Investigating the Applicability of the Peak Density Thickness Parameter over the Equatorial Region

The Peak Density Thickness (PDT) refers to a vertical region in the ionosphere encompassing the F2 peak, where electron density is at its maximum, and extending upward—maintaining a constant density—for a fixed altitude beyond this peak. This study builds on the previously established PDT concept, i...

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Main Authors: Mohamed O. Shammat, Bodo W. Reinisch, Ivan Galkin, Philip J. Erickson, Jay A. Weitzen, William C. Rideout
Format: Article
Language:English
Published: MDPI AG 2024-12-01
Series:Atmosphere
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Online Access:https://www.mdpi.com/2073-4433/16/1/10
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author Mohamed O. Shammat
Bodo W. Reinisch
Ivan Galkin
Philip J. Erickson
Jay A. Weitzen
William C. Rideout
author_facet Mohamed O. Shammat
Bodo W. Reinisch
Ivan Galkin
Philip J. Erickson
Jay A. Weitzen
William C. Rideout
author_sort Mohamed O. Shammat
collection DOAJ
description The Peak Density Thickness (PDT) refers to a vertical region in the ionosphere encompassing the F2 peak, where electron density is at its maximum, and extending upward—maintaining a constant density—for a fixed altitude beyond this peak. This study builds on the previously established PDT concept, initially explored at midlatitudes using data from Millstone Hill, by evaluating its applicability and effectiveness over equatorial latitudes using data from the Jicamarca Incoherent Scatter Radar (ISR) in Lima, Peru. A comprehensive analysis of electron density profiles measured by the Jicamarca ISR, spanning 1997 to 2020, was conducted using the Madrigal database to extract the PDT parameter for the F2 layer. Findings from the Jicamarca ISR indicate that the PDT parameter peaks around solar noon, aligning with observations from Millstone Hill. For selected case studies, the Vary-Chap topside model was employed to reconstruct the ionospheric profile above the F2 peak and PDT, demonstrating the model’s enhanced effectiveness when incorporating the PDT parameter over equatorial regions. This research confirms the presence of PDT in equatorial regions, consistent with its behavior at midlatitudes, and underscores the importance of PDT in refining predictive ionospheric models across different latitudes.
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spelling doaj-art-d42cfbd845a6499bbf7c048a811834ba2025-01-24T13:21:41ZengMDPI AGAtmosphere2073-44332024-12-011611010.3390/atmos16010010Investigating the Applicability of the Peak Density Thickness Parameter over the Equatorial RegionMohamed O. Shammat0Bodo W. Reinisch1Ivan Galkin2Philip J. Erickson3Jay A. Weitzen4William C. Rideout5Department of Electrical and Computer Engineering, University of Massachusetts Lowell, Lowell, MA 01854, USASpace Science Laboratory, University of Massachusetts Lowell, Lowell, MA 01854, USASpace Science Laboratory, University of Massachusetts Lowell, Lowell, MA 01854, USAMIT Haystack Observatory, Massachusetts Institute of Technology, Westford, MA 01886, USADepartment of Electrical and Computer Engineering, University of Massachusetts Lowell, Lowell, MA 01854, USAMIT Haystack Observatory, Massachusetts Institute of Technology, Westford, MA 01886, USAThe Peak Density Thickness (PDT) refers to a vertical region in the ionosphere encompassing the F2 peak, where electron density is at its maximum, and extending upward—maintaining a constant density—for a fixed altitude beyond this peak. This study builds on the previously established PDT concept, initially explored at midlatitudes using data from Millstone Hill, by evaluating its applicability and effectiveness over equatorial latitudes using data from the Jicamarca Incoherent Scatter Radar (ISR) in Lima, Peru. A comprehensive analysis of electron density profiles measured by the Jicamarca ISR, spanning 1997 to 2020, was conducted using the Madrigal database to extract the PDT parameter for the F2 layer. Findings from the Jicamarca ISR indicate that the PDT parameter peaks around solar noon, aligning with observations from Millstone Hill. For selected case studies, the Vary-Chap topside model was employed to reconstruct the ionospheric profile above the F2 peak and PDT, demonstrating the model’s enhanced effectiveness when incorporating the PDT parameter over equatorial regions. This research confirms the presence of PDT in equatorial regions, consistent with its behavior at midlatitudes, and underscores the importance of PDT in refining predictive ionospheric models across different latitudes.https://www.mdpi.com/2073-4433/16/1/10ionosphereelectron densitytopside profilebottomside profileIncoherent Scatter Radarionosonde
spellingShingle Mohamed O. Shammat
Bodo W. Reinisch
Ivan Galkin
Philip J. Erickson
Jay A. Weitzen
William C. Rideout
Investigating the Applicability of the Peak Density Thickness Parameter over the Equatorial Region
Atmosphere
ionosphere
electron density
topside profile
bottomside profile
Incoherent Scatter Radar
ionosonde
title Investigating the Applicability of the Peak Density Thickness Parameter over the Equatorial Region
title_full Investigating the Applicability of the Peak Density Thickness Parameter over the Equatorial Region
title_fullStr Investigating the Applicability of the Peak Density Thickness Parameter over the Equatorial Region
title_full_unstemmed Investigating the Applicability of the Peak Density Thickness Parameter over the Equatorial Region
title_short Investigating the Applicability of the Peak Density Thickness Parameter over the Equatorial Region
title_sort investigating the applicability of the peak density thickness parameter over the equatorial region
topic ionosphere
electron density
topside profile
bottomside profile
Incoherent Scatter Radar
ionosonde
url https://www.mdpi.com/2073-4433/16/1/10
work_keys_str_mv AT mohamedoshammat investigatingtheapplicabilityofthepeakdensitythicknessparameterovertheequatorialregion
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AT philipjerickson investigatingtheapplicabilityofthepeakdensitythicknessparameterovertheequatorialregion
AT jayaweitzen investigatingtheapplicabilityofthepeakdensitythicknessparameterovertheequatorialregion
AT williamcrideout investigatingtheapplicabilityofthepeakdensitythicknessparameterovertheequatorialregion