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During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance. Over a...
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Wave equations for porous media described by the Biot model.

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Related Experiment Video

Updated: Nov 27, 2025

Applying X-ray Imaging Crystal Spectroscopy for Use as a High Temperature Plasma Diagnostic
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Atmospheric wind and temperature profiles inversion using infrasound: An ensemble model context.

I Vera Rodriguez1, S P Näsholm1, A Le Pichon2

  • 1NORSAR, Kjeller, Norway.

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|December 2, 2020
PubMed
Summary

This study uses infrasound wave data to update atmospheric models, making complex inversions computationally feasible. The method successfully mapped stratospheric reflections from a real-world explosion.

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Area of Science:

  • Atmospheric science
  • Acoustic physics
  • Geophysics

Background:

  • Infrasound waves offer insights into atmospheric dynamics.
  • Updating atmospheric models with observational data is crucial but computationally challenging.
  • Previous inversion methods often require significant reformulation for new constraints.

Purpose of the Study:

  • To develop a flexible inversion methodology for updating atmospheric models using infrasound data.
  • To incorporate physical and numerical constraints without reformulating the inversion process.
  • To demonstrate the computational tractability of the inversion methodology.

Main Methods:

  • Utilized acoustic observations of infrasound waves to update an atmospheric model.
  • Employed parallel implementation and tight constraints derived from ERA5 ensemble reanalysis variance.
  • Used ensemble averages for initial model temperature and winds.
  • Inverted for stratospheric reflection altitude.

Main Results:

  • The inversion methodology proved computationally tractable despite an explicit search over the solution space.
  • Successfully applied to infrasound data from a Finnish ammunition destruction event.
  • Mapped stratospheric reflections within a classical shadow zone distance (178 km).

Conclusions:

  • The presented inversion methodology is a computationally feasible approach for integrating infrasound data into atmospheric models.
  • The method's flexibility allows for the incorporation of various physical and numerical constraints.
  • Demonstrated the utility of infrasound for probing atmospheric conditions, including stratospheric reflections.