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Deforestation reduces microclimate buffering of African montane forests

Titelangaben

Abera, Temesgen Alemayehu ; Maeda, Eduardo Eiji ; Heiskanen, Janne ; Wöllauer, Stephan ; Alibakhshi, Sara ; Pellikka, Petri ; Hemp, Andreas ; Moradi, Ayoub ; Hailu, Binyam Tesfaw ; Muhammed, Mohammed Ahmed ; Zeuss, Dirk:
Deforestation reduces microclimate buffering of African montane forests.
In: Communications Earth & Environment. Bd. 6 (2025) . - 877.
ISSN 2662-4435
DOI: https://doi.org/10.1038/s43247-025-02950-6

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Link zum Volltext (externe URL): Volltext

Angaben zu Projekten

Projekttitel:
Offizieller Projekttitel
Projekt-ID
Rückkopplungen zwischen Vegetation und Mikroklima im Kontext von Waldstörungen, Bewirtschaftung und Klimawandel im östlichen afromontanen Biodiversitätshotspot: Auswirkungen auf klimatische Mikrorefugien und Artenverbreitung in Afrika
560330469

Projektfinanzierung: Deutsche Forschungsgemeinschaft

Abstract

Montane forests are biodiversity hotspots that provide important ecosystem services, including temperature buffering for numerous species underneath forest canopies. In recent decades, montane forests have been under increasing pressure from small-and large-scale deforestation, yet associated spatio-temporal changes in temperature buffering capacity remain unclear. Here, we studied the changes in temperature buffering capacity due to forest loss from 2003 to 2022 in three montane forest ecosystems in Africa (Mount Kilimanjaro, Mount Bale, and the Taita Hills). We modeled the temperature buffering changes based on in situ microclimate measurements inside forests and in open areas, climate data, airborne laser scanning data, and satellite observations. We found that during the study period montane forests were lost at a rate of 2–9% across the study areas. This loss led to an annual average microclimate air temperature warming ranging from 2.0 ± 0.8 °C to 5.6 ± 2.1 °C across the three montane forests. The warming reduced the maximum air temperature buffering by an average of 3 ± 1.5 °C. Locally, the temperature buffering disappeared over time and transitioned to a mesoclimate amplification. Our findings demonstrate that microclimate buffering capacity was markedly diminished as a result of microclimate warming driven by recent forest loss.

Weitere Angaben

Publikationsform: Artikel in einer Zeitschrift
Begutachteter Beitrag: Ja
Institutionen der Universität: Fakultäten > Fakultät für Biologie, Chemie und Geowissenschaften > Fachgruppe Biologie > Lehrstuhl Pflanzensystematik
Forschungseinrichtungen > Zentrale wissenschaftliche Einrichtungen > Bayreuther Zentrum für Ökologie und Umweltforschung - BayCEER
Titel an der UBT entstanden: Ja
Themengebiete aus DDC: 500 Naturwissenschaften und Mathematik > 580 Pflanzen (Botanik)
Eingestellt am: 27 Mai 2026 12:03
Letzte Änderung: 27 Mai 2026 12:03
URI: https://eref.uni-bayreuth.de/id/eprint/97739