25.01.2015 Views

IASPEI - Picture Gallery

IASPEI - Picture Gallery

IASPEI - Picture Gallery

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

IUGG XXIV General Assembly July 2-13, 2007 Perugia, Italy<br />

(S) - <strong>IASPEI</strong> - International Association of Seismology and Physics of the Earth's<br />

Interior<br />

JSS011 Oral Presentation 2110<br />

Short wavelength topography on the inner core boundary<br />

Prof. Barbara Romanowicz<br />

Berkeley Seismological Laboratory University of California at Berkeley <strong>IASPEI</strong><br />

Aimin Cao, Yder Masson<br />

Constraining the topography of the ICB is important for studies of core-mantle coupling and the<br />

generation of the geodynamo. We present evidence for significant temporal variability in the amplitude<br />

of the inner core reflected phase PKiKP for an exceptionally high quality earthquake doublet, which<br />

occurred in the South Sandwich Islands within a ten year interval (1993/2003) and was observed at the<br />

short period Yellowknife seismic array (YK). While individual waveforms of the PP phase and its coda<br />

are highly similar for the doublet in a relatively wide frequency range of 0.5 to 2 Hz, the PKiKP<br />

amplitude for the 2003 event is 7.2 times larger than that for the 1993 event, and the corresponding<br />

amplitude ratio of PKiKP/PKIKP for the 2003 event is 3.1 times larger than that for the 1993 event in the<br />

frequency range of 1 to 2 Hz. We show that the PKiKP for the 2003 event is normal and the PKiKP for<br />

the 1993 is anomalous, most likely due to defocusing at the ICB. From the size of the amplitude<br />

anomaly, which is not accompanied by a significant travel time anomaly, we infer that this observation,<br />

complemented by data from several other doublets, indicates the presence of topography at the innercore<br />

boundary, with a horizontal wavelength on the order of 10 km. Such topography could be<br />

sustained by small scale convection at the top of the inner core, and is compatible with a rate of superotation<br />

of the inner core of _0.1-0.15 deg/year. Alternatively, if the inner core is not rotating, decadal<br />

scale temporal changes in the ICB topography would provide an upper bound on the viscosity at the top<br />

of the inner core of about 10^16 Pas.<br />

Keywords: inner core, topography, structure

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!