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Labow GJ, Flynn LE, Rawlins MA, et al. Estimation of ozone with total ozone portable spectroradiometer instruments. II. Practical operation and comparisons. Appl Opt. 1996;35(30):6084-9doi: 10.1364/AO.35.006084.
Labow, G. J., Flynn, L. E., Rawlins, M. A., Beach, R. A., Simmons, C. A., & Schubert, C. M. (1996). Estimation of ozone with total ozone portable spectroradiometer instruments. II. Practical operation and comparisons. Applied optics, 35(30), 6084-9. https://doi.org/10.1364/AO.35.006084
Labow, G J, et al. "Estimation of ozone with total ozone portable spectroradiometer instruments. II. Practical operation and comparisons." Applied optics vol. 35,30 (1996): 6084-9. doi: https://doi.org/10.1364/AO.35.006084
Labow GJ, Flynn LE, Rawlins MA, Beach RA, Simmons CA, Schubert CM. Estimation of ozone with total ozone portable spectroradiometer instruments. II. Practical operation and comparisons. Appl Opt. 1996 Oct 20;35(30):6084-9. doi: 10.1364/AO.35.006084. PMID: 21127624.
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Appl Opt. 1996 Oct 20;35(30):6084-9. doi: 10.1364/AO.35.006084.

Estimation of ozone with total ozone portable spectroradiometer instruments. II. Practical operation and comparisons.

Applied optics

G J Labow, L E Flynn, M A Rawlins, R A Beach, C A Simmons, C M Schubert

PMID: 21127624 DOI: 10.1364/AO.35.006084

Abstract

We used a microcomputer-controlled total ozone portable spectroradiometer instrument #21 (MTOPS21) to measure solar radiation at 298, 304 and 310 nm in Greenbelt, Md., during 1995. One day's ozone measurements from a Brewer instrument (B105) were used to calibrate the 304- and 310-nm channel ratios to a theoretical model. Total ozone estimates were then determined for the entire MTOPS21 data set. Differences between individual B105 and MTOPS21 ozone estimates show a 1% drop as solar zenith angles increase and depend on atmospheric attenuation and SO(2) variation at the ±2% level. Daily average values agree well (<0.5% average offset, 2% standard deviation).

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