N: 90 S: -90 E: 180 W: -180
Description
WARNING: To users of the derived product “co_mmr_midtrop” (carbon monoxide mass mixing ratio to dry air [kg/kg] at ~500 hPa). This variable has a significant bias due to a conversion error: the molecular weight of carbon dioxide (CO2, 44.01 g/mol) was used instead of carbon monoxide (CO, 28.01 g/mol). To correct, simply multiply “co_mmr_midtrop” by 28.01/44.01. Alternatively, derive a profile of mass mixing ratio from scratch using the retrieved column density values (“mol_lay/co_mol_lay”) in the Level 2 files. For further questions or concerns please contact the Sounder SIPS at: sounder.sips@jpl.nasa.gov
The CLIMCAPS (Community Long-term Infrared Microwave Coupled Product System) algorithm is used to analyze data from the Cross-track Infrared Sounder/Advanced Technology Microwave Sounder (CrIS/ATMS) instruments, also known as CrIMSS (Cross-track Infrared and Microwave Sounding Suite). The CrIS/ATMS instruments used for this product are on board the Suomi National Polar-orbiting Partnership (SNPP) platform and use the Full Spectral Resolution (FSR) data. The CrIS instrument is a Fourier transform spectrometer with a total of 2211 FSR infrared sounding channels covering the longwave (645-1095 cm-1), midwave (1210-1750 cm-1), and shortwave (2000-2550 cm-1) spectral regions. The ATMS instrument is a cross-track scanner with 22 channels in spectral bands from 23 GHz through 183 GHz.
The CLIMCAPS algorithm uses an Optimal Estimation methodology and uses an a-priori first guess to start the process. A CLIMCAPS sounding is comprised of a set of parameters that characterizes the full atmospheric state and includes a variety of geophysical parameters derived from the CrIMSS data. These include surface temperature and infrared emissivity; full atmosphere profiles of temperature, water vapor and ozone; infrared effective cloud top characteristics; carbon monoxide, methane, carbon dioxide, sulfur dioxide, nitrous oxide, and nitric acid.
A level 2 granule has been set as 6 minutes of data, 30 footprints cross track by 45 lines along track. There are 240 granules per day, with an orbit repeat cycle of approximately 16 day.
The CLIMCAPS algorithm uses data from the second Modern-Era Retrospective analysis for Research and Applications (MERRA-2) as a first-guess for the atmospheric state. Because MERRA-2 products typically have a latency from 3 to 7 weeks, so too do the CLIMCAPS products.
Product Summary
Citation
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Documents
ALGORITHM THEORETICAL BASIS DOCUMENT (ATBD)
PRODUCT QUALITY ASSESSMENT
Variables
Variables are a set of physical properties whose values determine the characteristics or behavior of something. For example, temperature and pressure are variables of the atmosphere. Parameters and variables can be used interchangeably. Variable level attributes provide individual information for each variable.
The Name in this table is the variable name. Fill value indicates missing or undefined data points in a variable. Valid range is the range of values the variable can store. Scale factor is used to increase or decrease the size of an object and can be used to correct for distortion. For questions on a specific variable, please use the Earthdata Forum.
| Name Sort descending | Description | Units | Data Type | Fill Value | Valid Range | Scale Factor |
|---|---|---|---|---|---|---|
| air_pres | pressure levels | Pa | float32 | 9.9692099683869E+36 | N/A | N/A |
| air_pres_h2o | H2O vapor pressure levels | Pa | float32 | 9.9692099683869E+36 | N/A | N/A |
| air_pres_h2o_nsurf | Index in air_pres_h2o of the level at the surface. Values at levels beyond this are invalid, representing data below the Earth's surface. | 1 | int16 | -32767 | N/A | N/A |
| air_pres_lay | pressure at the middle of each layer | Pa | float32 | 9.9692099683869E+36 | N/A | N/A |
| air_pres_lay_bnds | Min and max pressure of each layer | Pa | float32 | 9.9692099683869E+36 | N/A | N/A |
| air_pres_lay_nsurf | Index in air_pres_lay of the layer at the surface. Values for layers beyond this are invalid, representing data below the Earth's surface. | 1 | int16 | -32767 | N/A | N/A |
| air_pres_nsurf | Index in air_pres of the level at the surface. Values at levels beyond this are invalid, representing data below the Earth's surface. | 1 | int16 | -32767 | N/A | N/A |
| air_temp | air temperature profile | Kelvin | float32 | 9.9692099683869E+36 | N/A | N/A |
| air_temp_dof | The trace of the averaging kernel matrix as a measure of the number of pieces of information about the air temperature profile provided by the physical retrieval step. | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| air_temp_err | air_temp error estimate | Kelvin | float32 | 9.9692099683869E+36 | N/A | N/A |
| air_temp_qc | air_temp QC flag | N/A | int8 | -127 | N/A | N/A |
| asc_flag | ascending orbit flag: 1 if ascending, 0 descending | N/A | uint8 | 255 | N/A | N/A |
| asc_node_local_solar_time | local apparent solar time at the last ascending node before time_coverage_end in hours from midnight | hours | float32 | 9.9692099683869E+36 | N/A | N/A |
| asc_node_lon | Longitude of the last ascending node of spacecraft orbit before time_coverage_end. | degrees_east | float32 | 9.9692099683869E+36 | N/A | N/A |
| asc_node_tai93 | TAI93 time of the last ascending node of spacecraft orbit before time_coverage_end. | seconds since 1993-01-01 00:00 | float64 | 9.9692099683869E+36 | N/A | N/A |
| attitude_lbl | list of rotational directions (roll, pitch, yaw) | N/A | OTHER | N/A | N/A | N/A |
| aux/a0_cloud | intercept of alpha(1)=f(alpha(2)) fitting | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/aeff_1 | A_eff(1st eta step) | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/aeff_end | A_eff(last eta step) | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/ampl_eta | cloud clearing noise amplification factor | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/bad_mw_ret | Flag for bad microwave retrieval from bits 2 and 4 (values 2 and 8) of ispare_2. | N/A | uint8 | 255 | N/A | N/A |
| aux/bad_phys_ret | Flag for bad physical retrieval from bit 1 (value 1) of ispare_2. | N/A | uint8 | 255 | N/A | N/A |
| aux/bad_reg_ret | Flag for bad regression retrieval bits 3 and 5 (values 4 and 16) of ispare_2. | N/A | uint8 | 255 | N/A | N/A |
| aux/blue_spike_fire | Blue spike fire signal strength. Experimental. | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/bt2 | RMS(T(p) f/IR.ret - T(p) f/ AMSU.ret) | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/c2h6_dbt | Brightness temperature difference near 823 cm-1 indicating ethane. Values over +0.05 K are potential detections. Experimental. | Kelvin | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/c3h6_dbt | Brightness temperature difference near 911 cm-1 indicating propylene. Values over +0.05 K are potential detections. Experimental. | Kelvin | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/c5h8_dbt | Brightness temperature difference near 893 cm-1 indicating isoprene. Values over +0.05 K are potential detections. Experimental. | Kelvin | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/chi2_ch4 | Methane chi^2 of alpha(1)=f(alpha(2)) fitting | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/chi2_co | Carbon monoxide chi^2 of alpha(1)=f(alpha(2)) fitting | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/chi2_co2 | Carbon dioxide chi^2 of alpha(1)=f(alpha(2)) fitting | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/chi2_h2o | Water vapor chi^2 of alpha(1)=f(alpha(2)) fitting | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/chi2_hno3 | Nitric acid chi^2 of alpha(1)=f(alpha(2)) fitting | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/chi2_n2o | Nitrous oxide chi^2 of alpha(1)=f(alpha(2)) fitting | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/chi2_o3 | Ozone chi^2 of alpha(1)=f(alpha(2)) fitting | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/chi2_so2 | Sulfur dioxide chi^2 of alpha(1)=f(alpha(2)) fitting | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/chi2_temp | Temperature profile chi^2 of alpha(1)=f(alpha(2)) fitting | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/cldfrc_500 | Total cloud fraction over FOR below 500 hPa | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/cldfrc_tot | Total cloud fraction over FOR | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/clim_co2_mmr | Assumed carbon dioxide concentration | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/clim_surf_ir_emis | Infrared surface emissivity from the climatology first guess | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/clim_surf_ir_refl | infrared surface reflectivity from the climatology first guess | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/clim_surf_ir_wnum | Surface infrared emissivity frequencies (hinge points) for the climatology first guess | cm-1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/clim_surf_ir_wnum_cnt | Number of infrared surface emissivity frequencies for the climatology first guess | 1 | int16 | -32767 | N/A | N/A |
| aux/co2_vmr | carbon dioxide volume mixing ratio | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/co2_vmr_err | co2_vmr error estimate | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/co2_vmr_qc | co2_vmr QC flag | N/A | int8 | -127 | N/A | N/A |
| aux/etarej | cloud clearing residual used f/ rej at iteration = ieta_rej | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/fg_air_temp | air temperature profile from the MERRA2 first guess | Kelvin | float32 | 9.9692099683869E+36 | N/A | N/A |
| aux/fg_h2o_vap_mol_lay | water vapor layer totals from the MERRA2 first guess | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A |