Acknowledgements: This study was supported by the Estonian Ministry of Education and Research (project SF0170014s08), Estonian Science Foundation (Grant 8890), Järvseja Training and Experimental Forest Centre, Estonian Environmental Investment Centre, Estonian University of Life Sciences ASTRA project “Value-chain based bio-economy” (supported by the European Union, European Regional Development Fund). CG received funding from Natural Environment Research Council—United Kingdom Research and Innovation. UB received funding from the SustES project—Adaptation strategies for sustainable ecosystem services and food security under adverse environmental conditions (CZ.02.1.01/0.0/0.0/16_019/0000797), and the ERC Advanced project Monostar (AdG 882727). S.M received funding from the Estonian University of Life Sciences project P200189MIMP.Funder: European UnionFunder: European Regional Development FundFunder: Natural Environment Research Council; doi: http://dx.doi.org/10.13039/501100000270Abstract
Key message
An exceptionally high number of blue rings were formed within and between Scots pine trees from Estonia in 1976: a year that is well known for its outstanding summer heatwave over Western Europe, but its extreme autumnal cooling over Eastern Europe has so far been neglected in scientific literature.
Abstract
‘Blue rings’ (BRs) are visual indicators of less lignified cell walls typically formed towards the end of a tree’s growing season. Though BRs have been associated with ephemeral surface cooling, often following large volcanic eruptions, the intensity of cold spells necessary to produce BRs, as well as the consistency of their formation within and between trees still remains uncertain. Here, we report an exceptionally high BR occurrence within and between Scots pine (Pinus sylvestris L.) trees at two sites in Estonia, including the first published whole-stem analysis for BRs. Daily meteorological measurements from a nearby station allowed us to investigate the role temperature has played in BR formation since the beginning of the twentieth century. The single year in which BRs were consistently formed within and amongst most trees was 1976. While the summer of 1976 is well known for an exceptional heatwave in Northwest Europe, mean September and October temperatures were remarkably low over Eastern Europe, and 3.8 °C below the 1961–1990 mean at our sites. Our findings contribute to a better eco-physiological interpretation of BRs, and further demonstrate their ability to reveal ephemeral cooling not captured by dendrochronological ring width and latewood density measurements.
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