Comparing wavelet and Fourier perspectives on the decomposition of meridional energy transport into synoptic and planetary components

Abstract The Arctic region shows some of the world's most significant signs of climate change; for instance, a negative trend in summer sea‐ice cover of around 15% per decade and Arctic amplified surface‐air warming that is three times the global average. The atmospheric energy transport plays...

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Published in:Quarterly Journal of the Royal Meteorological Society
Main Authors: Heiskanen, Tuomas, Graversen, Rune Grand, Rydsaa, Johanne Hope, Isachsen, Pål Erik
Other Authors: Norges Forskningsråd
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2020
Subjects:
Online Access:http://dx.doi.org/10.1002/qj.3813
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spelling crwiley:10.1002/qj.3813 2024-06-02T08:00:50+00:00 Comparing wavelet and Fourier perspectives on the decomposition of meridional energy transport into synoptic and planetary components Heiskanen, Tuomas Graversen, Rune Grand Rydsaa, Johanne Hope Isachsen, Pål Erik Norges Forskningsråd 2020 http://dx.doi.org/10.1002/qj.3813 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.3813 https://onlinelibrary.wiley.com/doi/pdf/10.1002/qj.3813 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/qj.3813 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.3813 en eng Wiley http://creativecommons.org/licenses/by/4.0/ Quarterly Journal of the Royal Meteorological Society volume 146, issue 731, page 2717-2730 ISSN 0035-9009 1477-870X journal-article 2020 crwiley https://doi.org/10.1002/qj.3813 2024-05-03T10:49:54Z Abstract The Arctic region shows some of the world's most significant signs of climate change; for instance, a negative trend in summer sea‐ice cover of around 15% per decade and Arctic amplified surface‐air warming that is three times the global average. The atmospheric energy transport plays an important role in the Arctic climate. Recently a Fourier‐based method for studying the atmospheric energy transport contribution by planetary‐ and synoptic‐scale waves has been proposed. Recent studies based on this method show that planetary waves contribute more than synoptic waves to the atmospheric energy transport into the Arctic. However, this Fourier method suffers from being incapable of resolving spatially localized systems such as cyclones. Here an attempt to evaluate this problem is presented by applying the method on synthetic and reanalysis data. In addition, an alternative method based on a wavelet decomposition is proposed and compared with the Fourier‐based method. The wavelet method is based on localized basis functions which should be capable of resolving these localized systems. The wavelet method shows an impact of synoptic‐scale transport on Arctic temperatures which is not captured by the Fourier method, whilst the planetary‐scale effect of both methods appears similar. Article in Journal/Newspaper Arctic Climate change Sea ice Wiley Online Library Arctic Quarterly Journal of the Royal Meteorological Society 146 731 2717 2730
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract The Arctic region shows some of the world's most significant signs of climate change; for instance, a negative trend in summer sea‐ice cover of around 15% per decade and Arctic amplified surface‐air warming that is three times the global average. The atmospheric energy transport plays an important role in the Arctic climate. Recently a Fourier‐based method for studying the atmospheric energy transport contribution by planetary‐ and synoptic‐scale waves has been proposed. Recent studies based on this method show that planetary waves contribute more than synoptic waves to the atmospheric energy transport into the Arctic. However, this Fourier method suffers from being incapable of resolving spatially localized systems such as cyclones. Here an attempt to evaluate this problem is presented by applying the method on synthetic and reanalysis data. In addition, an alternative method based on a wavelet decomposition is proposed and compared with the Fourier‐based method. The wavelet method is based on localized basis functions which should be capable of resolving these localized systems. The wavelet method shows an impact of synoptic‐scale transport on Arctic temperatures which is not captured by the Fourier method, whilst the planetary‐scale effect of both methods appears similar.
author2 Norges Forskningsråd
format Article in Journal/Newspaper
author Heiskanen, Tuomas
Graversen, Rune Grand
Rydsaa, Johanne Hope
Isachsen, Pål Erik
spellingShingle Heiskanen, Tuomas
Graversen, Rune Grand
Rydsaa, Johanne Hope
Isachsen, Pål Erik
Comparing wavelet and Fourier perspectives on the decomposition of meridional energy transport into synoptic and planetary components
author_facet Heiskanen, Tuomas
Graversen, Rune Grand
Rydsaa, Johanne Hope
Isachsen, Pål Erik
author_sort Heiskanen, Tuomas
title Comparing wavelet and Fourier perspectives on the decomposition of meridional energy transport into synoptic and planetary components
title_short Comparing wavelet and Fourier perspectives on the decomposition of meridional energy transport into synoptic and planetary components
title_full Comparing wavelet and Fourier perspectives on the decomposition of meridional energy transport into synoptic and planetary components
title_fullStr Comparing wavelet and Fourier perspectives on the decomposition of meridional energy transport into synoptic and planetary components
title_full_unstemmed Comparing wavelet and Fourier perspectives on the decomposition of meridional energy transport into synoptic and planetary components
title_sort comparing wavelet and fourier perspectives on the decomposition of meridional energy transport into synoptic and planetary components
publisher Wiley
publishDate 2020
url http://dx.doi.org/10.1002/qj.3813
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fqj.3813
https://onlinelibrary.wiley.com/doi/pdf/10.1002/qj.3813
https://onlinelibrary.wiley.com/doi/full-xml/10.1002/qj.3813
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/qj.3813
geographic Arctic
geographic_facet Arctic
genre Arctic
Climate change
Sea ice
genre_facet Arctic
Climate change
Sea ice
op_source Quarterly Journal of the Royal Meteorological Society
volume 146, issue 731, page 2717-2730
ISSN 0035-9009 1477-870X
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1002/qj.3813
container_title Quarterly Journal of the Royal Meteorological Society
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