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 AIRS (Atmospheric Infrared Sounder) and AMSU (Advanced Microwave Sounding Unit). The AIRS instrument is a grating spectrometer (R = 1200) aboard the second Earth Observing System (EOS) polar-orbiting platform, EOS Aqua. The AIRS in combination with the AMSU constitutes an innovative atmospheric sounding group of infrared and microwave sensors. The AIRS Standard Retrieval Product consists of retrieved estimates of cloud and surface properties, plus profiles of retrieved temperature, water vapor, ozone, carbon monoxide and methane. The temperature profile vertical resolution is 100 levels total between 1100 mb and 0.1 mb, while moisture profile is reported at atmospheric layers between 1100 mb and 300 mb. The horizontal resolution is 50 km.
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.
This monthly one degree latitude by one degree longitude level-3 product starts with level-2 retrieval products applying the specific quality control (QC) methodology. Specific QC accepts profile level from the top of the atmosphere down to the level where the QC determines that it is still good. Below this level, the data is rejected.
Product Summary
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ALGORITHM THEORETICAL BASIS DOCUMENT (ATBD)
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_temp | air temperature profile on 100 levels | Kelvin | float32 | 9.9692099683869E+36 | N/A | N/A |
| ch4_mmr_midtrop | Methane mass mixing ratio to dry air at 40000 Pa, near the peak of sensitivity | kg / kg | float32 | 9.9692099683869E+36 | N/A | N/A |
| cld_frac | effective cloud fraction | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| cld_pres_lay | coarse cloud pressure layers | Pa | float32 | 9.9692099683869E+36 | N/A | N/A |
| cld_pres_lay_bnds | min and max pressure for coarse cloud layers | Pa | float32 | 9.9692099683869E+36 | N/A | N/A |
| cld_pres_lay_lbl | Altitude labels for cloud pressure layers | N/A | OTHER | N/A | N/A | N/A |
| cld_top_pres | cloud top pressure | Pa | float32 | 9.9692099683869E+36 | N/A | N/A |
| co2_vmr_uppertrop | Carbon Monoxide volume mixing ratio to dry air between 20,000-50,000 Pa, near the peak of sensitivity | m3 / m3 | float32 | 9.9692099683869E+36 | N/A | N/A |
| co_mmr_midtrop | Carbon Monoxide mass mixing ratio to dry air at 50000 Pa, near the peak of sensitivity | kg / kg | float32 | 9.9692099683869E+36 | N/A | N/A |
| dof/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 |
| dof/ch4_dof | The trace of the averaging kernel matrix as a measure of the number of pieces of information about the methane profile provided by the physical retrieval step. | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| dof/co2_dof | The trace of the averaging kernel matrix as a measure of the number of pieces of information about the carbon dioxide profile provided by the physical retrieval step. | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| dof/co_dof | The trace of the averaging kernel matrix as a measure of the number of pieces of information about the carbon monoxide profile provided by the physical retrieval step. | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| dof/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 |
| dof/o3_dof | The trace of the averaging kernel matrix as a measure of the number of pieces of information about the ozone profile provided by the physical retrieval step. | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| dof/surf_temp_dof | The trace of the averaging kernel matrix as a measure of the number of pieces of information about the surface provided by the physical retrieval step. | 1 | float32 | 9.9692099683869E+36 | 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 |
| h2o_vap_tot | total precipitable water vapor | kg / m2 | float32 | 9.9692099683869E+36 | N/A | N/A |
| lat | Degrees latitude | degrees_north | float32 | 9.9692099683869E+36 | N/A | N/A |
| lat_bnds | min and max degrees for each longitude grid cell | degrees_north | float32 | 9.9692099683869E+36 | N/A | N/A |
| lay_cld_frac | coarse layer effective cloud fraction | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| lon | Degrees longitude | degrees_east | float32 | 9.9692099683869E+36 | N/A | N/A |
| lon_bnds | min and max degrees for each longitude grid cell | degrees_east | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/air_temp_nobs | air_temp number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/ch4_mmr_midtrop_nobs | ch4_mmr_midtrop number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/cld_frac_nobs | cld_frac number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/cld_top_pres_nobs | cld_top_pres number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/co2_vmr_uppertrop_nobs | co2_vmr_uppertrop number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/co_mmr_midtrop_nobs | co_mmr_midtrop number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/gp_hgt_nobs | gp_hgt number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/h2o_vap_tot_nobs | h2o_vap_tot number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/nobs_max | Maximum number of observations including those for which no value was retrieved. Can be used with *_nobs to calculate yield. | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/o3_tot_nobs | o3_tot number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/prior_surf_pres_nobs | prior_surf_pres number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/rel_hum_nobs | rel_hum number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/spec_hum_nobs | spec_hum number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/surf_air_temp_nobs | surf_air_temp number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/surf_alt_nobs | surf_alt number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/surf_ir_emis_nobs | surf_ir_emis number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/surf_temp_nobs | surf_temp number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| nobs/tpause_pres_nobs | tpause_pres number of observations | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |
| o3_tot | Total column ozone. (Multiply by 4.670e5 to convert to Dobson Units from kg m^-2) | kg / m2 | float32 | 9.9692099683869E+36 | N/A | N/A |
| obs_time_tai93 | Nominal midtime for observations included in grid | seconds since 1993-01-01 00:00 | float64 | 9.9692099683869E+36 | N/A | N/A |
| obs_time_tai93_bnds | Nominal start and end time for observations included in grid | seconds since 1993-01-01 00:00 | float64 | 9.9692099683869E+36 | N/A | N/A |
| obs_time_utc | Nominal midtime for observations included in grid as an array of integers: year, month, day, hour, minute, second, millisec, microsec | N/A | uint16 | 65535 | N/A | N/A |
| orbit_pass | Nominal solar time when the spacecraft passes over the equator. Orbit pass bounds are defined by closest approach of the spacecraft to the poles. | hours | float32 | 9.9692099683869E+36 | N/A | N/A |
| prior_surf_pres | surface pressure from forecast for observations | Pa | float32 | 9.9692099683869E+36 | N/A | N/A |
| rel_hum | relative humidity over equilibrium phase | 1 | float32 | 9.9692099683869E+36 | N/A | N/A |