Annual cycle of temperature trends in Europe, 1961-2000

0521365 - ÚVGZ 2020 RIV NL eng J - Článek v odborném periodiku
Pokorná, Lucie - Kučerová, Monika - Huth, Radan
Annual cycle of temperature trends in Europe, 1961-2000.
Global and Planetary Change. Roč. 170, NOV 2018 (2018), s. 146-162. ISSN 0921-8181. E-ISSN 1872-6364
Institucionální podpora: RVO:86652079 ; RVO:68378289
Klíčová slova: surface air-temperature * minimum daily temperatures * warming hole * north-atlantic * united-states * precipitation trends * western-europe * climate trends * maximum * variability * Climate change * Maximum temperature * Minimum temperature * Temperature trend * Annual cycle * Europe
Obor OECD: Meteorology and atmospheric sciences; Meteorology and atmospheric sciences (UFA-U)
Impakt faktor: 4.100, rok: 2018
Způsob publikování: Open access s časovým embargem
https://www.sciencedirect.com/science/article/pii/S0921818117306677?via%3Dihub

Recent global warming has not been ubiquitous: there are seasons, regions, and time periods with negligible or even negative air temperature trends (frequently referred to as warming holes). This paper presents a novel method enabling a proper localization of specific trend events, such as periods of warming holes, of a particularly strong warming, and of rapid transitions of trend amplitudes during the calendar year. The method consists in analyzing trends for periods of a given length (10 to 90 days) that are sliding over the year with a one day step. This allows a detailed description of the annual cycle of trends. The analysis is conducted for daily maximum and minimum temperature at 135 stations in Europe in 1961-2000. Despite an overall warming in Europe, several warming holes are uncovered during various parts of the year, not only in autumn when a warming hole has already been reported. The autumn warming hole concentrates in Eastern Europe, but it changes its strength and spatial extent: it spreads into Western Europe in September and retreats to Eastern Europe in November when it intensifies especially north of the Black Sea. Three shorter warming holes are detected: In February and March, cooling occurs in the Eastern Mediterranean and Iceland, while in early April, cooling is detected over Central, Southern, and Southeastern Europe. Another large-scale cooling occurs in Central, Northern, and Northwestern Europe in mid-June. The periods of strongest warming occur around the middle of January in Eastern Europe, in early March over almost entire Europe, and in mid-May and early August mainly over Central and Western Europe. Cluster analysis of stations with respect to the annual cycles of trends demonstrates a spatial coherence of the trends, the lack of spatial coherence points to local peculiarities or data problems of individual stations. The method of sliding seasons proves to be much more effective in the identification and localization of notable trend events than the ordinary approach of trend detection for fixed calendar seasons and/or months.
Trvalý link: http://hdl.handle.net/11104/0305995