Abstract
Abstract. A version 2 processing of data from two ozone monitoring instruments on Suomi NPP, the OMPS nadir ozone mapper and the OMPS nadir ozone profiler, has now been completed. The previously released data were useful for many purposes but were not suitable for use in ozone trend analysis. In this processing, instrument artifacts have been identified and corrected, an improved scattered light correction and wavelength registration have been applied, and soft calibration techniques were implemented to produce a calibration consistent with data from the series of SBUV/2 instruments. The result is a high-quality ozone time series suitable for trend analysis. Total column ozone data from the OMPS nadir mapper now agree with data from the SBUV/2 instrument on NOAA 19 with a zonal average bias of −0.2 % over the 60∘ S to 60∘ N latitude zone. Differences are somewhat larger between OMPS nadir profiler and N19 total column ozone, with an average difference of −1.1 % over the 60∘ S to 60∘ N latitude zone and a residual seasonal variation of about 2 % at latitudes higher than about 50∘. For the profile retrieval, zonal average ozone in the upper stratosphere (between 2.5 and 4 hPa) agrees with that from NOAA 19 within ±3 % and an average bias of −1.1 %. In the lower stratosphere (between 25 and 40 hPa) agreement is within ±3 % with an average bias of +1.1 %. Tropospheric ozone produced by subtracting stratospheric ozone measured by the OMPS limb profiler from total column ozone measured by the nadir mapper is consistent with tropospheric ozone produced by subtracting stratospheric ozone from MLS from total ozone from the OMI instrument on Aura. The agreement of tropospheric ozone is within 10 % in most locations.
Highlights
NASA has been measuring ozone from space since the launch of the Backscatter Ultraviolet (BUV) instrument on Nimbus 4 in 1970
While some comparisons with data from the limb profiler will be shown in this paper, detailed LP validation results will be discussed in other papers
The goal of the version 2 processing is to produce ozone data sufficiently accurate to be used to continue the Merged Ozone Data (MOD) time series. This time series is a unified multi-instrument ozone data set created by merging data from a series of SBUV and SBUV/2 instruments beginning with the original BUV instrument launched on Nimbus 4 in 1970 and extending to the SBUV/2 instrument on NOAA 19, which continues to operate
Summary
NASA has been measuring ozone from space since the launch of the Backscatter Ultraviolet (BUV) instrument on Nimbus 4 in 1970. The series of follow-on instruments, SBUV (Solar Backscatter Ultraviolet) and TOMS (Total Ozone Mapping Spectrometer) on Nimbus 7 and SBUV/2 instruments on NOAA 9, 11, 14, 16, 17, 18, and 19 produced a long-term time series of global ozone observations. Ozone instruments on the Suomi NPP spacecraft and the planned series of JPSS (Joint Polar Satellite System) spacecraft will be used to continue this series of measurements in order to document long-term ozone change. R. McPeters et al.: Trend quality ozone from NPP OMPS: the version 2 processing (LP), an instrument that measures the ozone vertical distribution using light scattered from the Earth’s limb. The purpose of the version 2 processing of data from the two OMPS nadir sensors, which is the subject of this paper, is to correct various instrument artifacts and to apply an updated calibration that will be consistent with data from earlier instruments. While some comparisons with data from the limb profiler will be shown in this paper, detailed LP validation results will be discussed in other papers
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