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Continuous increase in evaporative demand shortened the growing season of European ecosystems in the last decade

Earth Sciences

Continuous increase in evaporative demand shortened the growing season of European ecosystems in the last decade

M. Rahmati, A. Graf, et al.

Recent research by Mehdi Rahmati and colleagues reveals a surprising reversal in the length of European growing seasons, potentially challenging our understanding of climate impacts. While early greening continues, trends indicate a shortening of the season back to levels not seen since the 1980s, primarily due to increased atmospheric water demands in summer. Discover the implications for ecosystem management in this cutting-edge study.

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~3 min • Beginner • English
Abstract
Despite previous reports on European growing seasons lengthening due to global warming, evidence shows that this trend has been reversing in the past decade due to increased transpiration needs. To asses this, we used an innovative method along with space-based observations to determine the timing of greening and dormancy and then to determine existing trends of them and causes. Early greening still occurs, albeit at slower rates than before. However, a recent (2011–2020) shift in the timing of dormancy has caused the season length to decrease back to 1980s levels. This shortening of season length is attributed primarily to higher atmospheric water demand in summer that suppresses transpiration even for soil moisture levels as of previous years. Transpiration suppression implies that vegetation is unable to meet the high transpiration needs. Our results have implications for future management of European ecosystems (e.g., net carbon balance and water and energy exchange with atmosphere) in a warmer world.
Publisher
Communications Earth & Environment
Published On
Jul 03, 2023
Authors
Mehdi Rahmati, Alexander Graf, Christian Poppe Terán, Wulf Amelung, Wouter Dorigo, Harrie-Jan Hendricks Franssen, Carsten Montzka, Dani Or, Matthias Sprenger, Jan Vanderborght, Niko E. C. Verhoest, Harry Vereecken
Tags
growing season
climate change
transpiration
European ecosystems
season length
dormancy timing
atmospheric water demand
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