Distinct ionospheric long-term trends in Antarctica due to the Weddell Sea Anomaly
<p>The Weddell Sea Anomaly (WSA), a summer ionospheric anomaly over the eastern Antarctic Peninsula, was first observed in 1958 and is characterized by a nighttime peak in electron concentration instead of a the typical daytime peak. There are some works that examine long-term trends at ionosp...
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Copernicus Publications
2025-07-01
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| Series: | Annales Geophysicae |
| Online Access: | https://angeo.copernicus.org/articles/43/383/2025/angeo-43-383-2025.pdf |
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| author | M. Canales T. Duran M. Bravo A. Zalizovski A. Zalizovski A. Zalizovski A. Foppiano |
| author_facet | M. Canales T. Duran M. Bravo A. Zalizovski A. Zalizovski A. Zalizovski A. Foppiano |
| author_sort | M. Canales |
| collection | DOAJ |
| description | <p>The Weddell Sea Anomaly (WSA), a summer ionospheric anomaly over the eastern Antarctic Peninsula, was first observed in 1958 and is characterized by a nighttime peak in electron concentration instead of a the typical daytime peak. There are some works that examine long-term trends at ionospheric stations in the WSA region, but they do not do a seasonal and diurnal analysis that is vital for differentiating the periods of the anomaly. This study investigates the seasonal and diurnal variation in the long-term trend in the F2-layer critical frequency (<i>fo</i>F2) at ionospheric stations located within the WSA region: Vernadsky (Argentine Island; 65.1° S, 64.2° W) and Port Stanley (51.6° S, 57.9° W), both with long-term <i>fo</i>F2 data. Data from Vernadsky (1960–2023) and Port Stanley (1960–2019) were analyzed alongside data from Syowa (69.0° S; 39.6° E) and Mawson (67.6° S, 62.9° E), two stations outside the WSA influence. The analysis reveals distinct seasonal and diurnal trends. For Vernadsky, negative <i>fo</i>F2 trends (<span class="inline-formula">−</span>0.02 MHz yr<span class="inline-formula"><sup>−1</sup></span>) are observed during summer nights, coinciding with the WSA's presence. Port Stanley shows similar trends but with a secondary nighttime maximum. The WSA's influence on Vernadsky is more pronounced, with Port Stanley exhibiting a weaker mid-latitude summer evening anomaly. In contrast, Syowa and Mawson show different trends, with Syowa not having a clear trend pattern, and Mawson showing negative trends throughout the year. The study concludes that the WSA significantly affects Vernadsky and, to a lesser extent, Port Stanley. The findings highlight regional variations in ionospheric behavior and contribute to the ongoing discussion on global ionospheric trends, suggesting that local phenomena like the WSA can modulate these trends.</p> |
| format | Article |
| id | doaj-art-7dad41ea26cf4f30a367e1e017aca5a6 |
| institution | OA Journals |
| issn | 0992-7689 1432-0576 |
| language | English |
| publishDate | 2025-07-01 |
| publisher | Copernicus Publications |
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| series | Annales Geophysicae |
| spelling | doaj-art-7dad41ea26cf4f30a367e1e017aca5a62025-08-20T02:36:08ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762025-07-014338339010.5194/angeo-43-383-2025Distinct ionospheric long-term trends in Antarctica due to the Weddell Sea AnomalyM. Canales0T. Duran1M. Bravo2A. Zalizovski3A. Zalizovski4A. Zalizovski5A. Foppiano6Departamento de Geofísica, Universidad de Concepción, Concepción, 4070386, ChileDepartamento de Física, Universidad Nacional del Sur, Bahía Blanca, 8000, ArgentinaCentro de Instrumentación Científica, Universidad Adventista de Chile, Chillán, 3780000, ChileInstitute of Radio Astronomy, National Academy of Sciences of Ukraine, 61002, Kharkiv, UkraineNational Antarctic Scientific Center of Ukraine, 01601, Kyiv, UkraineSpace Research Centre of Polish Academy of Sciences, 00-716, Warsaw, PolandCentro de Instrumentación Científica, Universidad Adventista de Chile, Chillán, 3780000, Chile<p>The Weddell Sea Anomaly (WSA), a summer ionospheric anomaly over the eastern Antarctic Peninsula, was first observed in 1958 and is characterized by a nighttime peak in electron concentration instead of a the typical daytime peak. There are some works that examine long-term trends at ionospheric stations in the WSA region, but they do not do a seasonal and diurnal analysis that is vital for differentiating the periods of the anomaly. This study investigates the seasonal and diurnal variation in the long-term trend in the F2-layer critical frequency (<i>fo</i>F2) at ionospheric stations located within the WSA region: Vernadsky (Argentine Island; 65.1° S, 64.2° W) and Port Stanley (51.6° S, 57.9° W), both with long-term <i>fo</i>F2 data. Data from Vernadsky (1960–2023) and Port Stanley (1960–2019) were analyzed alongside data from Syowa (69.0° S; 39.6° E) and Mawson (67.6° S, 62.9° E), two stations outside the WSA influence. The analysis reveals distinct seasonal and diurnal trends. For Vernadsky, negative <i>fo</i>F2 trends (<span class="inline-formula">−</span>0.02 MHz yr<span class="inline-formula"><sup>−1</sup></span>) are observed during summer nights, coinciding with the WSA's presence. Port Stanley shows similar trends but with a secondary nighttime maximum. The WSA's influence on Vernadsky is more pronounced, with Port Stanley exhibiting a weaker mid-latitude summer evening anomaly. In contrast, Syowa and Mawson show different trends, with Syowa not having a clear trend pattern, and Mawson showing negative trends throughout the year. The study concludes that the WSA significantly affects Vernadsky and, to a lesser extent, Port Stanley. The findings highlight regional variations in ionospheric behavior and contribute to the ongoing discussion on global ionospheric trends, suggesting that local phenomena like the WSA can modulate these trends.</p>https://angeo.copernicus.org/articles/43/383/2025/angeo-43-383-2025.pdf |
| spellingShingle | M. Canales T. Duran M. Bravo A. Zalizovski A. Zalizovski A. Zalizovski A. Foppiano Distinct ionospheric long-term trends in Antarctica due to the Weddell Sea Anomaly Annales Geophysicae |
| title | Distinct ionospheric long-term trends in Antarctica due to the Weddell Sea Anomaly |
| title_full | Distinct ionospheric long-term trends in Antarctica due to the Weddell Sea Anomaly |
| title_fullStr | Distinct ionospheric long-term trends in Antarctica due to the Weddell Sea Anomaly |
| title_full_unstemmed | Distinct ionospheric long-term trends in Antarctica due to the Weddell Sea Anomaly |
| title_short | Distinct ionospheric long-term trends in Antarctica due to the Weddell Sea Anomaly |
| title_sort | distinct ionospheric long term trends in antarctica due to the weddell sea anomaly |
| url | https://angeo.copernicus.org/articles/43/383/2025/angeo-43-383-2025.pdf |
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