Claimed detection of PH$_3$ in the clouds of Venus is consistent with mesospheric SO$_2$
Andrew P. Lincowski, Victoria S. Meadows, David Crisp, Alex B. Akins,, Edward W. Schwieterman, Giada N. Arney, Michael L. Wong, Paul G. Steffes, M., Niki Parenteau, Shawn Domagal-Goldman

TL;DR
The paper challenges previous claims of PH$_3$ detection in Venus clouds, showing the spectral feature is more likely due to mesospheric SO$_2$, based on radiative transfer modeling and vertical distribution analysis.
Contribution
It demonstrates that the 266.94 GHz spectral feature is caused by mesospheric SO$_2$ rather than PH$_3$, clarifying Venus's atmospheric composition.
Findings
The spectral line originates above 80 km in Venus's mesosphere.
Typical SO$_2$ distributions explain the observed spectral feature.
PH$_3$ presence would require an implausibly high source flux.
Abstract
The observation of a 266.94 GHz feature in the Venus spectrum has been attributed to PH in the Venus clouds, suggesting unexpected geological, chemical or even biological processes. Since both PH and SO are spectrally active near 266.94 GHz, the contribution to this line from SO must be determined before it can be attributed, in whole or part, to PH. An undetected SO reference line, interpreted as an unexpectedly low SO abundance, suggested that the 266.94 GHz feature could be attributed primarily to PH. However, the low SO and the inference that PH was in the cloud deck posed an apparent contradiction. Here we use a radiative transfer model to analyze the PH discovery, and explore the detectability of different vertical distributions of PH and SO. We find that the 266.94 GHz line does not originate in the clouds, but above 80 km in…
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