GP12A:
PL-O Coupling: Connecting Planetary Lithospheres to Outer Cores
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GP12A:
PL-O Coupling: Connecting Planetary Lithospheres to Outer Cores
PL-O Coupling: Connecting Planetary Lithospheres to Outer Cores
You can still search the program to see your colleague�s abstract submissions as well as the sessions submitted for the 2016 Fall Meeting. The final program will be released in early October.
Please note: this session is being considered for an alternate session format. Please be aware that if your abstracted is accepted in this session, your abstract may be scheduled as a panel discussion or lightning poster presentation. For more information please visit the following link: http://fallmeeting.agu.org/2016/alternate-session-formats/.
Session ID#: 15745
Session Description:
Planetary interiors are connected systems. Earth's inner core solidifies under conditions controlled by the outer core and overlying mantle. Thermal disequilibrium between mantle and core drive deep mantle instabilities, which affect magnetic field generation in the core. Experimental, theoretical and numerical approaches are complementary to understanding the dynamics of deep planetary interiors. Recent advances in these fields are this session’s focus.
Other planets display a variety of internal dynamics. Lithospheric rheology and tectonics are critical for cooling the deep interior and driving planetary magnetic fields. Synthesis of observations with theory relating to the coupled behaviors of whole planet systems is an end goal of deep interior geophysics. Outer cores that maintain magnetic dynamos offer a natural laboratory for such theories. Naturally we seek contributions that broadly connect the properties and dynamics of different parts of Earth and planetary interiors.
Oral presentations in this session may be 7-minute lightning talks.
Primary Convener: Jonathan M Aurnou, University of California Los Angeles, Department of Earth, Planetary, and Space Sciences, Los Angeles, United States
Conveners: Jonathan M Aurnou, University of California Los Angeles, Department of Earth, Planetary, and Space Sciences, Los Angeles, United States, Peter E Driscoll, Carnegie Science, Earth & Planets Lab, Washington, United States and Moritz H Heimpel, University of Alberta, Department of Physics, Edmonton, AB, Canada
Chairs: Moritz H Heimpel, University of Alberta, Department of Physics, Edmonton, AB, Canada, Peter E Driscoll, Carnegie Science, Earth & Planets Lab, Washington, United States and Jonathan M Aurnou, University of California Los Angeles, Department of Earth, Planetary, and Space Sciences, Los Angeles, United States
OSPA Liaison: Peter E Driscoll, Carnegie Science, Earth & Planets Lab, Washington, United States
Cross-Listed:
- DI - Study of the Earth's Deep Interior
- P - Planetary Sciences
- T - Tectonophysics
Index Terms:
1510 Dynamo: theories and simulations [GEOMAGNETISM AND PALEOMAGNETISM]
5430 Interiors [PLANETARY SCIENCES: SOLID SURFACE PLANETS]
8120 Dynamics of lithosphere and mantle: general [TECTONOPHYSICS]
8121 Dynamics: convection currents, and mantle plumes [TECTONOPHYSICS]
Abstracts Submitted to this Session:
Constraining mantle convection models with paleomagnetic reversals record and numerical dynamos (133843)
Examples of Viscosity-Free Dynamos (147112)
Subcritical thermal convection of liquid metals in a rotating sphere using a quasi-geostrophic model (143801)
See more of: Geomagnetism, Paleomagnetism and Electromagnetism
