Linking two centuries of tree growth and glacier dynamics with climate changes in Kamchatka

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12310%2F14%3A43887174" target="_blank" >RIV/60076658:12310/14:43887174 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/67985939:_____/14:00432302

Výsledek na webu

<a href="http://download.springer.com/static/pdf/783/art%253A10.1007%252Fs10584-014-1093-4.pdf?auth66=1422218694_9ed504a21ad7941edc1abbd1ffe733ac&ext=.pdf" target="_blank" >http://download.springer.com/static/pdf/783/art%253A10.1007%252Fs10584-014-1093-4.pdf?auth66=1422218694_9ed504a21ad7941edc1abbd1ffe733ac&ext=.pdf</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.1007/s10584-014-1093-4" target="_blank" >10.1007/s10584-014-1093-4</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Linking two centuries of tree growth and glacier dynamics with climate changes in Kamchatka

Popis výsledku v původním jazyce

Glaciers around the world retreated as the climate warmed substantially. For the majority of alpine and arctic areas, however, the lack of meteorological data over a long period makes it difficult to build long-term climate and glacial fluctuation relationships, emphasizing the importance of natural proxy archives. Here we use the 230-year record of stem radial growth of birch trees (Betula ermanii) from the treeline forests above the receding glaciers in eastern maritime Kamchatka to analyse temporal variations of climate as well as glacial advance and retreat. Glaciers in Kamchatka Peninsula represent the southern limit of glaciation in far eastern Eurasia, which makes them prone to global warming. Using instrumental climate data (1930-1996) from local meteorological stations, we find that the July temperature had most prominent positive impact on birch growth. On the contrary, smaller ring increments are associated with the positive summer and net annual ice mass balance of Koryto G

Název v anglickém jazyce

Linking two centuries of tree growth and glacier dynamics with climate changes in Kamchatka

Popis výsledku anglicky

Glaciers around the world retreated as the climate warmed substantially. For the majority of alpine and arctic areas, however, the lack of meteorological data over a long period makes it difficult to build long-term climate and glacial fluctuation relationships, emphasizing the importance of natural proxy archives. Here we use the 230-year record of stem radial growth of birch trees (Betula ermanii) from the treeline forests above the receding glaciers in eastern maritime Kamchatka to analyse temporal variations of climate as well as glacial advance and retreat. Glaciers in Kamchatka Peninsula represent the southern limit of glaciation in far eastern Eurasia, which makes them prone to global warming. Using instrumental climate data (1930-1996) from local meteorological stations, we find that the July temperature had most prominent positive impact on birch growth. On the contrary, smaller ring increments are associated with the positive summer and net annual ice mass balance of Koryto G

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

EH - Ekologie – společenstva

OECD FORD obor

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Projekt

<a href="/cs/project/GA13-13368S" target="_blank" >GA13-13368S: Změny rostlinné diverzity v důsledku oteplování: od regionální flory k stanovištním adaptacím a funkční diverzitě</a><br>

Návaznosti

S - Specificky vyzkum na vysokych skolach

Rok uplatnění

2014

Kód důvěrnosti údajů

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

Název periodika

CLIMATIC CHANGE

ISSN

0165-0009

e-ISSN

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Svazek periodika

124

Číslo periodika v rámci svazku

1-2

Stát vydavatele periodika

NL - Nizozemsko

Počet stran výsledku

14

Strana od-do

207-220

Kód UT WoS článku

000336365300016

EID výsledku v databázi Scopus

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