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Beyond maximum density: multi-parameter insights into Scots pine climate sensitivity
Inga K Homfeld1, Frederick Reinig1, Edurne Martinez Del Castillo1
1Department of Geography, Johannes Gutenberg University, 55099 Mainz, Germany.
Summary
Climate sensitivity in Scots pine (Pinus sylvestris) has shifted, particularly in minimum density, impacting dendroclimatology. This study explores tree-ring density parameters to better understand climate change responses.
Area of Science:
- Dendrochronology and Climate Science
- Ecology and Evolutionary Biology
- Forestry and Environmental Science
Background:
- Pinus sylvestris L. is a key species for Eurasian dendroclimatological reconstructions.
- Traditional methods rely on tree-ring width (TRW) and maximum latewood density (MXD).
- Climatic signals from earlywood/latewood density (EWD/LWD) and minimum density (MND) are under-explored.
Purpose of the Study:
- To investigate the climate change response of multiple P. sylvestris tree-ring parameters.
- To compare these responses at two contrasting sites in Scotland and Sweden.
- To assess the skill of EWD/LWD and MND in dendroclimatological reconstructions.
Main Methods:
- Analysis of well-replicated tree-ring density data from Scotland and Sweden.
- Correlation analysis between tree-ring parameters (LWD, MXD, MND) and temperature data.
- Investigation of temporal changes in climate-growth relationships.
Main Results:
- LWD and MXD showed strongest correlations with temperature (0.5–0.7) for July, August, and the June-August season.
- A significant negative correlation between MND and July temperatures was found in Swedish data, diminishing since the late 20th century.
- Northern Scotland's site showed no comparable inverse MND-temperature signal, suggesting site-specific physiological changes.
Conclusions:
- Climate sensitivity of P. sylvestris has changed, with shifts in minimum density.
- The stability of MXD contrasts with changes in MND, highlighting the need for additional density parameters.
- Altered tree growth sensitivity may reduce the effectiveness of proxies from northern European sites for climate reconstructions.
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