OMI_L2_OMAERUV

Variables

The table below lists the variables that are present in the HARP product that results from an ingestion of OMI_L2_OMAERUV data.

field name	type	dimensions	unit	description
datetime	double	{time}	[seconds since 2000-01-01]	time of the measurement
longitude	double	{time}	[degree_east]	longitude of the ground pixel center (WGS84)
latitude	double	{time}	[degree_north]	latitude of the ground pixel center (WGS84)
longitude_bounds	double	{time, 4}	[degree_east]	longitudes of the ground pixel corners (WGS84)
latitude_bounds	double	{time, 4}	[degree_north]	latitudes of the ground pixel corners (WGS84)
surface_pressure	double	{time}	[hPa]	terrain pressure
wavelength	double	{spectral}	[nm]	wavelength
aerosol_optical_depth	double	{time, spectral}	[]	aerosol optical depth
aerosol_absorbing_optical_depth	double	{time, spectral}	[]	aerosol absorbing optical depth
uv_aerosol_index	double	{time}	[]	UV aerosol index
index	int32	{time}		zero-based index of the sample within the source product

Mapping description

The shape and size of each ground pixel is not included in the product. HARP therefore provides its own approximation which is based on interpolation of the available center coordinates for each of the ground pixels. Each corner coordinate is determined by its four surrounding center coordinates. The corner coordinate is exactly at the intersection of the cross that can be made with these four points (each line of the cross is the great-circle distance from one center coordinate to the other). In situations where a corner coordinate is not surrounded by four center coordinates (i.e. at the boundaries) virtual center coordinates are created by means of extrapolation. The virtual center coordinate is placed such that the distance to its nearest real center coordinate equals the distance between that nearest real center coordinate and the next center coordinate going further inwards. In mathematical notation: when c(i,m+1) is the virtual center coordinate and c(i,m) and c(i,m-1) are real center coordinates, then ||c(i,m+1) - c(i,m)|| = ||c(i,m) - c(i,m-1)|| and all three coordinates should lie on the same great circle. The four virtual coordinates that lie in the utmost corners of the boundaries are calculated by extrapolating in a diagonal direction (e.g. c(n+1,m+1) is calculated from c(n,m) and c(n-1,m-1)).

The table below details where and how each variable was retrieved from the input product.

field name	mapping description
datetime	path	/HDFEOS/SWATHS/Aerosol_NearUV_Swath/Geolocation_Fields/Time[]
	description	the time of the measurement converted from TAI93 to seconds since 2000-01-01T00:00:00
longitude	path	/HDFEOS/SWATHS/Aerosol_NearUV_Swath/Geolocation_Fields/Longitude[]
latitude	path	/HDFEOS/SWATHS/Aerosol_NearUV_Swath/Geolocation_Fields/Latitude[]
longitude_bounds	description	interpolated from the available center coordinates for each of the ground pixels
latitude_bounds	description	interpolated from the available center coordinates for each of the ground pixels
surface_pressure	path	/HDFEOS/SWATHS/ColumnAmountO3/Geolocation_Fields/TerrainPressure[]
wavelength	description	three fixed wavelengths (354, 388, and 500 nm) as defined by the OMI OMAERUV product specification
aerosol_optical_depth	path	/HDFEOS/SWATHS/Aerosol_NearUV_Swath/Data_Fields/FinalAerosolOpticalDepth[]
aerosol_absorbing_optical_depth	path	/HDFEOS/SWATHS/Aerosol_NearUV_Swath/Data_Fields/FinalAerosolAbsOpticalDepth[]
uv_aerosol_index	path	/HDFEOS/SWATHS/Aerosol_NearUV_Swath/Data_Fields/UVAerosolIndex[]