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Spectral changes in the zenith skylight during total solar eclipses.
Zenith sky spectral intensity remained constant during a 1970 solar eclipse. Color shifts observed at lower solar angles align with Rayleigh scattering, but higher angles show inconsistencies.
Area of Science:
- Atmospheric optics
- Solar physics
- Spectroscopy
Background:
- Understanding the spectral distribution of the zenith sky is crucial for atmospheric studies.
- Total solar eclipses offer unique opportunities to study atmospheric light scattering.
- Previous measurements have shown varying results regarding color shifts during eclipses.
Purpose of the Study:
- To measure the relative spectral intensity of the zenith sky during a total solar eclipse.
- To investigate potential color shifts in the zenith sky spectrum during an eclipse.
- To compare eclipse observations with established atmospheric scattering models.
Main Methods:
- Utilized an optical scanning spectrometer for spectral intensity measurements.
- Recorded data at Nantucket Island, Massachusetts, during the March 7, 1970, total solar eclipse.
- Calculated spectral ratios I(5100 A)/I(4300 A) and I(5900 A)/I(5100 A).
Main Results:
- Spectral ratios remained constant for up to 96% solar obscuration.
- A blue color shift was observed for solar elevation angles below 45 degrees, consistent with Rayleigh scattering.
- Inconsistent color shifts were noted for solar elevation angles above 45 degrees.
Conclusions:
- Zenith sky spectral intensity is stable during significant solar obscuration.
- Rayleigh scattering explains observed color shifts at lower solar elevation angles.
- Inconsistencies at higher solar angles may stem from challenges in selecting a reference spectrum.
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