Planetary Atmospheres
Cover Page/Proposal Summary
ROSS-00 NRA 00-OSS-01
Date Due: 4/28/2000
This proposal shall be used and disclosed for evaluation purposes only, and a copy of this Government notice shall be applied to any reproduction or abstract thereof. Any authorized restrictive notices that the submitter places on this proposal shall also be strictly complied with. Disclosure of this proposal for any reason outside the Government evaluation purposes shall be made only to the extent authorized by the Government. |
Proposal Type: New Proposal |
Proposal Category: Dynamics |
Major Equipment Proposal? No |
Do you intend to submit an Education/Public Outreach (E/PO) proposal? No |
Proposal Title: |
Convection in Outer Planet Atmospheres: The Interaction of Convectionwith Radiative Transfer |
Abbreviated Proposal Title: |
Convection in Outer Planet Atmospheres |
Principal Investigator: |
Dr. Andrew Friedson Earth and Space Sciences MS 169-237 Jet Propulsion Laboratory 4800 Oak Grove Drive Pasadena, CA 91109-8099 Phone: 818-354-2397 Fax: 818-393-4619 E-mail: Andrew.J.Friedson@jpl.nasa.gov |
Signature | Date |
_____________________________________ | ____________ |
Co-Investigators and Collaborators: | |||
Type | Name | Affiliation | |
Sci Co-I | Dr. Ping Wang | JPL | Ping.Wang@jpl.nasa.gov |
Sci Collab | Dr. Glenn S. Orton | JPL | Glenn.Orton@jpl.nasa.gov |
Proposal Summary:
We propose to explore the nature of thermal convection in Jupiter and its role in establishing the differential rotation of the atmosphere and interior. Our primary aim is to examine whether turbulent convection in relatively thin layers engenders two-dimensional turbulent behavior similar to that observed in Jupiter's atmosphere. Specifically, we will determine how the nature of the convection, and its associated heat and angular momentum transport, is influenced by (i) the total depth of the convection zone (or zones), (ii) the presence of a 2000-K radiative zone, and (iii) radiative driving that is induced by the latitudinal insolation gradient when a 2000-K radiative zone is present. Numerical simulations exploring these effects will be performed by solving the 3-D anelastic equations of motion in spherical shells. The convection zones studied will be thinner than those of previous studies of Jovian convection in order to be consistent with the latest models of Jupiter's internal structure. Our simulations will be the first to explore the influence of a deep radiative zone on the convection and the dynamical response of the system to the lateral radiative drive induced by the insolation gradient and deep radiative zone. The calculations will be performed on a high-speed massively parallel supercomputer capable of meeting the computational demands imposed by the high spatial and temporal resolution required to model the flow at very high Rayleigh and Taylor numbers.
Certification of Compliance with Applicable Executive Orders and U.S. Code
By submitting the proposal identified in this Cover Sheet/Proposal Summary in response to this NRA or AO, the Authorizing Official of the proposing institution (or the individual proposer if there is no proposing institution) as identified below:
Willful provision of false information in this proposal and/or its supporting documents, or in reports required under an ensuing award, is a criminal offense (U.S. Code, Title 18, Section 1001).