subroutine, public module_radiation_aerosols::setaer	(	real (kind=kind_phys), dimension(:,:), intent(in)	prsi,
		real (kind=kind_phys), dimension(:,:), intent(in)	prsl,
		real (kind=kind_phys), dimension(:,:), intent(in)	prslk,
		real (kind=kind_phys), dimension(:,:), intent(in)	tvly,
		real (kind=kind_phys), dimension(:,:), intent(in)	rhlay,
		real (kind=kind_phys), dimension(:), intent(in)	slmsk,
		real (kind=kind_phys), dimension(:,:,:), intent(in)	tracer,
		real (kind=kind_phys), dimension(:), intent(in)	xlon,
		real (kind=kind_phys), dimension(:), intent(in)	xlat,
		integer, intent(in)	IMAX,
		integer, intent(in)	NLAY,
		integer, intent(in)	NLP1,
		logical, intent(in)	lsswr,
		logical, intent(in)	lslwr,
		real (kind=kind_phys), dimension(:,:,:,:), intent(out)	aerosw,
		real (kind=kind_phys), dimension(:,:,:,:), intent(out)	aerolw,
		real (kind=kind_phys), dimension(:,:), intent(out)	aerodp
	)

Parameters

prsi	(IMAX,NLP1), pressure at interface in mb
prsl	(IMAX,NLAY), layer mean pressure in mb
prslk	(IMAX,NLAY), exner function = \((p/p0)^{rocp}\)
tvly	(IMAX,NLAY), layer virtual temperature in K
rhlay	(IMAX,NLAY), layer mean relative humidity
slmsk	(IMAX), sea/land mask (sea:0,land:1,sea-ice:2)
tracer	(IMAX,NLAY,NTRAC), aerosol tracer concentration
xlon	(IMAX), longitude of given points in radiance, ok for both 0->2pi or -pi->+pi ranges
xlat	(IMAX), latitude of given points in radiance, default to pi/2 -> -pi/2, otherwise see in-line comment
IMAX	1, horizontal dimension of arrays
NLAY,NLP1	1, vertical dimensions of arrays
lsswr,lslwr	logical flags for sw/lw radiation calls
aerosw	(IMAX,NLAY,NBDSW,NF_AESW), aeros opt properties for sw (:,:,:,1): optical depth (:,:,:,2): single scattering albedo (:,:,:,3): asymmetry parameter
aerolw	(IMAX,NLAY,NBDLW,NF_AELW), aeros opt properties for lw (:,:,:,1): optical depth (:,:,:,2): single scattering albedo (:,:,:,3): asymmetry parameter
aerodp	(IMAX,NSPC1), vertically integrated optical depth

setaer General Algorithm

1. Convert lat/lon from radiance to degree.
2. Compute level height and layer thickness.
3. Calculate SW aerosol optical properties for the corresponding frequency bands:
   • if opac aerosol climatology is used, call aer_property(): this subroutine maps the 5 degree global climatological aerosol data set onto model grids, and compute aerosol optical properties for SW and LW radiations.
   • if gocart aerosol scheme is used, call setgocartaer(): this subroutine computes sw + lw aerosol optical properties for gocart aerosol species (merged from fcst and clim fields).
4. Compute stratosphere volcanic forcing:
   • select data in 4 lat bands, interpolation at the boundaries
   • Find lower boundary of stratosphere: polar, fixed at 25000pa (250mb); tropic, fixed at 15000pa (150mb); mid-lat, interpolation
   • SW: add volcanic aerosol optical depth to the background value
   • Smoothing profile at boundary if needed
   • LW: add volcanic aerosol optical depth to the background value

References aer_property(), physcons::con_g, physparam::iaerflg, physparam::iaermdl, physparam::ivflip, physparam::lalwflg, physparam::laswflg, physparam::lavoflg, and setgocartaer().

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