EconPapers    
Economics at your fingertips  
 

Monsoon-driven teleconnections between Holocene fire activity in Central Asian and Neotropical ecosystems

Sandra O. Camara-Brugger (), Heinz Wanner, Erika Gobet, Willy Tinner and Margit Schwikowski
Additional contact information
Sandra O. Camara-Brugger: University of Basel
Heinz Wanner: University of Bern
Erika Gobet: University of Bern
Willy Tinner: University of Bern
Margit Schwikowski: Paul Scherrer Institute

Climatic Change, 2025, vol. 178, issue 4, No 16, 17 pages

Abstract: Abstract Fires play an important role in the climate system. The boreal forests in Southern Siberia and the Neotropics are crucial regions for global fire emissions with only few available paleofire records. High-alpine ice archives such as Tsambagarav glacier in the Mongolian Altai and Illimani glacier in the Bolivian Andes located close to boreal and evergreen forest ecotones, respectively, are suitable to understand large-scale fire activity in these ecosystems. We discuss strong similarities between the Mongolian Altai and Neotropical ice core paleofire records with declining fire activity during the Late Holocene and hypothesize teleconnections between regional fire activity, possibly due to shared climate drivers in the Northern and Southern hemisphere. Well-documented records of South American summer monsoon activity over the Holocene show a consistent strengthening towards the Late Holocene. The related southwards shift of the Intertropical Convergence Zone resulted in increased monsoonal precipitation that reduced flammability of evergreen vegetation. In contrast, Asian paleo records suggest gradually weakening monsoon activity towards the Late Holocene that resulted in regionally drier conditions. These climate trends induced retractions of boreal forests in the Mongolian Altai, thus limiting fuel availability and fire incidence. We conclude that the main driver of fire activity in these two ecosystems was not temperature, but rather monsoonal-driven moisture. More data are needed to confirm our hypothesis on monsoon-driven teleconnections between regional fire activity.

Keywords: Paleofire; South American Summer monsoon (SASM); Afro-Asian Summer Monsoon (AASM); High-alpine ice core; Atmospheric teleconnections; Microscopic charcoal (search for similar items in EconPapers)
Date: 2025
References: Add references at CitEc
Citations:

Downloads: (external link)
http://link.springer.com/10.1007/s10584-025-03903-w Abstract (text/html)
Access to the full text of the articles in this series is restricted.

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:spr:climat:v:178:y:2025:i:4:d:10.1007_s10584-025-03903-w

Ordering information: This journal article can be ordered from
http://www.springer.com/economics/journal/10584

DOI: 10.1007/s10584-025-03903-w

Access Statistics for this article

Climatic Change is currently edited by M. Oppenheimer and G. Yohe

More articles in Climatic Change from Springer
Bibliographic data for series maintained by Sonal Shukla () and Springer Nature Abstracting and Indexing ().

 
Page updated 2025-04-02
Handle: RePEc:spr:climat:v:178:y:2025:i:4:d:10.1007_s10584-025-03903-w