Atmospheric jet stream variability reflects vegetation activity in Europe

Gabriele Messori, Minchao Wu, Giulia Vico, Vera Melinda Galfi

Research output: Contribution to JournalArticleAcademicpeer-review

Abstract

Jet streams are a key component of the climate system, whose dynamics couple closely to regional climate variability. Yet, the link between jet stream variability and vegetation activity has received little attention. Here, we leverage our understanding of the mid-latitude jet stream dynamics over the Euro-Atlantic sector to probe climate–vegetation interactions across Europe. We link indices related to the meridional location of the jet and the large-scale zonal wind speed with remotely-sensed vegetation greenness anomalies during locally-defined growing seasons. Correlations between greenness anomalies and jet latitude anomalies point to a control of the jet stream's variability on vegetation activity over large parts of Europe. This potential control is mediated by the jet latitude anomalies’ correlations with temperature, soil moisture and downward surface solar radiation. The sign and strength of these correlations depend on location and time of the year. Furthermore, jet stream variability modulates conditions at the onset and end of the growing season. The link between jet latitude anomalies and vegetation greenness is not only specific to the climate zone, but also to the landclass and subperiod within the growing season. It is thus important to use a locally-defined growing season for interpreting the atmospheric controls on regional vegetation phenology. Results consistent with the correlation analysis emerge when focussing on local high or low greenness months only or on zonal wind speed anomalies, confirming the relevance of jet variability for vegetation activity.
Original languageEnglish
Article number109008
JournalAgricultural and Forest Meteorology
Volume322
DOIs
Publication statusPublished - 15 Jul 2022
Externally publishedYes

Funding

G. Messori, M. Wu and G. Vico acknowledge the support of the Swedish Research Council FORMAS (Grant No. 2018-00968). G. Messori additionally acknowledges funding from the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation programme (Grant agreement No. 948309, CENÆ Project). G. Vico additionally acknowledges the European Commission and the Swedish Research Council FORMAS (Grant No. 2018-02787) for funding in the frame of the collaborative international consortium iAqueduct financed under the 2018 Joint call of the WaterWorks 2017 ERA-NET Cofund. This ERA-NET is an integral part of the activities developed by the Water JPI. M. Galfi acknowledges the support of the Air, Water and Landscape Science research programme at the Dept. of Earth Sciences, Uppsala University. All authors would like to thank S. Manzoni and two anonymous reviewers for constructive feedback on the manuscript.

FundersFunder number
Dept. of Earth Sciences
European Commission2018-02787
European Research Council
Svenska Forskningsrådet Formas2018-00968
Uppsala Universitet
Horizon 2020948309

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