Detection of temperature trends within the course of the year using “shifting subseasons”

Recent global warming has not been ubiquitous – there are seasons, regions, and time periods with clearly discernible zero or downward air temperature trends. Regions that are not warming or are even cooling – also known as “warming holes” – have been previously detected mainly in autumn in the seco...

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Main Authors: Cahynová, M. (Monika), Pokorná, L. (Lucie)
Format: Other/Unknown Material
Language:English
Published: 2015
Subjects:
Online Access:http://hdl.handle.net/11104/0247328
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spelling ftczacademyscien:oai:asep.lib.cas.cz:CavUnEpca/0444855 2024-09-15T18:14:34+00:00 Detection of temperature trends within the course of the year using “shifting subseasons” Cahynová, M. (Monika) Pokorná, L. (Lucie) 2015 http://hdl.handle.net/11104/0247328 eng eng urn:pissn: 1607-7962 http://hdl.handle.net/11104/0247328 info:eu-repo/semantics/other info:eu-repo/semantics/publishedVersion 2015 ftczacademyscien 2024-08-19T05:32:59Z Recent global warming has not been ubiquitous – there are seasons, regions, and time periods with clearly discernible zero or downward air temperature trends. Regions that are not warming or are even cooling – also known as “warming holes” – have been previously detected mainly in autumn in the second half of the 20th century in large parts of North America as well as in Central and Eastern Europe. Daily maximum and minimum temperature (TX and TN, respectively) and daily temperature range (DTR) at 136 stations in Europe during the period 1961– 2000 are employed to precisely locate the seasonal and subseasonal trends within the course of the year. Linear trends are calculated for moving “subseasons” of differing lengths (10, 20, 30, 60, and 90 days), each shifted by one day. Cluster analysis of the annual course of “shifting trends” reveals relatively well-defined regions with similar trend behavior. Over most of Europe, the observed warming is greatest in winter, and the highest trend magnitudes are reached by TN in Eastern Europe. Two regions stand out: in Iceland and the Eastern Mediterranean, the trends during the year are weak, positive in summer and mostly negative in winter, reaching statistical significance at only few stations. Significant autumn cooling centered on mid-November was found in Eastern and Southeastern Europe for both TX and TN; in many other regions trends are close to zero in the same period. Other clearly non-warming (or even cooling) periods occur in Western and Central Europe in February, April, and late June. Trends of DTR are largely inconclusive and no general picture can be drawn. Our results suggest that using different time scales, apart from the conventional three-month seasons or common months, is highly desirable for a proper location of trends within the course of the year. Other/Unknown Material Iceland The Czech Academy of Sciences: Publication Activity (ASEP)
institution Open Polar
collection The Czech Academy of Sciences: Publication Activity (ASEP)
op_collection_id ftczacademyscien
language English
description Recent global warming has not been ubiquitous – there are seasons, regions, and time periods with clearly discernible zero or downward air temperature trends. Regions that are not warming or are even cooling – also known as “warming holes” – have been previously detected mainly in autumn in the second half of the 20th century in large parts of North America as well as in Central and Eastern Europe. Daily maximum and minimum temperature (TX and TN, respectively) and daily temperature range (DTR) at 136 stations in Europe during the period 1961– 2000 are employed to precisely locate the seasonal and subseasonal trends within the course of the year. Linear trends are calculated for moving “subseasons” of differing lengths (10, 20, 30, 60, and 90 days), each shifted by one day. Cluster analysis of the annual course of “shifting trends” reveals relatively well-defined regions with similar trend behavior. Over most of Europe, the observed warming is greatest in winter, and the highest trend magnitudes are reached by TN in Eastern Europe. Two regions stand out: in Iceland and the Eastern Mediterranean, the trends during the year are weak, positive in summer and mostly negative in winter, reaching statistical significance at only few stations. Significant autumn cooling centered on mid-November was found in Eastern and Southeastern Europe for both TX and TN; in many other regions trends are close to zero in the same period. Other clearly non-warming (or even cooling) periods occur in Western and Central Europe in February, April, and late June. Trends of DTR are largely inconclusive and no general picture can be drawn. Our results suggest that using different time scales, apart from the conventional three-month seasons or common months, is highly desirable for a proper location of trends within the course of the year.
format Other/Unknown Material
author Cahynová, M. (Monika)
Pokorná, L. (Lucie)
spellingShingle Cahynová, M. (Monika)
Pokorná, L. (Lucie)
Detection of temperature trends within the course of the year using “shifting subseasons”
author_facet Cahynová, M. (Monika)
Pokorná, L. (Lucie)
author_sort Cahynová, M. (Monika)
title Detection of temperature trends within the course of the year using “shifting subseasons”
title_short Detection of temperature trends within the course of the year using “shifting subseasons”
title_full Detection of temperature trends within the course of the year using “shifting subseasons”
title_fullStr Detection of temperature trends within the course of the year using “shifting subseasons”
title_full_unstemmed Detection of temperature trends within the course of the year using “shifting subseasons”
title_sort detection of temperature trends within the course of the year using “shifting subseasons”
publishDate 2015
url http://hdl.handle.net/11104/0247328
genre Iceland
genre_facet Iceland
op_relation urn:pissn: 1607-7962
http://hdl.handle.net/11104/0247328
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