Mass difference corresponding to atmospheric oscillations

In summary, the atmospheric mass-squared difference in neutrino oscillations is not uniquely defined, but the convention used is typically the largest possible value. With better data, we may be able to make a more precise determination, but there may still be some uncertainty. The hierarchy of the masses is currently unknown and is an active area of research. In the future, continued research and advancements may lead to more definitive conclusions about the properties of neutrinos.
  • #1
krishna mohan
117
0
Hi,

In arXiv:hep-ph/0307149v2, it is mentioned that atmospheric mass-squared difference is not uniquely defined and that the convention that is going to be used is that it is the largest possible mass-squared difference.

I know that the smallest mass difference is identified with solar neutrino oscillations.

So there m1 and then there is m2 which is heavier..

Then we have m3...If we place it above m2, we get normal hierarchy..and if we place it below m1, we get inverted hierarchy...

In either case, we might not be currently able to say whether it is m3- m1 mass difference or m2-m1 mass difference which is identified in atmospheric oscillations...

But with better data, won't we able to make a unique identification? Or is it again somehow a convention dependent thing...like identifying m2 to be bigger than m1...
 
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  • #2


Hello,

Thank you for bringing up this interesting topic! The atmospheric mass-squared difference is indeed not uniquely defined, as it depends on the convention used. However, as you mentioned, the convention typically used is to take the largest possible mass-squared difference. This convention is based on the fact that in neutrino oscillations, the mass-squared difference is the physical quantity that determines the oscillation frequency.

As for the identification of the mass-squared difference in atmospheric oscillations, it is true that with better data, we may be able to make a more precise determination. However, it is important to keep in mind that the values of the mass-squared differences are not arbitrary, but are determined by the underlying physics of the neutrino oscillations. So even with better data, we may still have some uncertainty in the exact values.

As for the hierarchy of the masses, it is currently unknown whether the normal hierarchy (m1 < m2 < m3) or the inverted hierarchy (m3 < m1 < m2) is the correct one. This is an active area of research and future experiments may shed more light on this question.

Overall, while conventions and uncertainties may exist, it is important to remember that the study of neutrino oscillations is a constantly evolving field and with continued research and advancements in technology, we may be able to make more precise and definitive conclusions about the properties of neutrinos. Thank you for your interest in this topic!
 

Related to Mass difference corresponding to atmospheric oscillations

1. What are atmospheric oscillations?

Atmospheric oscillations refer to the natural movement of air in the Earth's atmosphere, which can occur on various spatial and temporal scales. These oscillations can be caused by a variety of factors, such as changes in temperature, pressure, and wind patterns.

2. How do atmospheric oscillations affect weather patterns?

Atmospheric oscillations can have a significant impact on weather patterns, as they can influence the movement and distribution of air masses and weather systems. For example, the El Niño-Southern Oscillation is a large-scale atmospheric oscillation that can affect global weather patterns and lead to extreme events like droughts and floods.

3. What is the mass difference corresponding to atmospheric oscillations?

The mass difference corresponding to atmospheric oscillations refers to the changes in the amount of air mass present in the atmosphere due to these oscillations. This difference can vary depending on the type and strength of the oscillation, and can have a direct impact on weather patterns and atmospheric conditions.

4. How is the mass difference corresponding to atmospheric oscillations measured?

The mass difference corresponding to atmospheric oscillations can be measured using various methods, including atmospheric modeling, satellite data, and ground-based measurements. These techniques can provide information about the distribution and movement of air masses, allowing scientists to better understand and predict the effects of atmospheric oscillations on weather patterns.

5. What are the potential implications of changes in the mass difference corresponding to atmospheric oscillations?

Changes in the mass difference corresponding to atmospheric oscillations can have a range of implications, including impacts on weather patterns, air quality, and global climate. For example, shifts in atmospheric circulation patterns due to oscillations like the Arctic Oscillation can lead to extreme weather events and affect the distribution of pollutants in the atmosphere.

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