Slow recovery of microclimate temperature buffering capacity after clear-cuts in boreal forests

• We compared microclimate buffering in even-aged and uneven-aged boreal forests. • Vertical structure was a strong driver of temperature buffering. • Both uneven-aged and even-aged forests buffered extreme temperatures. • Even-aged stands took on average 30 years to recover to pre-harvest buffering state. • Uneven-aged stands showed variable but consistent microclimate buffering. The majority of Fennoscandian boreal forests are managed. Forest management inherently changes the physical structure of forests, thus altering ecosystem functions and the conditions for living organisms within these environments. However, the impacts of management on the microclimate buffering of boreal forests have not been comprehensively studied, despite that microclimate is one of the key determinants of biodiversity. Here, we studied the effect of forest structure and management on the temperature buffering capacity of boreal forests using terrestrial laser scanning and microclimate measurements. We measured the temperature variability on forest plots representing two management types: even-aged rotation forestry and uneven-aged forestry. To quantify buffering, we calculated the slope coefficient of the linear regression between microclimate and clear-cut temperatures. We found that the total amount of plant material alone was not an adequate predictor of the buffering. Instead, increasing canopy layers and the density of the understory led to more buffered temperature variability compared to clear-cuts and forests with fewer layers. The buffering was high in both mature even-aged and uneven-aged sites, but the effect in even-aged forests depended on stand age, suggesting that a strong buffering capacity could be reached only after approximately 30 years after clear-cut. In uneven-aged stands, the buffering capacity varied with recurring partial selection cuttings, but never lead to a full coupling with open-air temperatures like in even-aged stands after clear-cuts. We conclude that despite the buffering being on average stronger in mature even-aged stands than in uneven-aged stands, it can take decades for a clear-cut stand to reach the same buffering capacity as an uneven-aged forest with continuous tree cover, and it will eventually disappear after a new clear-cut harvest. From biodiversity perspective, uneven-aged management can create more temporally stable microclimatic conditions and can thus aid in maintaining microrefugia and mitigate climate warming impacts.

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Publication Details

Journal
Agricultural and Forest Meteorology
Published
2025-02-06
DOI
https://doi.org/10.1016/j.agrformet.2025.110434
Citations
11
Primary Topic
Plant Water Relations and Carbon Dynamics
Type
article
Field-Weighted Citation Impact
12.16

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article

Slow recovery of microclimate temperature buffering capacity after clear-cuts in boreal forests

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11 citations
Agricultural and Forest Meteorology
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article

Slow recovery of microclimate temperature buffering capacity after clear-cuts in boreal forests

Iris Aalto, Eduardo Eiji Maeda, Sauli Valkonen, Juha Aalto, Steven Hancock, Leena Kalliovirta
article en
11 citations

Abstract

• We compared microclimate buffering in even-aged and uneven-aged boreal forests. • Vertical structure was a strong driver of temperature buffering. • Both uneven-aged and even-aged forests buffered extreme temperatures. • Even-aged stands took on average 30 years to recover to pre-harvest buffering state. • Uneven-aged stands showed variable but consistent microclimate buffering. The majority of Fennoscandian boreal forests are managed. Forest management inherently changes the physical structure of forests, thus altering ecosystem functions and the conditions for living organisms within these environments. However, the impacts of management on the microclimate buffering of boreal forests have not been comprehensively studied, despite that microclimate is one of the key determinants of biodiversity. Here, we studied the effect of forest structure and management on the temperature buffering capacity of boreal forests using terrestrial laser scanning and microclimate measurements. We measured the temperature variability on forest plots representing two management types: even-aged rotation forestry and uneven-aged forestry. To quantify buffering, we calculated the slope coefficient of the linear regression between microclimate and clear-cut temperatures. We found that the total amount of plant material alone was not an adequate predictor of the buffering. Instead, increasing canopy layers and the density of the understory led to more buffered temperature variability compared to clear-cuts and forests with fewer layers. The buffering was high in both mature even-aged and uneven-aged sites, but the effect in even-aged forests depended on stand age, suggesting that a strong buffering capacity could be reached only after approximately 30 years after clear-cut. In uneven-aged stands, the buffering capacity varied with recurring partial selection cuttings, but never lead to a full coupling with open-air temperatures like in even-aged stands after clear-cuts. We conclude that despite the buffering being on average stronger in mature even-aged stands than in uneven-aged stands, it can take decades for a clear-cut stand to reach the same buffering capacity as an uneven-aged forest with continuous tree cover, and it will eventually disappear after a new clear-cut harvest. From biodiversity perspective, uneven-aged management can create more temporally stable microclimatic conditions and can thus aid in maintaining microrefugia and mitigate climate warming impacts.

Agricultural and Forest MeteorologyVol. 363
Finnish Meteorological Institute (FI), University of Helsinki (FI), Helsinki Institute of Physics (FI), Natural Resources Institute Finland (FI), University of Edinburgh (GB)
Helsingin Yliopisto, Academy of Finland, Oskar Öflunds Stiftelse
Climate action
Openalex Percentile: Top 1%
Plant Water Relations and Carbon Dynamics
12.16
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