stratospheric circulation of jupiter
DESCRIPTION
Stratospheric Circulation of Jupiter. Xi Zhang 1,2 R. L. Shia 2 , A. P. Showman 1 , and Y. L. Yung 2 1 LPL, University o f Arizona, United States 2 California Institute of Technology, United States Supported by Bisgrove Postdoctoral Scholar Fellowship Apr 11, 2013, Wien. Outline. - PowerPoint PPT PresentationTRANSCRIPT
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Stratospheric Circulation of Jupiter
Xi Zhang1,2
R. L. Shia2, A. P. Showman1, and Y. L. Yung2
1LPL, University of Arizona, United States2California Institute of Technology, United States
Supported by Bisgrove Postdoctoral Scholar Fellowship
Apr 11, 2013, Wien
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Outline• Introduction • Derive the stratospheric circulation
based on Cassini and Voyager data• Problem and possible solutions
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Based on Sieff et al. (1998)
?
Brower (1949), Dobson (1956), Figures from Seinfeld and Pandis (2006)
Jovian Stratosphere
Residual mean meridional circulation/Horizontal eddy mixing
Earth
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How to derive the circulation pattern?
• Dynamical Simulation (requires wave properties)
• Diagnostic Approach (based on diabatic heating rate map)
Conrath et al. (1990); West et al. (1992); Moreno and Sedeno (1997)
• Tracer Approach (based on tracer distributions and 2-D chemical transport model)
Friedson et al. (1999); Liang et al. (2005); Lellouch et al. (2006)
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Diagnostic Approach
Conrath et al. (1990)
West et al. (1992)
Radiatively Driven Mechanically Driven
Without Aerosol Heating With Aerosol Heating
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Tracer Approach
Liang et al. (2005) Lellouch et al. (2006)
• Diffusional transport dominates, based on SL-9 dust data (Friedson et al., 1999) and C2H2 and C2H6 data (Liang et al., 2005)
• Horizontal advection is not negligible, based on SL-9 HCN and CO2 data (Lellouch et al., 2006)
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This Study
Zhang et al. (2013a)
• Temperature and tracer maps from Cassini CIRS + Voyager IRIS spectra (Zhang et al., 2013a)• Global stratospheric aerosol map from Cassini ISS data (Zhang et al., 2013b)• Revisit both approaches
Zhang et al. (2013b)
~10 nm
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Diagnostic ApproachWithout Aerosol Heating With Aerosol Heating
West et al. (1992)
This study:
Aerosol heating effect is significant
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Tracer Approach• State-of-art Caltech/JPL 2-D chemical transport model, validated against analytical solutions (Zhang et al., 2013c)
• Residual circulation pattern derived, advection is not negligible.
Observation
Model with
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Two patterns are not consistent
Diagnostic Approach Tracer Approach
• Uncertainties in the radiative diabatic heating rate ?• Atmosphere not in steady state?• Possible missing chemistry?
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Test possible polar ethane source• Assume there is a strong ethane source (10 times
larger than the photochemical source) from ion-chemistry in the aurora region
Observation
Model with horizontal mixing
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Summary• Residual mean meridional circulation pattern(s)
derived based on: (1) radiative diabatic heating rate map (2) tracer distributions and chemical transport model• Two patterns are not consistent • Possible solutions are discussed
Diagnostic Approach Tracer Approach