Preprints
https://doi.org/10.5194/egusphere-2026-3796
https://doi.org/10.5194/egusphere-2026-3796
07 Jul 2026
 | 07 Jul 2026
Status: this preprint is open for discussion and under review for Atmospheric Measurement Techniques (AMT).

Estimates of Tropospheric Ozone from Nimbus 7 LIMS and TOMS Datasets

Ellis Remsberg

Abstract. This work is a diagnostic study of distributions of tropical tropospheric column ozone (TRCO) based on subtracting Limb Infrared Monitor of the Stratosphere (LIMS) Version 6 (V6) Level 3 stratospheric column ozone (SCO) values from Total Ozone Mapping Spectrometer (TOMS) total ozone for several selected days of 1978–1979. The focus of this study is the low latitudes, where the tropopause is near 100 hPa and zonal wave activity is weak. TRCO exhibits a zonal wave-1 feature in the southern tropics with maximum values near 0° longitude during November 1978. Its zonal variation is 70 to 30 Dobson units (DU) and agrees with that of other similar analysis studies. V6 estimates of SCO and calculated TRCO are less reliable in March and May 1979 because those data are affected by temperature biases of order -1.0 to -2.0 K at 30 and 50 hPa; retrieved ozone at those levels may be too large by ~20 % as a result. The LIMS Level 3 sequential estimation algorithm provides smoothed zonal wave ozone amplitudes and reduced zonal variations of SCO. The corresponding calculated TRCO amplitudes are enhanced and not quantitative in those instances. The findings herein should be helpful to others, as they analyze infrared limb measurements of ozone and subtract their stratospheric column amounts from coincident total ozone to obtain accurate zonal variations of tropospheric ozone.

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Ellis Remsberg

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Ellis Remsberg
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Short summary
This study considers several sample days of tropospheric column ozone (TRCO) obtained by subtracting LIMS stratosphere column ozone (SCO) from TOMS total ozone. TRCO is elevated in the southern hemisphere tropics near west Africa during November 1978. Conversely, there are small biases in the LIMS ozone of the lower stratosphere that affect the accuracy of its SCO values in March and in May 1979; calculated zonal variations of TRCO are spurious on those days.
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