Underestimation of the Tambora effects in North American taiga ecosystems
Datos Bibliográficos
| ID | 15546136 |
|---|---|
| Autores | Fabio Gennaretti (0000-0002-8232-023X, Centre National de la Recherche Scientifique, autor de correspondencia), Étienne Boucher (0000-0003-2299-5021, Université du Québec à Montréal), Antoine Nicault (Centre National de la Recherche Scientifique), Guillermo Gea‐Izquierdo (0000-0003-0148-3721), Guillermo Gea-Izquierdo, Dominique Arseneault (0000-0002-3419-2480, Université du Québec à Rimouski), Frank Berninger (0000-0001-7718-1661, University of Helsinki), Martine M Savard (0000-0002-1687-5448, Natural Resources Canada), Christian Bégin (Natural Resources Canada), Joël Guiot (0000-0001-7345-4466, Centre National de la Recherche Scientifique) |
| Año | 2018 |
| Volumen | 13 |
| Número | 3 |
| Páginas | 034017-034017 |
| Fecha de publicación | 2018-02-01 |
| Peer Reviewed | Sí |
| Open Access | Sí |
| Tipo | ARTICLE |
| Revista | Environmental Research Letters (JOURNAL) |
| Identificadores de la revista | ISSN: 1748-9326 • E-ISSN: 1748-9326 |
| Editorial | IOP Publishing (PUBLISHER • GB) |
| DOI | 10.1088/1748-9326/aaac0c |
| OpenAlex | W2788615691 |
| Idioma | EN |
| Referencias citadas | 56 |
The Tambora eruption (1815 AD) was one of the major eruptions of the last two millennia and has no equivalents over the last two centuries. Here, we collected an extensive network of early meteorological time series, climate simulation data and numerous, well-replicated proxy records from Eastern Canada to analyze the strength and the persistence of the Tambora impact on the regional climate and forest processes. Our results show that the Tambora impacts on the terrestrial biosphere were stronger than previously thought, and not only affected tree growth and carbon uptake for a longer period than registered in the regional climate, but also determined forest demography and structure. Increased tree mortality, four times higher than the background level, indicates that the Tambora climatic impact propagated to influence the structure of the North American taiga for several decades. We also show that the Tambora signal is more persistent in observed data (temperature, river ice dynamics, forest growth, tree mortality) than in simulated ones (climate and forest-growth simulations), indicating that our understanding of the mechanisms amplifying volcanic perturbations on climates and ecosystems is still limited, notably in the North American taiga
Biology · Biosphere · Climate change · Climatology · Ecosystem · Forest ecology · Geography · Physical geography · Proxy (statistics · Taiga · Volcano · Environmental Science · Geology and Paleoclimatology Research · Plant Water Relations and Carbon Dynamics · Tree-ring climate responses · Ecology · Forestry · Geology
Stable isotopes in tree rings
Carbon Isotope Discrimination and Photosynthesis
Timing and climate forcing of volcanic eruptions for the past 2,500 years
Tambora 1815 as a test case for high impact volcanic eruptions
Late-Holocene climatic changes as detected by the growth and decay of ice wedges on the southern shore of Hudson Strait, northern Québec, Canada
A Holocene paleoclimate reconstruction for eastern Canada based on δ 18 O cellulose of Sphagnum mosses from Mer Bleue Bog
| Velocidad de citación | historical |
|---|---|
| Altamente citado | No |