRATET.f | Merged into “fastjx_mod.f” |
JVALUE.f | Merged into PHOTOJ in “fastjx_mod.f” |
jv_cmn.h | Input files, now merged into “fj2008.h”. |
jv_index.f | Merged into “fastjx_mod.f” |
jv_mie.h | Input files, now merged into “fj2008.h”. |
LEGND0.f | Merged into “fastjx_mod.f” |
MATIN4.f | Merged into “fastjx_mod.f” |
MIESCT.f | Merged into “fastjx_mod.f” |
NOABS.f | Removed, not even used in fast-j |
OPMIE.f | Merged into “fastjx_mod.f” |
photoj.f | Merged into “fastjx_mod.f” |
rd_js.f | Merged into “fastjx_mod.f” |
rd_prof.f | Merged into “fastjx_mod.f” |
RD_TJPL.f | This is changed to “RD_XXX” in “fastjx_mod.f”. |
set_aer.f | Merged into “fastjx_mod.f” |
set_prof.f | Merged into “fastjx_mod.f” |
SPHERE.f | Merged into “fastjx_mod.f”, now changed to sphere2 function. |
XSEC1D.f | Merged into PHOTOJ in “fastjx_mod.f” |
XSECO2.f | Merged into PHOTOJ in “fastjx_mod.f” |
XSECO3.f | Merged into PHOTOJ in “fastjx_mod.f” |