Changes and variability of spring-summer air temperature in Czechia during the past 300 years: comparison of instrumental, documentary and natural proxy data

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216224%3A14310%2F17%3A00112617" target="_blank" >RIV/00216224:14310/17:00112617 - isvavai.cz</a>

Alternative codes found

RIV/60162694:G43__/17:00534165

Result on the web

<a href="https://www.geografie.cz/archiv/stahnout/13" target="_blank" >https://www.geografie.cz/archiv/stahnout/13</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.37040/geografie2017122020190" target="_blank" >10.37040/geografie2017122020190</a>

Result language

čeština

Original language name

Změny a variabilita teploty vzduchu jarní a letní sezóny v Česku za posledních 300 let: porovnání přístrojových, dokumentárních a přírodních proxy dat

Original language description

Instrumental series, documentary and natural proxy air temperature reconstructions from the area of Czechia were employed to demonstrate spring/summer temporal variability and changes during the 1701-2010 period. Various statistical methods were applied to evaluate cold/warm periods, extreme seasons, oscillations and trends of individual series and also differences between them. Additional reconstructions from the Western and Central Europe were added to examine the role of geographical distance and type of climatological reconstruction. Instrumental series and documentary reconstructions agree well on the occurrence of cold/warm periods and extremes. There is a higher concentration of cold periods during the 18th and particularly 19th centuries. All of the series convincingly represent a positive temperature trend related to anthropogenic global warming. A tree-ring reconstruction contains a larger proportion of low-frequency signal. Despite spatial distance it has been recognized that an affinitive series such as tree-ring analyses from mountainous areas or reconstructions dealing with grape harvest-dates records share a vast extent of mutual variability.

Czech name

Změny a variabilita teploty vzduchu jarní a letní sezóny v Česku za posledních 300 let: porovnání přístrojových, dokumentárních a přírodních proxy dat

Czech description

Instrumental series, documentary and natural proxy air temperature reconstructions from the area of Czechia were employed to demonstrate spring/summer temporal variability and changes during the 1701-2010 period. Various statistical methods were applied to evaluate cold/warm periods, extreme seasons, oscillations and trends of individual series and also differences between them. Additional reconstructions from the Western and Central Europe were added to examine the role of geographical distance and type of climatological reconstruction. Instrumental series and documentary reconstructions agree well on the occurrence of cold/warm periods and extremes. There is a higher concentration of cold periods during the 18th and particularly 19th centuries. All of the series convincingly represent a positive temperature trend related to anthropogenic global warming. A tree-ring reconstruction contains a larger proportion of low-frequency signal. Despite spatial distance it has been recognized that an affinitive series such as tree-ring analyses from mountainous areas or reconstructions dealing with grape harvest-dates records share a vast extent of mutual variability.

Type

J_imp - Article in a specialist periodical, which is included in the Web of Science database

CEP classification

—

OECD FORD branch

10508 - Physical geography

Project

—

Continuities

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year

2017

Confidentiality

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Name of the periodical

Geografie

ISSN

1212-0014

e-ISSN

—

Volume of the periodical

122

Issue of the periodical within the volume

2

Country of publishing house

CZ - CZECH REPUBLIC

Number of pages

23

Pages from-to

190-212

UT code for WoS article

000404784100004

EID of the result in the Scopus database

2-s2.0-85032295457