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Tree rings and climate in Scandinavia and Southern Patagonia


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Title: Tree rings and climate in Scandinavia and Southern Patagonia
Authors: Fuentes, Mauricio
E-mail: mauricio.fuentes@gu.se
Issue Date: 30-Nov-2017
University: Göteborgs universitet. Naturvetenskapliga fakulteten
Institution: Department of Earth Sciences ; Institutionen för geovetenskaper
Parts of work: Fuentes, M., et al. 2017: A 970 year-long summer temperature reconstruction from Rogen, west entral Sweden, based on Blue Intensity from tree rings. The Holocene
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Linderholm H.W.,et al. 2015:Fennoscandia revisited: A spatially improved tree-ring reconstruction of summer temperatures for the last 900 years. Climate Dynamics 45: 933-947.
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Linderholm, H.W. et al., 2014: Growth dynamics of tree-line and lake-shore Scots pine (Pinus sylvestris L.) in the central Scandinavian Mountains during the Medieval Climate Anomaly and the early Little Ice Age. Frontiers in Ecology and Evolution 2: 20.
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Fuentes M.,et al.,(in review) Assessing the dendroclimatic potential of Magellan's beech (Nothofagus betuloides) in the southernmost Patagonian Archipelago. Trees (in review)

Fuentes et al. (Manuscript) Climate sensitivity of Nothofagus betuloides (Mirb) Oerst and Pilgerodendron uviferum (D.Don) Florin; growing in the southernmost forest in the world: the signal of the Southern Annular Mode, the Southern Osculation Index and large scale spatial patterns from the Southern Pacific.
Date of Defence: 2017-12-20
Disputation: December 20, 2017. Stora hörsalen Geovetarcentrum Guldhedsgatan 5a 405 30 Göteborg
Degree: Doctor of Philosophy
Publication type: Doctoral thesis
Keywords: Tree-rings
Pinus sylvestris
Fennoscandia
Atlantic Multidecadal Oscillation
Scandinavian Pattern
Patagonia
Nothofagus betuloides
Pilgerodendron uviferum
Temperature
Precipitation
Southern Annular Mode
Southern Oscillation
Amundsen lows
Sea Level Pressure
Sea Surface Temperature
Southern Pacific
Abstract: The present knowledge of temperature variability during the past millennium has been greatly improved due to an increasing availability of reconstructions made based on paleoclimate proxies, such as tree-rings. These improvements however, do not suffice to provide a coherent representation of the past climate at local to regional scale at higher latitudes. The reasons, are mainly due to the poor spatial density of the networks and the little understanding of how microsite variability affect... more
ISBN: 978-91-629-0385-5
978-91-629-0384-8
URI: http://hdl.handle.net/2077/53971
Appears in Collections:Doctoral Theses from University of Gothenburg / Doktorsavhandlingar från Göteborgs universitet
Doctoral Theses / Doktorsavhandlingar Institutionen för geovetenskaper

 

 

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