Interpreting cross-correlations in seismology

Research output: Chapter in Book/Report/Conference proceedingChapter

Abstract

Introduction Wavefields in the Sun and Earth, measured using various instruments, display small- amplitude fluctuations, essentially zero-mean random processes. More careful investigation reveals that these are seismic fluctuations generated by stochastic processes such as convection in the Sun and by anthropogenic activity and non-linear ocean wave interactions on Earth. The distinguishing feature of imaging with noise is that we do not know the dynamical details of the source (unlike in classical earthquake tomography) and we consequently seek a statistical description of the wavefield. Here, we discuss the interpretation of the cross-correlation measurement in solar and terrestrial scenarios. The most common measurement in the context of noise is the ensemble- averaged cross-correlation. The physics of such measurements can be markedly different from raw wavefield measurements (as in classical tomography). The helioseismic theory of stochastic oscillations in conjunction with computational adjoint optimization, widely used in terrestrial seismic applications, provides a unified framework for addressing outstanding inverse problems in these areas. The seismic methodologies and challenges in each of these fields, despite the vastly different physics, are intimately related and we highlight these similarities in this article. Seismology of the Sun The Sun, our nearest star, serves as an astrophysical benchmark, contributing to our understanding of stellar evolution, stellar interiors and atmospheres, etc. Life on Earth is directly affected by the magnetic variability of the Sun. Our climate is sensitive to variations in the irradiance of the Sun caused by cyclic magnetic activity. Space instrumentation and telecommunications are susceptible to solar high-energy eruptive events (e.g., for reviews, see, Schrijver and Zwaan, 2000). Predictive models of solar magnetic activity (e.g., Pesnell, 2008) depend on our knowledge of internal global-scale fluid motions of the Sun, constraints that can only be obtained seismically. Subsequent to the discovery of oscillations on the surface of the Sun some 50 years ago (Leighton et al., 1962), there has been significant progress in uncovering its properties.

Original languageEnglish (US)
Title of host publicationExtraterrestrial Seismology
PublisherCambridge University Press
Pages353-364
Number of pages12
ISBN (Electronic)9781107300668
ISBN (Print)9781107041721
DOIs
StatePublished - Jan 1 2015

Fingerprint

seismology
cross correlation
sun
tomography
stellar interiors
stellar atmospheres
oscillations
physics
random processes
stellar evolution
stochastic processes
wave interaction
irradiance
climate
telecommunication
astrophysics
oceans
convection
earthquakes
methodology

ASJC Scopus subject areas

  • Physics and Astronomy(all)

Cite this

Hanasoge, S. (2015). Interpreting cross-correlations in seismology. In Extraterrestrial Seismology (pp. 353-364). Cambridge University Press. https://doi.org/10.1017/CBO9781107300668.028

Interpreting cross-correlations in seismology. / Hanasoge, Shravan.

Extraterrestrial Seismology. Cambridge University Press, 2015. p. 353-364.

Research output: Chapter in Book/Report/Conference proceedingChapter

Hanasoge, S 2015, Interpreting cross-correlations in seismology. in Extraterrestrial Seismology. Cambridge University Press, pp. 353-364. https://doi.org/10.1017/CBO9781107300668.028
Hanasoge S. Interpreting cross-correlations in seismology. In Extraterrestrial Seismology. Cambridge University Press. 2015. p. 353-364 https://doi.org/10.1017/CBO9781107300668.028
Hanasoge, Shravan. / Interpreting cross-correlations in seismology. Extraterrestrial Seismology. Cambridge University Press, 2015. pp. 353-364
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