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Forest Science Database

Supporting your research in forest and wood science

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Abstract

The evolution of a debris-flow cone depends on a multitude of factors in the hydrogeomorphic system. Investigations of debris-flow history and cone dynamics in highly active catchments therefore require an integrative approach with a temporal and spatial resolution appropriate for the goals of the...

Author(s)
Procter, E.; Stoffel, M.; Schneuwly-Bollschweiler, M.; Neumann, M.
Publisher
Wiley-Blackwell, Chichester, UK
Citation
Earth Surface Processes and Landforms, 2012, 37, 9, pp 913-922
Abstract

Annually resolved and absolutely dated tree-ring chronologies are the most important proxy archives to reconstruct climate variability over centuries to millennia. However, the suitability of tree-ring chronologies to reflect the "true" spectral properties of past changes in temperature and...

Author(s)
Büntgen, U.; Trnka, M.; Krusic, P. J.; Kyncl, T.; Kyncl, J.; Luterbacher, J.; Zorita, E.; Ljungqvist, F. C.; Auer, I.; Konter, O.; Schneider, L.; Tegel, W.; Štěpánek, P.; Brönnimann, S.; Hellmann, L.; Nievergelt, D.; Esper, J.
Publisher
American Meteorological Society, Boston, USA
Citation
Journal of Climate, 2015, 28, 13, pp 5272-5288
Abstract

An ultra-long tree-ring width chronology (9111 years long, 7109 BC to AD 2002) has been established based on the analysis and dating of 1432 subfossil/dry dead wood samples and cores from 335 living trees. The material was collected from treeline or near-treeline sites (c. 2000 to 2400 m a.s.l.)...

Author(s)
Nicolussi, K.; Kaufmann, M.; Melvin, T. M.; Plicht, J. van der; Schiessling, P.; Thurner, A.
Publisher
Sage Publications Ltd, London, UK
Citation
Holocene, 2009, 19, 6, pp 909-920

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