Growth variability of Scots pine (Pinus sylvestris) along a West-East gradient across northern Fennoscandia: a dendroclimatic approach

• Main Authors: Macias, Marc, Timonen, Mauri, Kirchhefer, Andreas J., Lindholm, Markus, Eronen, Matti, Gutiérrez Merino, Emilia
• Format: Article in Journal/Newspaper
• Language: English
• Published: University of Colorado 2004
• Subjects: Pins; Creixement (Plantes); Dendrocronologia; Europa del Nord; Pine; Growth (Plants); Dendrochronology; Northern Europe; Antarctic and Alpine Research; Arctic; Fennoscandia; North Atlantic; North Atlantic oscillation
• Online Access: http://hdl.handle.net/2445/55849

We performed a spatiotemporal analysis of a network of 21 Scots pine (Pinus sylvestris) ring-width chronologies in northern Fennoscandia by means of chronology statistics and multivariate analyses. Chronologies are located on both sides (western and eastern) of the Scandes Mountains (67°N-70°N, 15°E-29°E). Growth relationships with temperature, precipitation, and North Atlantic Oscillation (NAO) indices were calculated for the period 1880-1991. We also assessed their temporal stability. Current July temperature and, to a lesser degree, May precipitation are the main growth limiting factors in the whole area of study. However, Principal Component Analysis (PCA) and mean interseries correlation revealed differences in radial growth between both sides of the Scandes Mountains, attributed to the Oceanic-Continental climatic gradient in the area. The gradient signal is temporally variable and has strengthened during the second half of the 20th century. Northern Fennoscandia Scots pine growth is positively related to early winter NAO indices previous to the growth season and to late spring NAO. NAO/growth relationships are unstable and have dropped in the second half of the 20th century. Moreover, they are noncontinuous through the range of NAO values: for early winter, only positive NAO indices enhance tree growth in the next growing season, while negative NAO does not. For spring, only negative NAO is correlated with radial growth.