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
The table below lists the variables contained within a single granule for this dataset. Variables often contain observed or derived geophysical measurements collected from a variety of sources, including remote sensing instruments on satellite and airborne platforms, field campaigns, in situ measurements, and model outputs. The terms variable, parameter, scientific data set, layer, and band have been used across NASA’s Earth science disciplines; however, variable is the designated nomenclature in NASA’s Common Metadata Repository (CMR). Variable metadata attributes such as Name, Description, Units, Data Type, Fill Value, Valid Range, and Scale Factor allow users to efficiently process and analyze the data. The full range of attributes may not be applicable to all variables. Additional information on variable attributes is typically available in the data, user guide, and/or other product documentation.
For questions on a specific variable, please use the Earthdata Forum.
| Name Sort descending | Description | Units | Data Type | Fill Value | Valid Range | Scale Factor | Offset |
|---|---|---|---|---|---|---|---|
| fov_obs_id | unique earth view observation identifier for FOV: yyyymmddThhmm.aaExx.f . Includes gran_id plus 2-digit along-track index (01-45), 2-digit cross-track index (01-30), and 1-digit FOV number (1-9). | N/A | OTHER | N/A | N/A | N/A | N/A |
| fov_surf_alt | mean surface altitude wrt earth model over the FOV | m | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| fov_surf_alt_sdev | standard deviation of surface altitude within the FOV | m | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| gp_hgt | Geopotential is the sum of the specific gravitational potential energy relative to the geoid and the specific centripetal potential energy. Geopotential height is the geopotential divided by the standard acceleration due to gravity. | m | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| gp_hgt_err | gp_hgt error estimate | m | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| gp_hgt_qc | gp_hgt QC flag | N/A | int8 | -127 | N/A | N/A | N/A |
| h2o_liq_mol_lay | cloud liquid water layer total | 1 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| h2o_liq_mol_lay_err | h2o_liq_mol_lay error estimate | 1 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| h2o_liq_mol_lay_qc | h2o_liq_mol_lay QC flag | N/A | int8 | -127 | N/A | N/A | N/A |
| h2o_liq_tot | total column cloud liquid water | kg m-2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| h2o_liq_tot_err | h2o_liq_ tot error estimate | kg m-2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| h2o_liq_tot_qc | h2o_liq_ tot QC flag | N/A | int8 | -127 | N/A | N/A | N/A |
| h2o_vap_dof | The trace of the averaging kernel matrix as a measure of the number of pieces of information about the water vapor profile provided by the physical retrieval step. | 1 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| h2o_vap_tot | total precipitable water vapor | kg / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| h2o_vap_tot_err | h2o_vap_tot error estimate | kg / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| h2o_vap_tot_qc | h2o_vap_tot QC flag | N/A | int8 | -127 | N/A | N/A | N/A |
| hno3_dof | The trace of the averaging kernel matrix as a measure of the number of pieces of information about the nitric acid profile provided by the physical retrieval step. | 1 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| ir_precip_est_24hr | The thickness of a layer of liquid water equivalent to the estimated preciptitation over 24 hours. | m | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| ir_precip_est_24hr_err | ir_precip_est_24hr error estimate | m | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| ir_precip_est_24hr_qc | ir_precip_est_24hr QC flag | N/A | int8 | -127 | N/A | N/A | N/A |
| land_frac | land fraction over the FOR | 1 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| lat | latitude of FOR center | degrees_north | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| lat_bnds | latitudes of points forming a polygon around the perimeter of the FOV | degrees_north | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| lat_geoid | latitude of FOR center on the geoid (without terrain correction) | degrees_north | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| local_solar_time | local apparent solar time in hours from midnight | hours | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| lon | longitude of FOR center | degrees_east | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| lon_bnds | longitudes of points forming a polygon around the perimeter of the FOV | degrees_east | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| lon_geoid | longitude of FOR center on the geoid (without terrain correction) | degrees_east | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mean_anom_wrt_equat | spacecraft mean anomaly measured with respect to the ascending node | degree | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/ch4_mol_lay | Methane layer total on 100 layers | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/ch4_mol_lay_err | ch4_mol_lay error estimate | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/ch4_mol_lay_qc | ch4_mol_lay QC flag | N/A | int8 | -127 | N/A | N/A | N/A |
| mol_lay/co_mol_lay | Carbon monoxide layer total on 100 layers | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/co_mol_lay_err | co_mol_lay error estimate | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/co_mol_lay_qc | co_mol_lay QC flag | N/A | int8 | -127 | N/A | N/A | N/A |
| mol_lay/h2o_vap_mol_lay | Water vapor layer total on 100 layers | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/h2o_vap_mol_lay_err | h2o_vap_mol_lay error estimate | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/h2o_vap_mol_lay_qc | h2o_vap_mol_lay QC flag | N/A | int8 | -127 | N/A | N/A | N/A |
| mol_lay/hno3_mol_lay | nitric acid layer total on 100 layers | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/hno3_mol_lay_err | hno3_mol_lay error estimate | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/hno3_mol_lay_qc | hno3_mol_lay QC flag | N/A | int8 | -127 | N/A | N/A | N/A |
| mol_lay/n2o_mol_lay | nitrous oxide layer total on 100 layers | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/n2o_mol_lay_err | n2o_mol_lay error estimate | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/n2o_mol_lay_qc | n2o_mol_lay QC flag | N/A | int8 | -127 | N/A | N/A | N/A |
| mol_lay/o3_mol_lay | Ozone layer total on 100 layers | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/o3_mol_lay_err | o3_mol_lay error estimate | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/o3_mol_lay_qc | o3_mol_lay QC flag | N/A | int8 | -127 | N/A | N/A | N/A |
| mol_lay/so2_mol_lay | sulfur dioxide layer total on 100 layers | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/so2_mol_lay_err | so2_mol_lay error estimate | molecules / m2 | float32 | 9.9692099683869E+36 | N/A | N/A | N/A |
| mol_lay/so2_mol_lay_qc | so2_mol_lay QC flag | N/A | int8 | -127 | N/A | N/A | N/A |