Critical Refraction
Critical Refraction is a seismic refraction phenomenon in which a refracted wave propagates along the interface between two geological layers at the critical angle, resulting in the minimum angle of incidence at which the refracted ray travels parallel to the boundary, thereby enabling the detection of subsurface layer velocities and depths through first-arrival travel-time analysis.
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2017–2026
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Head WaveHead Waves
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The GPS Radio Occultation Technique
E. R. Kursinski, G. A. Hajj, S. S. Leroy et al. · Terrestrial Atmospheric and Oceanic Sciences · 2000 · 254 citations · Full text
Lower troposphere refractivity bias in GPS occultation retrievals
C. O. Ao, T. K. Meehan, G. A. Hajj et al. · Journal of Geophysical Research Atmospheres · 2003 · 183 citations · Full text
Atmosphere and Ionosphere of Venus from the Mariner V S-Band Radio Occultation Measurement
A. J. Kliore, G. S. Levy, D. L. Cain et al. · Science · 1967 · 163 citations
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Jet Propulsion Laboratory
Pasadena, United States
4 h-index
13 publications
2.1K citations

Harbin Institute of Technology
Harbin, China
2 h-index
2 publications
31 citations
Stanford University
Stanford, United States
2 h-index
3 publications
383 citations
Jiangsu University of Science and Technology
Zhenjiang, China
2 h-index
4 publications
62 citations
University of Arizona
Tucson, United States
2 h-index
3 publications
366 citations

Hokkaido University
Sapporo, Japan
1 h-index
9 publications
279 citations
BP (United Kingdom)
London, United Kingdom
1 h-index
1 publications
15 citations

Beijing Institute of Technology
Beijing, China
1 h-index
6 publications
84 citations
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3 publications · 141 citations
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JASA · 2 publications · 167 citations
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GJI · 2 publications · 49 citations
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2 publications · 28 citations
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JGR · 1 publications · 183 citations
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