Meredith is also a co-PI of the Global CMT project, working to support and improve the routine analysis of moderate and large earthquakes worldwide.
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Meredith's research focuses on
tomographic imaging of the Earth's upper mantle and studies
of the earthquake source. Tomographic work includes the development of
a robust and well-constrained model of the radially anisotropic, 3-D
shear velocity structure of the upper mantle beneath North America.
Current earthquake studies include an effort to constrain the source
characteristics of glacial earthquakes and the processes that lead
to those earthquakes. In addition, Meredith has a nascent interest in
glaciology, and spends a large fraction of her time working on a major
interdisciplinary geophysical observing campaign at Helheim Glacier, in
East Greenland (see "Glacial Earthquakes", below).
Meredith is also a co-PI of the Global CMT project, working to support and improve the routine analysis of moderate and large earthquakes worldwide. |
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Glacial Earthquakes |
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Centroid Moment Tensor Project |
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Surface Wave Tomography |
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Unusual Earthquakes |