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  • Other Sources  (5)
  • American Association for the Advancement of Science
  • American Institute of Physics
  • American Physical Society
  • Periodicals Archive Online (PAO)
  • Springer Nature
  • 1995-1999  (5)
  • 1
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    Springer Nature
    In:  Nature, 382 (6590). pp. 408-409.
    Publication Date: 2021-09-02
    Type: Article , PeerReviewed
    Format: text
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  • 2
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    American Institute of Physics
    In:  Journal of the Acoustical Society of America, 103 (3). pp. 1346-1352.
    Publication Date: 2020-07-16
    Description: Two sets of equations, covering all world oceans and seas, are presented to calculate pressure from depth for the computation of sound speed, and depth from pressure for use in ocean engineering. They are based on the algorithm of UNESCO 1983 [N. P. Fofonoff and R. C. Millard, Jr., Unesco Tech. Papers in Mar. Sci. No. 44 (1983)], and on calculations from temperature and salinity profiles. The pressure to depth conversion is presented first. The equations can be used in those cases where the desired accuracy is reduced to ±0.8 m. The equations to convert depth to pressure provide an overall accuracy between ±8000 Pa and ±1000 Pa. This leads to errors in sound speed consistently smaller than ±0.02 m/s. The discussion, and comparisons with results and other formulas, suggest that the new equations are a substantial improvement on the previous simplified ones, which should now be abandoned.
    Type: Article , PeerReviewed
    Format: text
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  • 3
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    American Institute of Physics
    In:  The Leading Edge, 18 (1). pp. 74-80.
    Publication Date: 2018-01-18
    Type: Article , NonPeerReviewed
    Format: text
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  • 4
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    American Institute of Physics
    In:  The Leading Edge, 15 (10). p. 1090.
    Publication Date: 2016-08-30
    Description: Attributes have proliferated recently with different selections available on different workstations. What do they all mean? When do we use one and when another? The answers to these questions are not easy but the first step is to understand what our options are, and herein lies the purpose of this article.
    Type: Article , PeerReviewed
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  • 5
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    American Institute of Physics
    In:  The Leading Edge, 14 (10). pp. 1053-1058.
    Publication Date: 2016-07-26
    Description: Seismic data are usually acquired and processed for imaging reflections. This paper describes a method of processing seismic data for imaging discontinuities (e.g., faults and stratigraphic features). One application of this nontraditional process is a 3-D volume, or cube, of coherence coefficients within which faults are revealed as numerically separated surfaces. Figure 1 compares a traditional 3-D reflection amplitude time slice with the results of the new method. To our knowledge, this is the first published method of revealing fault surfaces within a 3-D volume for which no fault reflections have been recorded.
    Type: Article , PeerReviewed
    Format: text
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