Long-term changes in forest response to extreme atmospheric dryness

© 2023 The Authors. Global Change Biology published by John Wiley & Sons Ltd.

Bibliographische Detailangaben
Veröffentlicht in:Global change biology. - 1999. - 29(2023), 18 vom: 11. Sept., Seite 5379-5396
1. Verfasser: Shekhar, Ankit (VerfasserIn)
Weitere Verfasser: Hörtnagl, Lukas, Buchmann, Nina, Gharun, Mana
Format: Online-Aufsatz
Sprache:English
Veröffentlicht: 2023
Zugriff auf das übergeordnete Werk:Global change biology
Schlagworte:Journal Article VPD eddy covariance net ecosystem productivity random forest recovery resistance
Beschreibung
Zusammenfassung:© 2023 The Authors. Global Change Biology published by John Wiley & Sons Ltd.
Atmospheric dryness, as indicated by vapor pressure deficit (VPD), has a strong influence on forest greenhouse gas exchange with the atmosphere. In this study, we used long-term (10-30 years) net ecosystem productivity (NEP) measurements from 60 forest sites across the world (1003 site-years) to quantify long-term changes in forest NEP resistance and NEP recovery in response to extreme atmospheric dryness. We tested two hypotheses: first, across sites differences in NEP resistance and NEP recovery of forests will depend on both the biophysical characteristics (i.e., leaf area index [LAI] and forest type) of the forest as well as on the local meteorological conditions of the site (i.e., mean VPD of the site), and second, forests experiencing an increasing trend in frequency and intensity of extreme dryness will show an increasing trend in NEP resistance and NEP recovery over time due to emergence of long-term ecological stress memory. We used a data-driven statistical learning approach to quantify NEP resistance and NEP recovery over multiple years. Our results showed that forest types, LAI, and median local VPD conditions explained over 50% of variance in both NEP resistance and NEP recovery, with drier sites showing higher NEP resistance and NEP recovery compared to sites with less atmospheric dryness. The impact of extreme atmospheric dryness events on NEP lasted for up to 3 days following most severe extreme events in most forests, indicated by an NEP recovery of less than 100%. We rejected our second hypothesis as we found no consistent relationship between trends of extreme VPD with trends in NEP resistance and NEP recovery across different forest sites, thus an increase in atmospheric dryness as it is predicted might not increase the resistance or recovery of forests in terms of NEP
Beschreibung:Date Completed 15.08.2023
Date Revised 26.01.2024
published: Print-Electronic
ErratumIn: Glob Chang Biol. 2024 Jan;30(1):e17062. doi: 10.1111/gcb.17062. - PMID 38273588
Citation Status MEDLINE
ISSN:1365-2486
DOI:10.1111/gcb.16846