Inactivation times from 290 to 315 nm UVB in sunlight for SARS coronaviruses CoV and CoV-2 using OMI satellite data for the sunlit Earth

Jay Herman,Bryan Biegel,Liang Huang

doi:10.1007/s11869-020-00927-2

Jay Herman, Bryan Biegel + Show 1 more

Open Access

https://doi.org/10.1007/s11869-020-00927-2

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Abstract

UVB in sunlight, 290–315 nm, can inactivate SARS CoV and SARS CoV-2 viruses on surfaces and in the air. Laboratory exposure to ultraviolet irradiance in the UVC range inactivates many viruses and bacteria in times less than 30 min. Estimated UVB inactivation doses from sunlight in J/m2 are obtained from UVC measurements and radiative transfer calculations, weighted by a virus inactivation action spectrum, using OMI satellite atmospheric data for ozone, clouds, and aerosols. For SARS CoV, using an assumed UVC dose near the mid-range of measured values, D90 = 40 J/m2, 90% inactivation times T90 are estimated for exposure to midday 10:00–14:00 direct plus diffuse sunlight and for nearby locations in the shade (diffuse UVB only). For the assumed D90 = 40 J/m2 model applicable to SARS CoV viruses, calculated estimates show that near noon 11:00–13:00 clear-sky direct sunlight gives values of T90 < 90 min for mid-latitude sites between March and September and less than 60 min for many equatorial sites for 12 months of the year. Recent direct measurements of UVB sunlight inactivation of the SARS CoV-2 virus that causes COVID-19 show shorter T90 inactivation times less than 10 min depending on latitude, season, and hour. The equivalent UVC 254 nm D90 dose for SARS CoV-2 is estimated as 3.2 ± 0.7 J/m2 for viruses on a steel mesh surface and 6.5 ± 1.4 J/m2 for viruses in a growth medium. For SARS CoV-2 clear-sky T90 on a surface ranges from 4 min in the equatorial zone to less than 30 min in a geographic area forming a near circle with solar zenith angle < 60O centered on the subsolar point for local solar times from 09:00 to 15:00 h.

Highlights

For estimating day-to-day inactivation times, the exact T90 numbers for SARS CoV-2 virus are unimportant on any given day because of the larger T90 variability caused by significant atmospheric transmission changes even on days that appear relatively clear of clouds and aerosols
A study of coronavirus inactivation times by UV solar irradiation is presented for two classes of experimental laboratory data
Are those measurements made at 254 nm and extrapolated to wavelength longer than 290 nm using an action spectrum A(λ) (Lytle and Sagripanti 2005), and second, are the measurements made in simulated sunlight (RatnesarShumate et al 2020) that do not require the use of an action spectrum

Summary

Introduction

The method used here relies on finding a value of 254 nm D90 that yields approximately the same inactivation time, 6.8 min, as RS finds for midday during the summer solstice at 40O N latitude using the same TUV radiative transfer code. The value D90 = 3.2 J/m2 is approximately 12.5 times smaller than the UVC D90 = 40 J/m2 for the SARS CoV virus used in the previous sections leading to T90 of about 4 min at the equator and about 5 min at 40O N during the summer solstice (Fig. 15b). For estimating day-to-day inactivation times, the exact T90 numbers for SARS CoV-2 virus are unimportant on any given day because of the larger T90 variability caused by significant atmospheric transmission changes even on days that appear relatively clear of clouds and aerosols. Note that these are annual minimum T90 that includes both summer solstices in their respective hemispheres giving rise to two minima

Summary and discussion

Findings

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