Catherine Louise Johnson
Professor
Planetary geophysics
Office: EOS-South 363 Phone: 604-827-3480
E-mail:
Personal Website: http://www.eos.ubc.ca/~cjohnson/
MESSENGER Mission Updates (in reverse chronological order)
I. Mercury
I am a Participating Scientist on the MESSENGER mission to Mercury and am a member ofr the Geophysics and Atmosphere & Magnetopshere science teams. On March 18 00:45 UTC (March 17, 5:45pm PDT) NASA's MESSENGER spacecraft successfully went into orbit around the innermost planet, after over 6 years of travel. MESSENGER Mission Web Page. Collaborators:
II. Lunar Geophysics
Lunar Seismicity: Understanding both the origin of lunar quakes observed in the Apollo Passive Seismic Experiment data, and in what these quakes tell us about the internal structure of the Moon. Collaborators:
Lunar Magnetism: Determining if and when the moon might have had a core dynamo. In particular I am interested in understanding the origin of strong mangetizations measured in some Apollo samples (notably in samples with ages in the 3.9 - 3.6 Ga range), and the origin of crustal magnetic anomalies observed globally by the Lunar Prospector Magnetometer and Electron Reflectometer. Collaborators:
Impact Craters: Characterizing the topography of complex craters using new high resolution altimetry data returned by the Lunar Reconnaissance Orbiter Prospector Mission. Collaborators:
IV: Evolution of Mars' Magnetic Field and Atmosphere
Understanding how long Mars could have retained an early atmosphere either with or without the presence of a global magnetic field. Collaborators:
V: Long-term Geomagnetic Field Behavior
A long-standing question in geomagnetism has been whether spatial variations in the physical and chemical properties of the lowermost mantle affect outer core dynamics in a way that has an observable surface expression. For example, there has been ongoing debate as to whether the magnetic field in the Pacific region is anomalous since the paleomagnetic work of Allan Cox and colleagues in the 1970s. My research in this area includes field work, laboratory measurements, data assimilation from the literature, and the development and application inversion techniques and statistical approaches to model the time-averaged field and its temporal variations. Collaborators:
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