Cited by 76Astro and Planetary ScienceAtmospheric Ozone and ClimateIonosphere and magnetosphere dynamics

Latitudinal and seasonal models of stratospheric photochemistry on Saturn: Comparison with infrared data from IRTF/TEXES

Moses, J. I., Greathouse, T. K.·2005·Journal of Geophysical Research: Planets

Abstract

The variation of hydrocarbon abundances with altitude, latitude, and season in Saturn's stratosphere is investigated using a one‐dimensional, time‐variable, photochemical model. The results indicate that hydrocarbon abundances at pressures less than ∼0.01 mbar are extremely sensitive to solar flux variations due to changes in season, latitude, orbital radius, solar cycle, and ring shadowing. Long vertical diffusion times in the 0.01–1 mbar region introduce phase lags in the response to insolation changes. At pressures greater than 1 mbar, vertical diffusion timescales are longer than a Saturnian year. Therefore, relatively long‐lived hydrocarbons like C 2 H 2, C 2 H 6, and C 3 H 8 exhibit little seasonal variation in the lower stratosphere, and the yearly averaged solar insolation combined with vertical diffusion control species abundances in this region. Species with short photochemical lifetimes (e.g., CH 3, C 2 H 4) continue to experience seasonal variations, even at low altitudes. The model results are compared with infrared observations from the TEXES spectrometer at NASA's Infrared Telescope Facility. We find that the observed C 2 H 2 mixing‐ratio variation with latitude is reasonably well predicted, whereas the C 2 H 6 distribution is poorly predicted by the models. Meridional transport is likely affecting the distribution of C 2 H 6, which has a long photochemical lifetime, whereas the distribution of shorter‐lived C 2 H 2 is controlled by photochemistry and vertical diffusion. Given the different observed behavior of C 2 H 2 and C 2 H 6, we constrain meridional transport timescales at 2 mbar on Saturn to be in the range ∼100–700 years, corresponding to meridional wind or diffusion speeds of ∼0.4–2 cm s−1.

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Crossref · 10.1029/2005je002450

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  • The primary stratospheric coolants ethane and acetylene are spatially and temporally variable due to photochemistry and atmospheric circulation.

    “In particular, the primary stratospheric coolants (ethane and acetylene) are spatially and temporally variable due to both photochemistry and atmospheric circulation18–24”
  • There is a weak trend with photochemical species longevity: longer-lived ethane and propane show the most similarity between poles (ratios 0.7-1.0), while shorter-lived acetylene, diacetylene and methyl acetylene show greater contrasts (0.2-0.6).

    “There may be a weak trend with the longevity of the photochemical species18, with longer-lived ethane and propane showing the most similarity between the poles (ratios of 0.7–1.0) and the shorter-lived acetylene, diacetylene and methyl acetylene showing greater contrasts (0.2–0.6).”

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Authors
Moses, J. I., & Greathouse, T. K.
Affiliations
Lunar and Planetary Institute (US)
Venue
Journal of Geophysical Research: Planets
Published
2005-09
Volume
110
Issue
E9
ISSN
0148-0227 (ISSN-L)
OpenAlex
W2005523626
Cited by
76
References
1
Citations by year
2025: 1 · 2024: 6 · 2023: 2 · 2022: 2 · 2021: 2 · 2020: 3 · 2019: 2 · 2018: 7 · 2017: 2 · 2016: 3 · 2015: 10 · 2014: 2 · 2013: 4 · 2012: 5
FWCI
2.27
Type
journal article
Language
en
Open access
closed
Locations
Journal of Geophysical Research Atmospheres (publishedVersion)
Topics
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Atmospheric Ozone and Climate
  • Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Ionosphere and magnetosphere dynamics
Keywords
stratospheric photochemistry, hydrocarbon abundances, acetylene, ethane, vertical diffusion, meridional transport, seasonal variation, latitudinal variation, solar irradiation, photochemical lifetime, IRTF

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