CDF time Date Tue Jul 17 21:23:29 2012 Author NDave Turner, SSEC / University of Wisconsin - Madison (dturner@ssec.wisc.edu) Version M$Id: merge_mixcra_mwrret.pro,v 1.1 2012/07/16 21:38:52 dturner Exp dturner $ MWRRET_version M$Id: aer_mwr_retrieval.c,v 1.4 2006/05/22 10:39:47 dturner Release_ddt_1_4 $ MWRRET_processing_date Wed May 24 15:42:55 2006 CDT MWRRET_command_line _/home/dturner/work/aer_mwr_retrieval/mwrret/mwrret -N -p -c 300 -snsa -fC1 -n 9999 -d 20040326 MIXCRA_version ?$Id: phys_retrieval.c,v 4.11 2007/01/11 12:02:26 dturner Exp $ MIXCRA_processing_date Thu Feb 15 00:26:47 2007 CST MIXCRA_gas_od_scaling sMWR RET stat2 PWV data, if available, were used to scale the gaseous optical depths for the first guess (option 5) MIXCRA_LBLRTM_times m -2.00000, 1.00000, 4.00000, 7.00000, 10.00000, 13.00000, 16.00000, 19.00000, 22.00000, 25.00000 MIXCRA_SSP_water !ssp_db.mie_wat.gamma_sigma_0p100 MIXCRA_SSP_ice ssp_db.SolidCol.gamma.0p100 Missing_value -999.000 Comment This processing uses (a) the neural-network based hatch open-closed flag and (b) a monthly-varying Reff climatology (when this value cannot be retrieved from the AERI radiances) base_time long_name Base time in Epoch units $seconds since 1970-1-1 0:00:00 0:00 time_offset long_name Time offset from base_time units seconds hour long_name Hours since 00:00 UTC units Hour lwp long_name Liquid water path units g/m2 comment0 dThis field is the stat2_lwp field from MWRRET that has been calibrated to agree with the MIXCRA LWP comment1 |Calibration is performed by removing an offset from the MWRRET data, where the offset was determined from MIXCRA retrievals reffw long_name (Effective radius of the liquid droplets units microns comment0 PThe reffw_MIXCRA values are blended smoothly into climotological value of reffw Climotological_value 8.25000 phase_flag_mixcra long_name #Cloud phase determined from MIXCRA units unitless comment0 8Cloud phase flag from MIXCRA overlaid on this time-grid value0 5Value of 0 implies no cloud identified (i.e., clear) value1 Value of 1 implies liquid-only value2 Value of 2 implies ice-only value3 Value of 3 implies mixed-phase value4 Value of 4 implies opaque value5 1Value of 5 implies ambiguous or failed retrieval retrieval_comment0 pThe algorithm was run in dual-phase mode, but under certain conditions it will convert into a single-phase mode retrieval_comment1 QIf the cloud temperature is larger than 1 degC, will convert to liquid-only mode retrieval_comment2 QIf the cloud temperature is smaller than -40 degC, will convert to ice-only mode retrieval_comment3 hIf the surface-to-cloud-top transmittance at 560 cm-1 is less than 5%, will convert to liquid-only mode lwp_mixcra long_name Liquid water path from MIXCRA units g/m2 comment0 ?LWP retrievals directly from MIXCRA overlaid on this time-grid offset_lwp long_name LWP offsets applied units g/m2 comment0 *Determined off-line with manual smoothing comment1 1This offset was already applied to the field lwp reffw_mixcra long_name 4Effective radius of the liquid droplets from MIXCRA units microns comment0 dEffective radius retrievals of the liquid component determined by MIXCRA overlaid on this time-grid tauw_mixcra long_name Optical depth of the liquid units unitless comment0 aOptical depth retrievals of the liquid component determined by MIXCRA overlaid on this time-grid reffi_mixcra long_name 1Effective radius of the ice crystals from MIXCRA units microns comment0 aEffective radius retrievals of the ice component determined by MIXCRA overlaid on this time-grid taui_mixcra long_name Optical depth of the ice units unitless comment0 ^Optical depth retrievals of the ice component determined by MIXCRA overlaid on this time-grid t_cloud_mixcra long_name Cloud temperature from MIXCRA units K comment0 6Temperature of the cloud used in the MIXCRA retrieval lat long_name north latitude units degrees lon long_name east longitude units degrees alt long_name altitude units meters above Mean Sea Level @crBT@ > <(d A*Я@y y $y y y y y @7 <Ana@Fy y y y y y y @N <$Az@y y ~!y y y y y @U = A@.y y ?_y y y y y @^@ =3A@,Zy y jy y y y y @b =OXAnk@y y y y y y y @f =y,`A@y y 3y y y y y @i ==q@@y y |y y y y y @n` =IA@y y y y y y y @p =_A q@y y Ny y y y y @r =lA/@y y y y y y y @tp =X@+@y y Ty y y y y @v =A `@y y C_y y y y y @x? 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