Asymmetry of day-to-day temperature changes and its causes
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68378289%3A_____%2F20%3A00538495" target="_blank" >RIV/68378289:_____/20:00538495 - isvavai.cz</a>
Alternative codes found
RIV/00216208:11310/20:10413113
Result on the web
<a href="https://link.springer.com/article/10.1007%2Fs00704-020-03116-4" target="_blank" >https://link.springer.com/article/10.1007%2Fs00704-020-03116-4</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s00704-020-03116-4" target="_blank" >10.1007/s00704-020-03116-4</a>
Alternative languages
Result language
angličtina
Original language name
Asymmetry of day-to-day temperature changes and its causes
Original language description
Previous studies indicate that the temperature changes from a day to the following day are not normally distributed either in winter or in summer. However, this study is the first to investigate the causes of the asymmetry in these temperature changes. We hypothesised that the asymmetries are driven by the passages of atmospheric fronts and by the radiative processes during anticyclonic circulation conditions. We used the maximum and minimum temperatures observed at the Praha-Karlov station, the records of front passages, and 7 different catalogues of circulation types over central Europe. We demonstrated that the asymmetries in the large temperature changes (5 degrees C and larger) were related to the passages of all three front types in winter and to the passages of cold fronts in summer. The asymmetries in the slight temperature changes (up to 3 degrees C) were mainly caused by cold advection from the north and the northeast in winter and by warm advection from the south, the southeast, and the east in summer. We suppose that our results can be generalized: that is, the passages of atmospheric fronts and cold/warm advection are the likely causes of the asymmetries of the day-to-day temperature changes elsewhere in Europe. The presented findings can be applied as a tool for the validation of climate model outputs.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10509 - Meteorology and atmospheric sciences
Result continuities
Project
<a href="/en/project/GA17-07043S" target="_blank" >GA17-07043S: Teleconnections - major building blocks of atmospheric circulation</a><br>
Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2020
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Theoretical and Applied Climatology
ISSN
0177-798X
e-ISSN
—
Volume of the periodical
140
Issue of the periodical within the volume
1-2
Country of publishing house
AT - AUSTRIA
Number of pages
8
Pages from-to
683-690
UT code for WoS article
000521505600047
EID of the result in the Scopus database
2-s2.0-85082633153