On seeding equatorial spread F during solstices

Interpretation of the morphology of equatorial spread F (ESF) is usually given in terms of factors that modulate the growth rate of the Rayleigh‐Taylor instability. That interpretation is, however, incomplete because only one means for growth‐rate enhancement has been included; that is, the strength...

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Published in:Geophysical research letters Vol. 37; no. 5
Main Author: Tsunoda, Roland T.
Format: Journal Article
Language:English
Published: Washington, DC Blackwell Publishing Ltd 01-03-2010
American Geophysical Union
John Wiley & Sons, Inc
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Abstract Interpretation of the morphology of equatorial spread F (ESF) is usually given in terms of factors that modulate the growth rate of the Rayleigh‐Taylor instability. That interpretation is, however, incomplete because only one means for growth‐rate enhancement has been included; that is, the strength of the post‐sunset rise of the F layer could become enhanced, when the solar terminator aligns with geomagnetic field lines. Maxima in ESF occurrence observed near equinoxes seem accountable by this means, but maxima observed near solstices require another source of enhancement. Seasonal migration and latitudinal alignment of the inter‐tropical convergence zone (ITCZ) with the magnetic dip equator is suggested as the missing source, and shown able to fill that void.
AbstractList Interpretation of the morphology of equatorial spread F (ESF) is usually given in terms of factors that modulate the growth rate of the Rayleigh‐Taylor instability. That interpretation is, however, incomplete because only one means for growth‐rate enhancement has been included; that is, the strength of the post‐sunset rise of the F layer could become enhanced, when the solar terminator aligns with geomagnetic field lines. Maxima in ESF occurrence observed near equinoxes seem accountable by this means, but maxima observed near solstices require another source of enhancement. Seasonal migration and latitudinal alignment of the inter‐tropical convergence zone (ITCZ) with the magnetic dip equator is suggested as the missing source, and shown able to fill that void.
Interpretation of the morphology of equatorial spread F (ESF) is usually given in terms of factors that modulate the growth rate of the Rayleigh‐Taylor instability. That interpretation is, however, incomplete because only one means for growth‐rate enhancement has been included; that is, the strength of the post‐sunset rise of the F layer could become enhanced, when the solar terminator aligns with geomagnetic field lines. Maxima in ESF occurrence observed near equinoxes seem accountable by this means, but maxima observed near solstices require another source of enhancement. Seasonal migration and latitudinal alignment of the inter‐tropical convergence zone (ITCZ) with the magnetic dip equator is suggested as the missing source, and shown able to fill that void.
Author Tsunoda, Roland T.
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  givenname: Roland T.
  surname: Tsunoda
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  organization: Center for Geospace Studies, SRI International, California, Menlo Park, USA
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Issue 5
Keywords Field line
growth rates
morphology
strength
dip
geomagnetic field
Seeding
Sunset
Alignment
interpretation
Solar terminator
Rayleigh Taylor instability
migration
Spread F
Intertropical convergence zone
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Snippet Interpretation of the morphology of equatorial spread F (ESF) is usually given in terms of factors that modulate the growth rate of the Rayleigh‐Taylor...
Interpretation of the morphology of equatorial spread F (ESF) is usually given in terms of factors that modulate the growth rate of the Rayleigh‐Taylor...
Interpretation of the morphology of equatorial spread F (ESF) is usually given in terms of factors that modulate the growth rate of the Rayleigh-Taylor...
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SubjectTerms Alignment
Atmospheric sciences
Convergence
Dipping
Earth sciences
Earth, ocean, space
Equator
equatorial spread F
Exact sciences and technology
Geomagnetic field
Maxima
Migration
Nucleation
Solstices
Spread F
Title On seeding equatorial spread F during solstices
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