Could we find any signal of the stratosphere-ionosphere coupling in Antarctica?
An investigation searching for a possible coupling between the lower ionosphere and the middle atmosphere in Antarctica is here performed on the basis of stratospheric vertical temperature profiles and ionospheric absorption data observed at the Antarctic Italian Base of Terra Nova Bay (74.69°S, 164...
Published in: | Annals of Geophysics |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
2009
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Subjects: | |
Online Access: | https://www.openaccessrepository.it/record/130007 https://doi.org/10.4401/ag-3484 |
_version_ | 1821771983426158592 |
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author | Carlo Scotto G. De Franceschi Edward S. Kazimirovsky Paolo Grigioni Marco Pietrella |
author_facet | Carlo Scotto G. De Franceschi Edward S. Kazimirovsky Paolo Grigioni Marco Pietrella |
author_sort | Carlo Scotto |
collection | Istituto Nazionale di Fisica Nucleare (INFN): Open Access Repository |
container_issue | 1 |
container_title | Annals of Geophysics |
container_volume | 45 |
description | An investigation searching for a possible coupling between the lower ionosphere and the middle atmosphere in Antarctica is here performed on the basis of stratospheric vertical temperature profiles and ionospheric absorption data observed at the Antarctic Italian Base of Terra Nova Bay (74.69°S, 164.12°E) during local summer time. The result obtained by applying a multi-regression analysis and a Superimposed Epoch Analysis (SEA) shows a statistically significant ionosphere-stratosphere interaction. In particular, by selecting stratospheric temperature maxima occurring at different heights as the referring epoch («zero day») for the SEA approach, the ionospheric absorption is found to show a positive and/or negative trend (several days) around it. The tendency for an increasing/decreasing absorption is obtained for temperature maxima occurring below/above the stratospheric level of about 17-19 km, respectively. |
format | Article in Journal/Newspaper |
genre | Antarc* Antarctic Antarctica |
genre_facet | Antarc* Antarctic Antarctica |
geographic | Antarctic Terra Nova Bay The Antarctic |
geographic_facet | Antarctic Terra Nova Bay The Antarctic |
id | ftopenaccessrep:oai:zenodo.org:130007 |
institution | Open Polar |
language | unknown |
op_collection_id | ftopenaccessrep |
op_doi | https://doi.org/10.4401/ag-3484 |
op_relation | url:https://www.openaccessrepository.it/communities/itmirror https://www.openaccessrepository.it/record/130007 doi:10.4401/ag-3484 |
op_rights | info:eu-repo/semantics/openAccess |
publishDate | 2009 |
record_format | openpolar |
spelling | ftopenaccessrep:oai:zenodo.org:130007 2025-01-16T19:38:44+00:00 Could we find any signal of the stratosphere-ionosphere coupling in Antarctica? Carlo Scotto G. De Franceschi Edward S. Kazimirovsky Paolo Grigioni Marco Pietrella 2009-12-18 https://www.openaccessrepository.it/record/130007 https://doi.org/10.4401/ag-3484 und unknown url:https://www.openaccessrepository.it/communities/itmirror https://www.openaccessrepository.it/record/130007 doi:10.4401/ag-3484 info:eu-repo/semantics/openAccess NEANIAS Atmospheric Research Community Geophysics info:eu-repo/semantics/article publication-article 2009 ftopenaccessrep https://doi.org/10.4401/ag-3484 2023-10-03T22:19:57Z An investigation searching for a possible coupling between the lower ionosphere and the middle atmosphere in Antarctica is here performed on the basis of stratospheric vertical temperature profiles and ionospheric absorption data observed at the Antarctic Italian Base of Terra Nova Bay (74.69°S, 164.12°E) during local summer time. The result obtained by applying a multi-regression analysis and a Superimposed Epoch Analysis (SEA) shows a statistically significant ionosphere-stratosphere interaction. In particular, by selecting stratospheric temperature maxima occurring at different heights as the referring epoch («zero day») for the SEA approach, the ionospheric absorption is found to show a positive and/or negative trend (several days) around it. The tendency for an increasing/decreasing absorption is obtained for temperature maxima occurring below/above the stratospheric level of about 17-19 km, respectively. Article in Journal/Newspaper Antarc* Antarctic Antarctica Istituto Nazionale di Fisica Nucleare (INFN): Open Access Repository Antarctic Terra Nova Bay The Antarctic Annals of Geophysics 45 1 |
spellingShingle | NEANIAS Atmospheric Research Community Geophysics Carlo Scotto G. De Franceschi Edward S. Kazimirovsky Paolo Grigioni Marco Pietrella Could we find any signal of the stratosphere-ionosphere coupling in Antarctica? |
title | Could we find any signal of the stratosphere-ionosphere coupling in Antarctica? |
title_full | Could we find any signal of the stratosphere-ionosphere coupling in Antarctica? |
title_fullStr | Could we find any signal of the stratosphere-ionosphere coupling in Antarctica? |
title_full_unstemmed | Could we find any signal of the stratosphere-ionosphere coupling in Antarctica? |
title_short | Could we find any signal of the stratosphere-ionosphere coupling in Antarctica? |
title_sort | could we find any signal of the stratosphere-ionosphere coupling in antarctica? |
topic | NEANIAS Atmospheric Research Community Geophysics |
topic_facet | NEANIAS Atmospheric Research Community Geophysics |
url | https://www.openaccessrepository.it/record/130007 https://doi.org/10.4401/ag-3484 |