HR: 0800h
AN: G51C-0102 [Abstracts]
TI: Spatiospectral concentration and spectral analysis of potential fields on the sphere
AU: Wieczorek, M A
EM: wieczor@ipgp.jussieu.fr
AF: D{\'e}partement de G{\'e}ophysique Spatiale et Plan{\'e}taire, Institut de Physique du Globe de
Paris, St. Maur, 94701
France
AU: * Simons, F J
EM: fjsimons@alum.mit.edu
AF: D{\'e}partement de G{\'e}ophysique Spatiale et Plan{\'e}taire, Institut de Physique du Globe de
Paris, St. Maur, 94701
France
AU: * Simons, F J
EM: fjsimons@alum.mit.edu
AF: Princeton University, Department of Geosciences, Guyot Hall, Princeton, NJ 08544
United States
AU: Dahlen, F A
EM: fad@princeton.edu
AF: Princeton University, Department of Geosciences, Guyot Hall, Princeton, NJ 08544
United States
AB:
Physical properties, such as the elastic strength or the magnetization depth of a planetary lithosphere can be estimated from
the cross-spectral properties of potential fields. Such data are most commonly available as bandlimited spherical harmonic
coefficients, measured by artificial satellites or spacecraft. In many if not most applications, planetary curvature
prohibits the use of locally flat approximations. Thus, the determination of spatially localized estimates of planetary
properties requires spatiospectral localization methods that go beyond those available in the plane. Single spherical
windows or tapers have been developed and applied in a number of recent studies; however, these are neither optimally
concentrated, nor as reliable as an orthogonal family of multitapers in the extraction of robust localized statistical
information from bandlimited spherical data.
Here, we pose and solve the analogue of Slepian's time-frequency concentration problem on the surface of the unit sphere to
determine an orthogonal family of strictly bandlimited functions that are optimally concentrated within a closed region of
the sphere, or, alternatively, of strictly spacelimited functions that are optimally concentrated within the spherical
harmonic domain. Such a basis of simultaneously spatially and spectrally concentrated functions should
be a useful data analysis and representation tool in a variety of geophysical and planetary applications, as well as in
medical imaging, computer science, cosmology and numerical analysis. The spherical Slepian functions can be found either by
solving an algebraic eigenvalue problem in the spectral domain or by solving a Fredholm integral equation in the spatial
domain. The associated eigenvalues are a measure of the spatiospectral concentration. When the concentration region is an
axisymmetric polar cap the spatiospectral projection operator commutes with a Sturm-Liouville
operator; this enables the eigenfunctions to be computed extremely accurately and efficiently, even when their area-bandwidth
product, or Shannon number, is large. In the asymptotic limit of a small concentration region and a large spherical harmonic
bandwidth the spherical concentration problem approaches its planar equivalent, which exhibits self-similarity when the
Shannon number is kept invariant.
Our examples show families of bandlimited spherical harmonic expansions that are localized to Earth's continents. In a
related presentation, we investigate the ability of our orthogonal data tapers to obtain spectral estimates by analyzing the
bias and variance properties of the multitaper estimator constructed using our windows.
UR: http://www.frederik.net
DE: 4259 Ocean acoustics
DE: 4294 Instruments and techniques
SC: Geodesy [G]
MN: 2004 AGU Fall Meeting