NetCDF parameter
From Atomix
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ATOMIX subgroup | Parameter (short) Name | CF parameter | Standard name | Units of measurement | Long name | Dir positive | Reference datum | Data code | fillValue | validMin | validMax | NetcDF type | ||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
All | TIME | 1 | time | days, or Days since YYYY-MM-DDT00:00:00Z | Decimal day | days since 1950-01-01 00:00 UTC | -999999 | float | Why not seconds since 1950-01-01 00:00 | |||||
All | PRES | 1 | sea_water_pressure | dbar | Sea water pressure, equals 0 at sea-level | down | -999999 | float | ||||||
All | DEPTH | 1 | depth | m | down | sea surface | Z | -999999 | -5 | 12000 | float | |||
All | LATITUDE | 1 | latitude | degrees_north | WGS84 geographic coordinate system | -999999 | -90 | 90 | float | |||||
All | LONGITUDE | 1 | longitude | degrees_east | WGS84 geographic coordinate system | -999999 | -180 | 180 | float | |||||
All | TEMP | 1 | sea_water_temperature | degrees_Celsius | sea water temperature in-situ ITS-90 scale | T | -999999 | -2.5 | 40 | float | ||||
All | CNDC | 1 | sea_water_electrical_conductivity | S m-1 | C | -999999 | 0 | 50000 | float | |||||
All | PSAL | 1 | sea_water_practical_salinity | 1 | S | -999999 | 0 | 41 | float | |||||
All | DENS | 1 | sea_water_density | kg m-3 | D | -999999 | float | |||||||
All | BVFSQ | 1 | square_of_brunt_vaisala_frequency_in_sea_water | (rad s-1)2 | T | -999999 | 0 | 10000 | float | Copied from CF: The phrase "square_of_X" means X*X. Frequency is the number of oscillations of a wave per unit time. Brunt-Vaisala frequency is also sometimes called "buoyancy frequency" and is a measure of the vertical stratification of the medium. | ||||
All | CSPD | 1 | water_speed | m s-1 | V | -999999 | 0 | 10 | float | |||||
All | PITCH | 1 | platform_pitch_angle | degree | -999999 | -180 | 180 | float | ||||||
All | HEADING | 1 | platform_yaw_angle | degree | clockwise | true North | -999999 | 0 | 360 | float | ||||
All | HEADING_MAG | 1 | platform_yaw_angle | degree | clockwise | magnetic North | -999999 | 0 | 360 | float | ||||
All | ROLL | 1 | platform_roll_angle | degree | -999999 | -180 | 180 | float | ||||||
All | EPSI | 1 | specific_turbulent_kinetic_energy_dissipation_in_sea_water | W kg-1 | dissipation rate of turbulent kinetic energy per unit mass in sea water estimated from individual shear probes / beams | T | -999999 | 1.00E-12 | 1.00E+00 | float | Copied from CF standard table: "Specific" means per unit mass. "Turbulent kinetic energy" is the kinetic energy of chaotic fluctuations of the fluid flow. | |||
All | EPSI_FINAL | 0 | specific_turbulent_kinetic_energy_dissipation_in_sea_water | W kg-1 | final dissipation rate of turbulent kinetic energy per unit mass in sea water (averaged using all accepted shear probes / beams / or best estimate from single channel) | -999999 | double | This is the average (over probes, beams), final estimate | ||||||
All | K_TEMP | 0 | water_vertical_diffusivity_of_heat | m2 s-1 | T | -999999 | 1.00E-12 | 100 | float | |||||
All | K_RHO | 0 | water_diapycnal_diffusivity | m2 s-1 | T | -999999 | 1.00E-12 | 100 | float | |||||
All | KAPPA_TEMP | 0 | seawater_molecular_diffusivity_temperature | m2 s-1 | P | -999999 | 1.00E-09 | 1.00E-05 | float | |||||
All | KVISC | 0 | kinematic_viscosity_of_water | m2 s-1 | Kinematic viscosity of (sea) water | P | -999999 | 1.00E-08 | 1.00E-04 | float | ||||
All | dTEMP_dZ | 0 | derivative_of_seawater_temperature_wrt_z | degrees_Celsius m-1 | T | -999999 | 0 | 100 | float | |||||
All | PROFILE | 0 | unique_identifier_for_each_profile_feature_instance_in_this_file | 1 | -999999 | int | Copied from IMOS | |||||||
All | SECTION_NUMBER | 0 | unique_identifier_for_each_section_of_data_from_timeseries | 1 | A unique indentifier counter defining sections of the time series from the fast (or slow) channels extracted for dissipation estimates | -999999 | int | More useful for ADV/ADCP. | ||||||
All | PSPD_REL | 1 | platform_speed_wrt_sea_water | m s-1 | Platform speed with respect to sea water | -999999 | float | |||||||
Shear Probes | SHEAR | 0 | sea_water_velocity_shear | s-1 | rate of change of cross axis sea water velocity along transect measured by shear probes | -999999 | double | |||||||
Shear Probes | VIB | 0 | platform_vibration | 1 | platform vibration detected by piezo-accelerometers | -999999 | double | |||||||
Shear Probes | ACC | 0 | platform_acceleration | m s-2 | platform acceleration detected by accelerometers | -999999 | double | |||||||
Shear Probes | SH_SPEC | 0 | shear_probe_spectrum | s-2 cpm-1 | cyclic wavenumber spectrum of sea water velocity shear | -999999 | 1.00E-12 | 1.00E+00 | float | Matrix where every column represents a shear probe. | ||||
Shear Probes | SH_SPEC_CLEAN | 0 | shear_probe_spectrum_clean | s-2 cpm-1 | cleaned cyclic wavenumber spectrum of sea water velocity shear | -999999 | float | |||||||
Shear Probes | A_SPEC | 0 | acceleration_sensor_spectrum | m2 s-4 cpm-1 | acceleration spectrum from accelerometers | -999999 | 1.00E-12 | 1.00E+00 | float | Matrix where every column represents a acceleration sensor. | ||||
Shear Probes | AP_SPEC | 0 | vibration_sensor_spectrum | 1 | vibration spectrum from vibration sensors | -999999 | 1.00E-12 | 1.00E+12 | float | Matrix where every column represents a vibration sensor. | ||||
Shear Probes | SH_A_SPEC | 0 | shear_and_acceleration_cross-spectral_matrix | Complex cross-spectral matrix of shear and acceleration | -999999 | float | ||||||||
Shear Probes | SH_AP_SPEC | 0 | shear_and_vibration_cross-spectral_matrix | Complex cross-spectral matrix of shear and vibration | -999999 | float | ||||||||
ADV/Shear probes | KMAX | 0 | maximum_wavenumber_used_for_estimating_turbulent_kinetic_energy_dissipation | cpm | maximum wavenumber for integration of shear spectrum | -999999 | 0 | 1000 | float | |||||
Shear probes | FOM | 0 | figure_of_merit | - | Figure of merit of shear spectrum relative to the model spectrum. It is MAD multiplied by the sqrt( degrees of freedom) of the spectra | -999999 | float | |||||||
ADV/Shear probes | MAD | 0 | mean_absolute_deviation | - | mean absolute deviation of shear spectrum relative to the model spectrum | -999999 | float | |||||||
ADV/Shear probes | DOF | 0 | degrees_of_freedom_of_spectrum | -999999 | 0 | 500 | float | |||||||
ADV/Shear probes | FREQ | 0 | frequency | Hz | -999999 | 0 | 1.00E+04 | float | ||||||
ADV/Shear probes | FREQ_W | 0 | angular_frequency | rad s-1 | -999999 | 0 | 1.00E+04 | float | ||||||
ADV/Shear probes | KCYC | 0 | cyclic_wavenumber | cpm | wavenumber along the direction of instrument motion in cycles per meter | -999999 | 0 | 1.00E+04 | float | |||||
ADV | MAD_SQRT_DOF | 0 | mean_absolute_deviation_multiplied_sqrt_of_degrees_of_freedom | -999999 | 0 | 1000 | float | |||||||
ADV | KMIN | 0 | minimum_wavenumber_used_for_estimating_turbulent_kinetic_energy_dissipation | cpm | minimum wavenumber for integration of shear spectrum | -999999 | 0 | 1000 | float | |||||
ADV | DIR_CSPD | 0 | direction_of_water_speed | degree | counterclockwise | east | -999999 | 0 | 360 | float | ||||
ADV | ROT_AXIS | 0 | axis_of_rotation_from_east_to_x | Axis i,j.k in geographical coordinates that must be used to rotate from geographical to flow frame of reference | -999999 | -1 | 1 | float | ||||||
ADV | ROT_ANGLE | 1 | angle_of_rotation_from_east_to_x | degree | Used to rotate from geographical to flow frame of reference via the specified axis_of_rotation | counterclockwise | east | -999999 | 0 | 360 | float | |||
ADV | ANISO | 0 | ratio_of_large_turbulence_length_scale_to_smallest_kolmogorov_length | - | -999999 | 1 | float | |||||||
ADV | UVW_VEL | 0 | water_velocity_rotated_in_direction_of_water_speed | ms-1 | The measurements have been rotated into a frame of reference for which the x (longitudinal) axis coincides with the direction of mean water speed | Background flow | V | -999999 | -10 | 10 | float | |||
ADV | UVW_VEL_SPEC | 0 | power_spectrum_density_of_velocity_in_the_flow_frame_of_reference | (m s-1)2 s | Summation of the spectra across all frequencies is equal to the signal's variance in time-domain. | V | -999999 | 1.00E-12 | 1.00E+00 | float | Takes less space to simply save the spectra in frequency space. Avoids having a large matrix for the time-variable wavenumber vector | |||
ADV | XYZ_VEL | 0 | water_velocity_measured_in_instrument_coordinates | ms-1 | V | -999999 | -10 | 10 | float | |||||
ADV | ENU_VEL | 0 | water_velocity_in_geographical_east_north_up_coordinates | ms-1 | Geographical | V | -999999 | -10 | 10 | float | ||||
ADV | ENU_VEL_DETRENDED | 0 | detrended_water_velocity_in_geographical_east_north_up_coordinates | ms-1 | Includes surface wave and turbulence contributions | V | -999999 | -5 | 5 | float | ||||
ADV | UVW_VEL_DETRENDED | 0 | detrended_water_velocity_in_the_flow_frame_of_reference | ms-1 | Includes surface wave and turbulence contributions. The UVW velocities are those rotated in the direction of mean water speed using a 3D axis of rotation | V | -999999 | -5 | 5 | float | ||||
ADV | UVW_VEL_RMS | 0 | root_mean_square_of_velocity_in_flow_frame_of_reference | ms-1 | An rms calculation on a detrended timeseries (mean removed) is the same as the standard deviation | V | -999999 | 0 | 5 | float | ||||
ADV | UVW_VEL_STD | 0 | standard_deviation_of_velocity_in_the_flow_frame_of_reference | ms-1 | V | -999999 | 0 | 5 | float | |||||
ADV | TAYL | 0 | ratio_of_rms_turb_U_to_water_speed | - | T | -999999 | 0 | 10000 | float | |||||
ADV | SNR | 0 | signal_noise_ratio_from_each_acoustic_beam | decibel | A | -999999 | 0 | 150 | float | |||||
ADV | ABSIC | 0 | backscater_intensity_from_each_acoustic_beam | count | AlongBeam_distance | A | -999999 | 0 | float | |||||
ADV | CORRN | 0 | noise_correlation_percent_from_each_acoustic_beam | percent | E | -999999 | 0 | 100 | float | |||||
ADV | N_VEL_INSTRUMENT | 0 | number_of_unique_velocity_instruments | - | D | -999999 | 1 | int | ||||||
ADV | N_VEL_COMPONENT | 0 | number_of_velocity_component | - | D | -999999 | 1 | 3 | int | |||||
ADV | SPEC_SLOPE | 0 | estimated_spectral_slope_of_fitted_wavenumbers_in_logspace | - | Nonlinear least square fit to find most likely spectral slope | T | -999999 | float | ||||||
ADV | SPEC_SLOPE_CI_LOW | 0 | low_limit_confidence_interval_of_spectral_slope_in_logspace | - | T | -999999 | float | |||||||
ADV | SPEC_SLOPE_CI_HIGH | 0 | high_limit_confidence_interval_of_spectral_slope_in_logspace | - | T | -999999 | float | |||||||
ADV/ADCP | dUCUR_dZ | 0 | derivative_of_eastward_velocity_wrt_z | s-1 | V | -999999 | -10 | 10 | float | |||||
ADV/ADCP | dVCUR_dZ | 0 | derivative_of_northtward_velocity_wrt_z | s-1 | V | -999999 | -10 | 10 | float | |||||
ADV/ADCP | dWCUR_dZ | 0 | derivative_of_upward_velocity_wrt_z | s-1 | V | -999999 | -5 | 5 | float | |||||
ADV/ADCP | HEIGHT_AB | 1 | height_above_bottom | m | up | bottom | D | -999999 | 0 | 12000 | float | |||
ADV/ADCP | BURST_NUMBER | 0 | unique_identifier_for_each_burst_in_this_file | - | D | -999999 | 1 | int | Meant to accomade burst sampling programs. A burst may be longer than # of samples required for a spectra or structure fct calc | |||||
ADV/ADCP | PERG | 0 | percentage_of_samples_good | percent | E | -999999 | 0 | 100 | float | |||||
ADV/ADCP | N_BEAMS | 0 | beam_number_of_the_instrument | D | -999999 | 1 | 10 | int | ||||||
ADCP | ABSI | 0 | backscatter_intensity_from_each_acoustic_beam | decibel | AlongBeam_distance | -999999 | 0 | float | ||||||
ADCP | ABSI5 | 0 | backscatter_intensity_from_acoustic_beam_5 | decibel | AlongBeam_distance | -999999 | 0 | float | ||||||
ADCP | CORR | 0 | correlation_magnitude_from_each_acoustic_beam | AlongBeam_distance | -999999 | 0 | float | |||||||
ADCP | CORR5 | 0 | correlation_magnitude_from_acoustic_beam_5 | AlongBeam_distance | -999999 | 0 | float | |||||||
ADCP | R_DIST | 0 | distance_from_sensor_along_beams | m | outwards from transducer | sensor | -999999 | 0 | dimension | |||||
ADCP | HEIGHT_AS | 1 | height_above_sensor | m | up | sensor | Z | -999999 | -12000 | 12000 | float | |||
ADCP | THETA | 0 | beam_angle_from_z_axis | degrees | clockwise | vertical axis | -999999 | 0 | 90 | float | ||||
ADCP | BIN_SIZE | 0 | instrument_measurement_volume_bin_size | m | E | -999999 | 0 | 100 | float | |||||
ADCP | RVEL | 0 | radial_velocity_of_scatterers_toward_instrument_in_each_beam | m/s | towards instrument | V | -999999 | -10 | 10 | float | ||||
ADCP | RVEL_FLAGS | 0 | data_flags_for_radial_velocities | |||||||||||
ADCP | RVEL5 | 0 | radial_velocity_of_scatterers_toward_instrument_in_beam_5 | m/s | towards instrument | V | -999999 | -5 | 5 | float | ||||
ADCP | RVEL_DETRENDED | 0 | detrended_radial_velocity_of_scatterers_towards_instrument | m/s | High-frequency content of the velocity signal, which may contain contributions from surface waves, turbulence, and vibrations etc | towards instrument | V | -999999 | -10 | 10 | float | Description of calculation in meta data? | ||
ADCP | R_DEL | 0 | along-beam_separation_distance_over_which_DLL_is_evaluated | m | -999999 | 0 | float | |||||||
ADCP | R_MAX | 0 | maximum_separation_distance_over_for_DLL_regression | m | -999999 | 0 | float | |||||||
ADCP | DLL | 0 | second_order_structure_function | m2/s2 | AlongBeam_distance | -999999 | 0 | float | ||||||
ADCP | DLL_N | 0 | number_of_velocity_difference_samples_in_DLL_mean | count | -999999 | 0 | int | Can be used as QA criterion | ||||||
ADCP | DLL_FLAGS | 0 | data_flags_for_dll | -999999 | float | Can be used as QA criterion for including in regression | ||||||||
ADCP | C2 | 0 | constant_used_in_conversion_of_DLL_regression_coefficient_to_EPSILON | -999999 | float | |||||||||
ADCP | REGRESSION_COUNT | 0 | number_of_DLL_values_used_in_regression | count | -999999 | int | For central-difference scheme, count is the number of del_r evaluate, for forward-difference, there may be multiple instances for each del_r | |||||||
ADCP | REGRESSION_RSQUARED | 0 | regression_goodness_of_fit_adjusted_for_number_of_terms | count | -999999 | float | standard regression uses 2 terms, modified regression uses 3 | |||||||
ADCP/ADV | EPSI_CI_LOW | 0 | low_limit_confidence_interval_for_epsilon | W kg-1 | 95% confidence interval | -999999 | float | |||||||
ADCP/ADV | EPSI_CI_HIGH | 0 | high_limit_confidence_interval_for_epsilon | W kg-1 | 95% confidence interval | -999999 | float | |||||||
ADCP | QAx_BDF | 0 | QA_criterion_x_bad_data_flag | logical | -999999 | 0 | 1 | logical | Details of the QA criterion in meta data? | |||||
ADCP | REGRESSION_COEFF_A0 | 0 | DLL_regression_intercept | m2 s-2 | -999999 | float | Intercept for the DLL regression | |||||||
ADCP | REGRESSION_COEFF_A1 | 0 | DLL_regression_coefficient_for_r^2/3 | m4/3 s-2 | -999999 | float | Coefficient for r^2/3 from either standard or modified DLL regression | |||||||
ADCP | REGRESSION_COEFF_A3 | 0 | DLL_regression_coefficient_for_(r^2/3)^3 | s-2 | -999999 | float | Coefficient for (r^2/3)^3 from modified DLL regression | |||||||
ADCP | REGRESSION_N | |||||||||||||
ADCP | REGRESSION_RSQUARED | |||||||||||||
ADCP | ||||||||||||||
All | L_K | 0 | kolmogorov_length_scale | m | L | -999999 | 0 | 1000 | float | |||||
All | L_S | 0 | turbulent_corssin_shear_length_scale | m | L | -999999 | 0 | 100000 | float | |||||
All | L_O | 0 | turbulent_ozmidov_stratification_length_scale | m | L | -999999 | 0 | 100000 | float |