Forests: buffers for temperature in the future?

Even if you followed this webspace only occasionally, you should have gotten the idea of the fact that we are starting to get a good hold of microclimate across the globe. We know how much European forest understories differ from weather station temperatures, for example, or how much soils across the globe buffer temperature.

A very big black box, however, is how these microclimates will change in the future. When the climate warms, will forests buffer temperature more, or less? We now did a little first peek into that black box, in a paper just published in the STOTEN journal.

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Set-up of our analysis of future forest buffering. First, we used a database of temperatures measured inside and outside forests across the globe to calculate the ‘offset’ between the two. This offset was linked statistically to values of topography, tree cover, macroclimate and other things to predict the buffering effects of forests across the world. The statistical relationship with macroclimate could then be used to predict future buffering. Figure and rest of the story based on the Twitter thread by Pieter De Frenne

The result of the exercise as described above was pretty impressive: we project that temperatures within forests will warm slower by 0.3-0.6°C than outside forests by 2060-2080

Modelled mean annual offset in forests (red: forests warmer than the surrounding area; blue: forests are cooling) will turn more negative by 2060-2080.

To get to these results, we used a (freely available) global database of 714 paired temperature time series inside forests vs. in nearby open habitats. We then used past and future climate data, topography and forest cover, and height to model past and project future offsets between free-air temperature and sub-canopy microclimates.

Our projections have important implications for instance for forest management and the potential cooling of urban green areas and urban heat islands, as this suggests that forest microclimates will warm at a slower rate than open areas.

Important to note, however, is that we had to assume – for now – that forest cover remains the same over time. If large tree mortality would occur (as is already happening in many parts of the globe, among others due to climate change and drought), the buffering capacity of forests will decrease.

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Spruce dieback in Belgium

What happens to the microclimate in past and future if we take these land-use changes into account, that’s food for future research. But I promise you, we are not letting this rest, as getting the correct predictions of microclimate change are too important to ignore.

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