Analyzing WSTP trend: a new method for global warming assessment

Detalhes bibliográficos
Autor(a) principal: Heydari Alamdarloo, Esmail
Data de Publicação: 2021
Outros Autores: Moradi, Ehsan, Abdolshahnejad, Mahsa, Fatahi, Yalda, Khosravi, Hassan, da Silva, Alexandre Marco [UNESP]
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://dx.doi.org/10.1007/s10661-021-09600-2
http://hdl.handle.net/11449/229886
Resumo: This paper tries to introduce a time-series of temperature parameters as a potential method for studying the global warming. So, we investigated the spatial–temporal variations of warm-season temperature parameters (WSTP), including start time, end time, length of season, base value, peak time, peak value, amplitude, large integrated value, right drive, and left drive, using a database of 30 years’ period in different climates of Iran. We used daily temperature data from 1989 to 2018 over Iran to extract the parameters by TIMESAT software. We studied the trend analysis of WSTP through the Mann–Kendall method. Then, we considered the Pearson correlation coefficient to calculate the correlation between WSTP and time. We assessed the trends of the slope using a simple linear regression method. Then, we compared the results of the WSTP trend analysis in climatic zones. Our results accused the hyper-arid climatic zone has the longest warm season (194.89 days a year). The warm season in this region starts earlier than other regions and increases with moderate speed (left drive, 0.19 °C day−1). Then, it reaches a peak value (31.3 °C) earlier than the different climatic zones. On the other hand, the humid regions’ warm season starts with the shortest length and ends later than the other climatic zones (112.1 and 297.5 days a year for start and end times, respectively). We detected that the trend of the start time parameter has decreased by 98.02% of the study area during the last 30 years. The base value, length, and large integrated value parameters have an increasing trend of 66.47%, 80.11%, and 92.95% in Iran. The highest correlation coefficient with time was for start time and large integrated value parameters. Hence, the start time and large integrated value parameters have almost the most negative (< − 0.5) and positive (> 5) trend slope, among other parameters, respectively. In general, these results demonstrate that the studied region has faced global warming impacts over time by increasing the warm season and thermal energy, especially in arid and hyper-arid. We highlight the necessity of planning the land use under the high natural vulnerability of the studied local, especially in this new age of global warming.
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spelling Analyzing WSTP trend: a new method for global warming assessmentMann–KendallPearson correlation coefficientSimple linear regressionSpatial–temporal variations of WSTPTIMESATThis paper tries to introduce a time-series of temperature parameters as a potential method for studying the global warming. So, we investigated the spatial–temporal variations of warm-season temperature parameters (WSTP), including start time, end time, length of season, base value, peak time, peak value, amplitude, large integrated value, right drive, and left drive, using a database of 30 years’ period in different climates of Iran. We used daily temperature data from 1989 to 2018 over Iran to extract the parameters by TIMESAT software. We studied the trend analysis of WSTP through the Mann–Kendall method. Then, we considered the Pearson correlation coefficient to calculate the correlation between WSTP and time. We assessed the trends of the slope using a simple linear regression method. Then, we compared the results of the WSTP trend analysis in climatic zones. Our results accused the hyper-arid climatic zone has the longest warm season (194.89 days a year). The warm season in this region starts earlier than other regions and increases with moderate speed (left drive, 0.19 °C day−1). Then, it reaches a peak value (31.3 °C) earlier than the different climatic zones. On the other hand, the humid regions’ warm season starts with the shortest length and ends later than the other climatic zones (112.1 and 297.5 days a year for start and end times, respectively). We detected that the trend of the start time parameter has decreased by 98.02% of the study area during the last 30 years. The base value, length, and large integrated value parameters have an increasing trend of 66.47%, 80.11%, and 92.95% in Iran. The highest correlation coefficient with time was for start time and large integrated value parameters. Hence, the start time and large integrated value parameters have almost the most negative (< − 0.5) and positive (> 5) trend slope, among other parameters, respectively. In general, these results demonstrate that the studied region has faced global warming impacts over time by increasing the warm season and thermal energy, especially in arid and hyper-arid. We highlight the necessity of planning the land use under the high natural vulnerability of the studied local, especially in this new age of global warming.Department of Arid and Mountainous Regions Reclamation Faculty of Natural Resources University of TehranDepartment of Environmental Engineering Institute of Sciences and Technology of Sorocaba São Paulo State University (UNESP)Department of Environmental Engineering Institute of Sciences and Technology of Sorocaba São Paulo State University (UNESP)University of TehranUniversidade Estadual Paulista (UNESP)Heydari Alamdarloo, EsmailMoradi, EhsanAbdolshahnejad, MahsaFatahi, YaldaKhosravi, Hassanda Silva, Alexandre Marco [UNESP]2022-04-29T08:36:22Z2022-04-29T08:36:22Z2021-12-01info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://dx.doi.org/10.1007/s10661-021-09600-2Environmental Monitoring and Assessment, v. 193, n. 12, 2021.1573-29590167-6369http://hdl.handle.net/11449/22988610.1007/s10661-021-09600-22-s2.0-85119072186Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengEnvironmental Monitoring and Assessmentinfo:eu-repo/semantics/openAccess2022-04-29T08:36:22Zoai:repositorio.unesp.br:11449/229886Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462024-08-05T23:06:02.162073Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv Analyzing WSTP trend: a new method for global warming assessment
title Analyzing WSTP trend: a new method for global warming assessment
spellingShingle Analyzing WSTP trend: a new method for global warming assessment
Heydari Alamdarloo, Esmail
Mann–Kendall
Pearson correlation coefficient
Simple linear regression
Spatial–temporal variations of WSTP
TIMESAT
title_short Analyzing WSTP trend: a new method for global warming assessment
title_full Analyzing WSTP trend: a new method for global warming assessment
title_fullStr Analyzing WSTP trend: a new method for global warming assessment
title_full_unstemmed Analyzing WSTP trend: a new method for global warming assessment
title_sort Analyzing WSTP trend: a new method for global warming assessment
author Heydari Alamdarloo, Esmail
author_facet Heydari Alamdarloo, Esmail
Moradi, Ehsan
Abdolshahnejad, Mahsa
Fatahi, Yalda
Khosravi, Hassan
da Silva, Alexandre Marco [UNESP]
author_role author
author2 Moradi, Ehsan
Abdolshahnejad, Mahsa
Fatahi, Yalda
Khosravi, Hassan
da Silva, Alexandre Marco [UNESP]
author2_role author
author
author
author
author
dc.contributor.none.fl_str_mv University of Tehran
Universidade Estadual Paulista (UNESP)
dc.contributor.author.fl_str_mv Heydari Alamdarloo, Esmail
Moradi, Ehsan
Abdolshahnejad, Mahsa
Fatahi, Yalda
Khosravi, Hassan
da Silva, Alexandre Marco [UNESP]
dc.subject.por.fl_str_mv Mann–Kendall
Pearson correlation coefficient
Simple linear regression
Spatial–temporal variations of WSTP
TIMESAT
topic Mann–Kendall
Pearson correlation coefficient
Simple linear regression
Spatial–temporal variations of WSTP
TIMESAT
description This paper tries to introduce a time-series of temperature parameters as a potential method for studying the global warming. So, we investigated the spatial–temporal variations of warm-season temperature parameters (WSTP), including start time, end time, length of season, base value, peak time, peak value, amplitude, large integrated value, right drive, and left drive, using a database of 30 years’ period in different climates of Iran. We used daily temperature data from 1989 to 2018 over Iran to extract the parameters by TIMESAT software. We studied the trend analysis of WSTP through the Mann–Kendall method. Then, we considered the Pearson correlation coefficient to calculate the correlation between WSTP and time. We assessed the trends of the slope using a simple linear regression method. Then, we compared the results of the WSTP trend analysis in climatic zones. Our results accused the hyper-arid climatic zone has the longest warm season (194.89 days a year). The warm season in this region starts earlier than other regions and increases with moderate speed (left drive, 0.19 °C day−1). Then, it reaches a peak value (31.3 °C) earlier than the different climatic zones. On the other hand, the humid regions’ warm season starts with the shortest length and ends later than the other climatic zones (112.1 and 297.5 days a year for start and end times, respectively). We detected that the trend of the start time parameter has decreased by 98.02% of the study area during the last 30 years. The base value, length, and large integrated value parameters have an increasing trend of 66.47%, 80.11%, and 92.95% in Iran. The highest correlation coefficient with time was for start time and large integrated value parameters. Hence, the start time and large integrated value parameters have almost the most negative (< − 0.5) and positive (> 5) trend slope, among other parameters, respectively. In general, these results demonstrate that the studied region has faced global warming impacts over time by increasing the warm season and thermal energy, especially in arid and hyper-arid. We highlight the necessity of planning the land use under the high natural vulnerability of the studied local, especially in this new age of global warming.
publishDate 2021
dc.date.none.fl_str_mv 2021-12-01
2022-04-29T08:36:22Z
2022-04-29T08:36:22Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://dx.doi.org/10.1007/s10661-021-09600-2
Environmental Monitoring and Assessment, v. 193, n. 12, 2021.
1573-2959
0167-6369
http://hdl.handle.net/11449/229886
10.1007/s10661-021-09600-2
2-s2.0-85119072186
url http://dx.doi.org/10.1007/s10661-021-09600-2
http://hdl.handle.net/11449/229886
identifier_str_mv Environmental Monitoring and Assessment, v. 193, n. 12, 2021.
1573-2959
0167-6369
10.1007/s10661-021-09600-2
2-s2.0-85119072186
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Environmental Monitoring and Assessment
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.source.none.fl_str_mv Scopus
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
instacron:UNESP
instname_str Universidade Estadual Paulista (UNESP)
instacron_str UNESP
institution UNESP
reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
repository.name.fl_str_mv Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)
repository.mail.fl_str_mv
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