Related Experiment Video
Updated: Jan 20, 2026

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
Published on: June 8, 2015
Sub-GeV Atmospheric Neutrinos and CP Violation in DUNE
Kevin J Kelly1, Pedro A N Machado2, Ivan Martinez-Soler2,3,4
1Theory Department, Fermi National Accelerator Laboratory, Batavia, Illinois 60510, USA.
Researchers can determine the leptonic CP-violating phase using sub-GeV atmospheric neutrinos detected by liquid argon time projection chambers. This method offers a new way to probe CP violation in neutrino physics.
Area of Science:
- Particle Physics
- Astrophysics
- Neutrino Physics
Background:
- Studying atmospheric neutrinos provides insights into fundamental particle physics.
- Liquid argon time projection chambers offer unique capabilities for detecting low-energy events.
Purpose of the Study:
- To utilize liquid argon time projection chambers for sub-GeV atmospheric neutrino analysis.
- To determine the leptonic CP-violating phase (δCP) using atmospheric neutrinos.
- To explore the impact of sub-GeV atmospheric neutrino flux on other physics areas.
Main Methods:
- Employing the event topology and reconstruction capabilities of liquid argon time projection chambers.
- Detecting low-energy recoiled protons to measure neutrino interactions.
- Analyzing sub-GeV atmospheric neutrino data.
Main Results:
- The proposed analysis can exclude a range of δCP values beyond the 3σ level.
- This method provides a determination of δCP independent of accelerator neutrino measurements.
Conclusions:
- Sub-GeV atmospheric neutrinos offer a novel avenue for probing CP violation in the lepton sector.
- Accurate determination of atmospheric neutrino flux has implications for supernova neutrino detection and dark matter searches.
Related Concept Videos
Definition and Measurement of Pressure: Atmospheric Pressure, Barometer, and Manometer
Variation of Atmospheric Pressure
Assuming the air temperature is constant at a given altitude and that the ideal gas law of thermodynamics describes the atmosphere to a good approximation, one can find the variation of atmospheric pressure with height.
Let p(y) be the atmospheric pressure at...
13:27Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
09:34Extraction and Characterization of Surfactants from Atmospheric Aerosols
Influence of Earth's Curvature and Atmospheric Refraction on Leveling
