Differences in wind speeds according to measured and homogenized series in the Czech Republic, 1961-2015
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F19%3A00504652" target="_blank" >RIV/86652079:_____/19:00504652 - isvavai.cz</a>
Alternative codes found
RIV/00020699:_____/18:N0000111 RIV/00216224:14310/19:00107175
Result on the web
<a href="https://rmets.onlinelibrary.wiley.com/doi/epdf/10.1002/joc.5800" target="_blank" >https://rmets.onlinelibrary.wiley.com/doi/epdf/10.1002/joc.5800</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1002/joc.5800" target="_blank" >10.1002/joc.5800</a>
Alternative languages
Result language
angličtina
Original language name
Differences in wind speeds according to measured and homogenized series in the Czech Republic, 1961-2015
Original language description
Non-meteorological factors may bias wind speed measurements in a number of ways, among them the types of instruments used, their calibration and standards of maintenance, station relocations, and changes in the physical surroundings of a given station. Moreover, homogenisation of series of such measurements is more complicated than that of other climatic variables. This contribution uses figures from the Czech Republic as an example to demonstrate that measured (raw) data may produce different results in mean daily wind speeds from those acquired in homogenous series. A basic set of measurements taken in 1961-2015 at 178 meteorological stations was quality-checked and then homogenized using the Standard Normal Homogeneity test (SNHT) and the Maronna-Yohai test. Subsequent analyses were based on homogenized series from 119 stations. Station relocations and automation of wind speed measurements were identified as the most important sources of break-points in series of mean daily wind speeds. Generally lower mean wind speeds (as well as wind speed variability) were obtained from homogenous series in comparison with measured data, with reflections also found in their spatial distribution around the territory of the Czech Republic. Statistically significant decreasing linear trends calculated from measured and homogenized daily wind speed series from 119 stations confirm the existence of wind stilling as a typical feature of land mid-latitudes in recent decades. However, trends from measured data are highly overestimated compared with those from homogenized series.
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/LO1415" target="_blank" >LO1415: CzechGlobe 2020 – Development of the Centre of Global Climate Change Impacts Studies</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2019
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
International Journal of Climatology
ISSN
0899-8418
e-ISSN
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Volume of the periodical
39
Issue of the periodical within the volume
1
Country of publishing house
US - UNITED STATES
Number of pages
16
Pages from-to
235-250
UT code for WoS article
000459638400018
EID of the result in the Scopus database
2-s2.0-85052918622