Relationship between weather conditions advantageous for the development of urban heat island and atmospheric macrocirculation changes

Urban heat island (UHI) and climate change belong to two separate scientific fields within meteorology nowadays. Climate change, however, may affect the characteristics of UHI as well. Various atmospheric macrocirculation conditions determine the frequency of certain weather conditions at a given ar...

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Published in:International Journal of Climatology
Main Authors: László, Elemér, Salavec, Péter
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2018
Subjects:
Online Access:http://dx.doi.org/10.1002/joc.5496
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spelling crwiley:10.1002/joc.5496 2024-06-02T08:11:27+00:00 Relationship between weather conditions advantageous for the development of urban heat island and atmospheric macrocirculation changes László, Elemér Salavec, Péter 2018 http://dx.doi.org/10.1002/joc.5496 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.5496 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.5496 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 38, issue 8, page 3224-3232 ISSN 0899-8418 1097-0088 journal-article 2018 crwiley https://doi.org/10.1002/joc.5496 2024-05-03T11:36:47Z Urban heat island (UHI) and climate change belong to two separate scientific fields within meteorology nowadays. Climate change, however, may affect the characteristics of UHI as well. Various atmospheric macrocirculation conditions determine the frequency of certain weather conditions at a given area, thus they influence the frequency of the occurrence of conditions advantageous for UHI development. In the present research, the time series data of conditions advantageous for UHI (advantageous meteorological conditions [AMC]) were determined in the case of Debrecen (Hungary) and similar patterns existing in the AMC time series were searched in those of North Atlantic Oscillation, East Atlantic Oscillation, East Atlantic (EA)/Western Russia (WR) Pattern and Scandinavian Oscillation indices for the period between 1961 and 2010 using Gábor–Morlet wavelet transformations. Several significantly coherent oscillations were found. The occurrence frequency of AMC can be approximated from macrocirculation conditions in these periods, according to the concept of heat island. These estimations are consistent with the calculated AMC time series. This proves that there is some relationship between macrocirculation and heat island development. Based on the results, using seasonal and climate models the changes of UHIs at seasonal and climatic scales may become predictable. Article in Journal/Newspaper North Atlantic North Atlantic oscillation Wiley Online Library International Journal of Climatology 38 8 3224 3232
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Urban heat island (UHI) and climate change belong to two separate scientific fields within meteorology nowadays. Climate change, however, may affect the characteristics of UHI as well. Various atmospheric macrocirculation conditions determine the frequency of certain weather conditions at a given area, thus they influence the frequency of the occurrence of conditions advantageous for UHI development. In the present research, the time series data of conditions advantageous for UHI (advantageous meteorological conditions [AMC]) were determined in the case of Debrecen (Hungary) and similar patterns existing in the AMC time series were searched in those of North Atlantic Oscillation, East Atlantic Oscillation, East Atlantic (EA)/Western Russia (WR) Pattern and Scandinavian Oscillation indices for the period between 1961 and 2010 using Gábor–Morlet wavelet transformations. Several significantly coherent oscillations were found. The occurrence frequency of AMC can be approximated from macrocirculation conditions in these periods, according to the concept of heat island. These estimations are consistent with the calculated AMC time series. This proves that there is some relationship between macrocirculation and heat island development. Based on the results, using seasonal and climate models the changes of UHIs at seasonal and climatic scales may become predictable.
format Article in Journal/Newspaper
author László, Elemér
Salavec, Péter
spellingShingle László, Elemér
Salavec, Péter
Relationship between weather conditions advantageous for the development of urban heat island and atmospheric macrocirculation changes
author_facet László, Elemér
Salavec, Péter
author_sort László, Elemér
title Relationship between weather conditions advantageous for the development of urban heat island and atmospheric macrocirculation changes
title_short Relationship between weather conditions advantageous for the development of urban heat island and atmospheric macrocirculation changes
title_full Relationship between weather conditions advantageous for the development of urban heat island and atmospheric macrocirculation changes
title_fullStr Relationship between weather conditions advantageous for the development of urban heat island and atmospheric macrocirculation changes
title_full_unstemmed Relationship between weather conditions advantageous for the development of urban heat island and atmospheric macrocirculation changes
title_sort relationship between weather conditions advantageous for the development of urban heat island and atmospheric macrocirculation changes
publisher Wiley
publishDate 2018
url http://dx.doi.org/10.1002/joc.5496
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.5496
https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.5496
genre North Atlantic
North Atlantic oscillation
genre_facet North Atlantic
North Atlantic oscillation
op_source International Journal of Climatology
volume 38, issue 8, page 3224-3232
ISSN 0899-8418 1097-0088
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/joc.5496
container_title International Journal of Climatology
container_volume 38
container_issue 8
container_start_page 3224
op_container_end_page 3232
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