Abstract

AbstractThe spatial distribution of water, ammonia, phosphine, germane, and arsine in the Jupiter's troposphere has been inferred from the Jovian Infrared Auroral Mapper (JIRAM) Juno data. Measurements allow us to retrieve the vertically averaged concentration of gases between ~3 and 5 bars from infrared‐bright spectra. Results were used to create latitudinal profiles. The water vapor relative humidity varies with latitude from <1% to over 15%. At intermediate latitudes (30–70°) the water vapor maxima are associated with the location of cyclonic belts, as inferred from mean zonal wind profiles (Porco et al., 2003). The high‐latitude regions (beyond 60°) are drier in the north (mean relative humidity around 2–3%) than the south, where humidity reaches 15% around the pole. The ammonia volume mixing ratio varies from 1 × 10−4 to 4 × 10−4. A marked minimum exists around 10°N, while data suggest an increase over the equator. The high‐latitude regions are different in the two hemispheres, with a gradual increase in the south and more constant values with latitude in the north. The phosphine volume mixing ratio varies from 4 × 10−7 to 10 × 10−7. A marked minimum exists in the North Equatorial Belt. For latitudes poleward 30°S and 30°N, the northern hemisphere appears richer in phosphine, with a decrease toward the pole, while the opposite is observed in the south. JIRAM data indicate an increase of germane volume mixing ratio from 2 × 10−10 to 8 × 10−10 from both poles to 15°S, with a depletion centered around the equator. Arsine presents the opposite trend, with maximum values of 6 × 10−10 at the two poles and minima below 1 × 10−10 around 20°S.

Highlights

  • The energy transfer in planetary atmospheres of the Solar System at the pressure level of few bars is dominated by convection and air temperature variations with pressure follow an adiabatic profile [Robinson and Catling, 2013]

  • Their mean values between 40°S and 10°S and 25°N and 40°N are in excellent agreement with our findings (2.5×10-4). This is in contrast with the results presented in Giles et al,. [2017b] from CRIRES-VLT data in the 5.1525.188 μm spectral range at a spectral resolving power of 96,000. These authors presented a latitudinal profile at 3.3 bar where, in North and South Equatorial belts, the ammonia mixing ratio is typically twice what we find, and falls below 1×10-4 in the most opaque latitudes

  • The analysis of Jovian Infrared Auroral Mapper (JIRAM) 5-μm data presented in this paper supports the view of significant horizontal variations in the mixing ratios of minor gases in the troposphere of Jupiter at the level of few bars

Read more

Summary

Introduction

The energy transfer in planetary atmospheres of the Solar System at the pressure level of few bars is dominated by convection and air temperature variations with pressure follow an adiabatic profile [Robinson and Catling, 2013]. In the 0.3-0.6 bar range, for a large variety of conditions, optically thick planetary atmospheres become transparent in the thermal infrared region, so that energy transport is by radiative rather than convective processes [e.g.: Wallance and Hobbs, 2006] If this convective-radiative boundary is overlaid by atmospheric regions where opacity at short wavelengths (notably ultraviolet) is much higher than in the infrared, absorption of solar photons causes a local heating of the atmosphere and a rise of air temperature while moving upward. Several other non-condensable species (phosphine, germane, arsine, carbon monoxide) are in thermochemical disequilibrium at the pressure and temperature conditions of the troposphere where they are detected. Their presence at these levels is usually interpreted as evidence of strong convection from deep atmosphere where those species are in thermochemical equilibrium. The O/H ratio is an important consideration in Jupiter's formation models, but difficult to derive directly by IR spectroscopy due to the condensation of water vapor

Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call