The Semidiurnal Tidal Response of the Low Latitude Ionosphere to Northern Hemisphere Polar Vortex Strength (2020–2023) From COSMIC‐2 Global Ionospheric Specification

Abstract This paper investigates the day‐to‐day global tidal variability in the ionosphere/thermosphere system due to fluctuations in the strength of the northern hemisphere stratospheric polar vortex. Using COSMIC‐2 (Constellation Observing System for Meteorology, Ionosphere, and Climate‐2) Global...

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Main Authors: Deepali Aggarwal, Jens Oberheide, Nicholas Pedatella, Benjamin C. Martinez
Format: Article
Language:English
Published: Wiley 2025-01-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2024GL111313
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author Deepali Aggarwal
Jens Oberheide
Nicholas Pedatella
Benjamin C. Martinez
author_facet Deepali Aggarwal
Jens Oberheide
Nicholas Pedatella
Benjamin C. Martinez
author_sort Deepali Aggarwal
collection DOAJ
description Abstract This paper investigates the day‐to‐day global tidal variability in the ionosphere/thermosphere system due to fluctuations in the strength of the northern hemisphere stratospheric polar vortex. Using COSMIC‐2 (Constellation Observing System for Meteorology, Ionosphere, and Climate‐2) Global Ionospheric Specification data, ionospheric tides are derived, with the Northern Annular Mode (NAM) index indicating polar vortex variability. The semidiurnal migrating solar tide shows the largest response, with relative electron density in the F‐region significantly higher (∼ 60%) under a weak vortex and lower (∼ 20%) under a strong vortex, correlated at −0.58 with the NAM index. The study compares solar/geomagnetic forcing and vortex impacts using SD‐WACCM‐X (Specified Dynamics Whole Atmosphere Community Climate Model with thermosphere and ionosphere extension) model runs. Findings suggest tidal modulation of the E‐region dynamo as the coupling mechanism. Our study can potentially improve ionospheric space weather predictability because the NAM index can be known a few days in advance.
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institution Kabale University
issn 0094-8276
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publishDate 2025-01-01
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series Geophysical Research Letters
spelling doaj-art-4d46cc4067b7451eb5840328c8517ca12025-01-20T13:05:57ZengWileyGeophysical Research Letters0094-82761944-80072025-01-01521n/an/a10.1029/2024GL111313The Semidiurnal Tidal Response of the Low Latitude Ionosphere to Northern Hemisphere Polar Vortex Strength (2020–2023) From COSMIC‐2 Global Ionospheric SpecificationDeepali Aggarwal0Jens Oberheide1Nicholas Pedatella2Benjamin C. Martinez3Department of Physics and Astronomy Clemson University Clemson SC USADepartment of Physics and Astronomy Clemson University Clemson SC USAHigh Altitude Observatory National Center for Atmospheric Research Boulder CO USADepartment of Physics and Astronomy Clemson University Clemson SC USAAbstract This paper investigates the day‐to‐day global tidal variability in the ionosphere/thermosphere system due to fluctuations in the strength of the northern hemisphere stratospheric polar vortex. Using COSMIC‐2 (Constellation Observing System for Meteorology, Ionosphere, and Climate‐2) Global Ionospheric Specification data, ionospheric tides are derived, with the Northern Annular Mode (NAM) index indicating polar vortex variability. The semidiurnal migrating solar tide shows the largest response, with relative electron density in the F‐region significantly higher (∼ 60%) under a weak vortex and lower (∼ 20%) under a strong vortex, correlated at −0.58 with the NAM index. The study compares solar/geomagnetic forcing and vortex impacts using SD‐WACCM‐X (Specified Dynamics Whole Atmosphere Community Climate Model with thermosphere and ionosphere extension) model runs. Findings suggest tidal modulation of the E‐region dynamo as the coupling mechanism. Our study can potentially improve ionospheric space weather predictability because the NAM index can be known a few days in advance.https://doi.org/10.1029/2024GL111313ionosphereE‐region dynamoatmospheric tidespolar vortexvertical couplingshort‐term variability
spellingShingle Deepali Aggarwal
Jens Oberheide
Nicholas Pedatella
Benjamin C. Martinez
The Semidiurnal Tidal Response of the Low Latitude Ionosphere to Northern Hemisphere Polar Vortex Strength (2020–2023) From COSMIC‐2 Global Ionospheric Specification
Geophysical Research Letters
ionosphere
E‐region dynamo
atmospheric tides
polar vortex
vertical coupling
short‐term variability
title The Semidiurnal Tidal Response of the Low Latitude Ionosphere to Northern Hemisphere Polar Vortex Strength (2020–2023) From COSMIC‐2 Global Ionospheric Specification
title_full The Semidiurnal Tidal Response of the Low Latitude Ionosphere to Northern Hemisphere Polar Vortex Strength (2020–2023) From COSMIC‐2 Global Ionospheric Specification
title_fullStr The Semidiurnal Tidal Response of the Low Latitude Ionosphere to Northern Hemisphere Polar Vortex Strength (2020–2023) From COSMIC‐2 Global Ionospheric Specification
title_full_unstemmed The Semidiurnal Tidal Response of the Low Latitude Ionosphere to Northern Hemisphere Polar Vortex Strength (2020–2023) From COSMIC‐2 Global Ionospheric Specification
title_short The Semidiurnal Tidal Response of the Low Latitude Ionosphere to Northern Hemisphere Polar Vortex Strength (2020–2023) From COSMIC‐2 Global Ionospheric Specification
title_sort semidiurnal tidal response of the low latitude ionosphere to northern hemisphere polar vortex strength 2020 2023 from cosmic 2 global ionospheric specification
topic ionosphere
E‐region dynamo
atmospheric tides
polar vortex
vertical coupling
short‐term variability
url https://doi.org/10.1029/2024GL111313
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