Predicted sea-ice loss will terminate Iceland's driftwood supply by 2060 CE
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F22%3A00558440" target="_blank" >RIV/86652079:_____/22:00558440 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/62156489:43410/22:43921411 RIV/00216224:14310/22:00126061
Výsledek na webu
<a href="https://www.sciencedirect.com/science/article/pii/S0921818122001011?via%3Dihub#" target="_blank" >https://www.sciencedirect.com/science/article/pii/S0921818122001011?via%3Dihub#</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.gloplacha.2022.103834" target="_blank" >10.1016/j.gloplacha.2022.103834</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Predicted sea-ice loss will terminate Iceland's driftwood supply by 2060 CE
Popis výsledku v původním jazyce
Driftwood supply was a pivotal factor for the Norse expansion in medieval times and still exhibits an essential resource for Arctic settlements. The physical causes and societal consequences of long-term changes in the distribution of Arctic driftwood are, however, poorly understood. Here, we use dendrochronology to reconstruct the age and origin of 289 driftwood samples that were collected at remote shorelines in northeast Iceland. Based on 240 reference tree-ring width chronologies from the boreal forest zone, and an overall provenance success of 73%, we show that most of the driftwood is pine and larch from the Yenisei catchment in central Siberia. Our study reveals an abrupt decline in the amount of driftwood reaching Iceland since the 1980s, which is corroborated by the experience of local farmers and fishers. Despite the direct and indirect effects of changes in both, logging activity across Siberia as well as Arctic Ocean currents, the predicted amount of sea-ice loss under anthropogenic global warming is likely to terminate Iceland's driftwood supply by 2060 CE.
Název v anglickém jazyce
Predicted sea-ice loss will terminate Iceland's driftwood supply by 2060 CE
Popis výsledku anglicky
Driftwood supply was a pivotal factor for the Norse expansion in medieval times and still exhibits an essential resource for Arctic settlements. The physical causes and societal consequences of long-term changes in the distribution of Arctic driftwood are, however, poorly understood. Here, we use dendrochronology to reconstruct the age and origin of 289 driftwood samples that were collected at remote shorelines in northeast Iceland. Based on 240 reference tree-ring width chronologies from the boreal forest zone, and an overall provenance success of 73%, we show that most of the driftwood is pine and larch from the Yenisei catchment in central Siberia. Our study reveals an abrupt decline in the amount of driftwood reaching Iceland since the 1980s, which is corroborated by the experience of local farmers and fishers. Despite the direct and indirect effects of changes in both, logging activity across Siberia as well as Arctic Ocean currents, the predicted amount of sea-ice loss under anthropogenic global warming is likely to terminate Iceland's driftwood supply by 2060 CE.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10510 - Climatic research
Návaznosti výsledku
Projekt
<a href="/cs/project/EF16_019%2F0000797" target="_blank" >EF16_019/0000797: SustES - Adaptační strategie pro udržitelnost ekosystémových služeb a potravinové bezpečnosti v nepříznivých přírodních podmínkách</a><br>
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2022
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Global and Planetary Change
ISSN
0921-8181
e-ISSN
1872-6364
Svazek periodika
213
Číslo periodika v rámci svazku
JUN
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
8
Strana od-do
103834
Kód UT WoS článku
000800553100004
EID výsledku v databázi Scopus
2-s2.0-85129512466