The emergence of snow droughts as drivers of negative extremes in plant productivity over the past decades
Rattachement africain : de, gb, ru. Niveau de preuve : code pays fourni par la source.
Le résumé fourni par la source
Abstract Hydroclimatic extremes such as droughts cause significant anomalies in the global carbon cycle, e.g. via reductions in ecosystem gross primary production (GPP), and hamper the storage capacity of the terrestrial carbon sink. At the same time, across snow covered ecosystems, plant-water availability is often dependent on the snowpack melt during spring and summer. Snow droughts, i.e. anomalous reductions in the amount of water stored in the snowpack, represent an emerging hydroclimatic extreme for these ecosystems. However, the role of snow droughts as drivers of carbon cycle anomalies remains largely unknown. In this study, we quantify the adverse impacts of snow droughts as drivers of negative GPP extreme events across the Northern Hemisphere (30–60° N) for the period 1982–2016. We attribute −4.48 PgC [−2.48 | −7.09 PgC] (mean [min|max] value across GPP datasets) of cumulative negative GPP anomalies to preceding snow droughts. They subsequently drive 23.5% [21.2 | 25.7%] of the negative GPP anomalies in the study region which corresponds to 9.6% [8.9 | 10.8%] of the global negative GPP anomalies. The attributable GPP anomalies show marked increases of +46.5% [+34.2 | +66.2%] in the recent study period (2000–2016 compared to 1982–1998). Particularly, more severe snow droughts act as drivers of negative GPP anomalies and lead to the most pronounced increases in anomalies between the two periods. Snow droughts act as isolated drivers for 15.9% [9.0 | 20.8%] of the cumulative negative GPP anomalies. Additionally, 30.7% [26.5 | 35.3%] of the negative GPP anomalies that were attributed to droughts occurring during a later stage of the growing season also reveal preceding snow droughts. Our study demonstrates the prominent role of snow droughts as drivers of negative GPP anomalies and subsequently impacting the carbon cycle, highlighting the importance of snow droughts in the context of advancing climate change.
Ce résumé expose les affirmations des auteurs. BNTIC ne l’interprète pas comme une validation indépendante des résultats.
Le contrôle bibliographique ouvert
DOI retrouvé dans Crossref DOI retrouvé ; titre concordant.
- Titre Crossref
- The emergence of snow droughts as drivers of negative extremes in plant productivity over the past decades
- Date Crossref
- 23/04/2026
- Éditeur
- IOP Publishing
- Type
- journal-article
Ce recoupement confirme des métadonnées liées au DOI. Il ne confirme ni la méthode ni les conclusions de l’étude, et il ne compte pas comme une seconde source scientifique indépendante.
Où se fait cette recherche
-
Ludwig-Maximilians-Universität München pays non établi dans la noticeUniversité ou école supérieure
-
University of Exeter Science and Economy pays non établi dans la noticeUniversité ou école supérieure
-
University of Augsburg Institute of Geography pays non établi dans la noticeUniversité ou école supérieure
-
V. B. Sochava Institute of Geography pays non établi dans la noticeStructure de recherche
-
BOKU University pays non établi dans la noticeUniversité ou école supérieure
Ludwig-Maximilians-Universität München, Science and Economy — University of Exeter et Institute of Geography — University of Augsburg, avec 2 autres affiliations.
Une affiliation ne permet pas de déduire la nationalité d’un auteur.