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

Kód výsledku v 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>

Nalezeny alternativní kódy

RIV/60162694:G43__/17:00534165

Výsledek na webu

<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>

Jazyk výsledku

čeština

Název v původním jazyce

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

Popis výsledku v původním jazyce

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.

Název v anglickém jazyce

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

Popis výsledku anglicky

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.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10508 - Physical geography

Projekt

—

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2017

Kód důvěrnosti údajů

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

Název periodika

Geografie

ISSN

1212-0014

e-ISSN

—

Svazek periodika

122

Číslo periodika v rámci svazku

2

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

23

Strana od-do

190-212

Kód UT WoS článku

000404784100004

EID výsledku v databázi Scopus

2-s2.0-85032295457