Resilience of subarctic Scots pine and Norway spruce forests to extreme weather events

• Published in: Agricultural and Forest Meteorology
• Main Authors: Matkala, Laura, Kulmala, Liisa, Kolari, Pasi, Aurela, Mika, Bäck, Jaana
• Other Authors: Department of Forest Sciences, Ecosystem processes (INAR Forest Sciences), Institute for Atmospheric and Earth System Research (INAR), Micrometeorology and biogeochemical cycles, INAR Physics, Viikki Plant Science Centre (ViPS), Forest Ecology and Management
• Format: Article in Journal/Newspaper
• Language: English
• Published: Elsevier Scientific Publ. Co 2021
• Subjects: 1172 Environmental sciences; 4112 Forestry; 1171 Geosciences; Extreme weather events; Eddy covariance; Scots pine; Norway spruce; Carbon; water; CARBON-DIOXIDE EXCHANGE; CLIMATE-CHANGE; SUMMER DROUGHT; HETEROTROPHIC RESPIRATION; TEMPERATURE SENSITIVITY; WHITE SPRUCE; GROWTH; IMPACTS; PHOTOSYNTHESIS; PRODUCTIVITY; Norway; Varrio; Arctic; Subarctic; Lapland
• Online Access: http://hdl.handle.net/10138/324089

We studied the occurrence of extreme weather events and their effects on the carbon dioxide and water exchange of two subarctic forest stands. One study site was a Scots pine site in eastern Finnish Lapland (VarriO), and the other was a Norway spruce site in western Finnish Lapland (Kenttarova). We compared short-term meteorological data with long-term data and found that the pine forest had experienced extremely warm, wet and dry years as well as cold spells during the growing season in the studied period of 2012-2018. The spruce forest was studied during the period 2003-2013, during which time it experienced extremely warm and wet summers, and dry periods, although the dry times were not statistically defined as such. The spruce forest was less resilient to warm and dry periods, as its total ecosystem respiration and respiration potential decreased during warm and dry summers, while the same effect was not seen in the pine forest. The decreased respiration values may have occurred due to slowed decomposition of organic matter. The pine forest experienced two cold spells during the studied period. One of these cold periods was more of a continuation of the previous cold spring and late start of the growing season in 2017, while the other one occurred after a warm period in 2014. The ecosystem respiration rates and gross primary production in 2017 remained low for the whole July-August time period likely due to cold-inhibited growth of ground vegetation, while in 2014 no such effect could be seen. We saw no effect of extreme weather events in the water exchange related measurements in either of the forests. Overall, both forests, especially the trees, were resilient to the weather extremes and experienced no long-term damage. Peer reviewed