Impacts of 1.5°C and 2.0°C Global Warming on the Onset, Cessation, and Length of the Rainy Season in Global Land Monsoon Regions

dc.contributor.authorTaguela, Thierry N.en
dc.contributor.authorRaji, Ibraheemen
dc.contributor.authorAkinsanola, Akintomide A.en
dc.contributor.authorSinghai, Priyanshien
dc.contributor.authorAdeyeri, Oluwafemi E.en
dc.contributor.authorWainwright, Caroline M.en
dc.contributor.authorBarimalala, Rondrotianaen
dc.date.accessioned2025-12-28T21:40:43Z
dc.date.available2025-12-28T21:40:43Z
dc.date.issued2026en
dc.description.abstractThe onset, cessation, and length of the rainy season are crucial for global water resources, agricultural practices, and food security. However, the response of precipitation seasonality to global warming remains uncertain. In this study, we analyze how global warming levels (GWLs) of 1.5°C and 2°C could affect the timing of rainfall onset (RODs), rainfall cessation (RCDs), and the overall duration of the rainy season (LRS) over global land monsoon (GLM) regions using simulations from CMIP6 under the SSP2-4.5 and SSP5-8.5 scenarios. With high model consensus, our results reveal that RODs are projected to occur later over Southern Africa, North Africa, and South America, but earlier over South Asia and Australia, in a warmer climate. The projected early RODs in Australia are more pronounced at the 2°C GWL under SSP5-8.5. On the other hand, early RCDs are projected over South America and East Asia, while late RCDs are projected over North Africa, with high inter-model agreement. These changes are associated with a future decrease in LRS in most GLM regions. Additionally, we found that continuous warming over 1.5°C will further reduce the length of the rainy season, especially over the South America, North Africa, and Southern Africa monsoon regions. The findings underscore the urgent need to mitigate global warming.en
dc.description.sponsorshipWe thank the World Climate Research Programme’s Working Group on Coupled Modeling for managing the CMIP initiative, and express our gratitude to the climate modeling groups (as listed in Table S1) for their model outputs. We also appreciate the institution that provided the CPC observational data used in this research. Oluwafemi E. ADEYERI is supported by the Australian Research Council (Grant No. CE230100012).en
dc.description.statusPeer-revieweden
dc.format.extent16en
dc.identifier.issn0256-1530en
dc.identifier.otherORCID:/0000-0002-9735-0677/work/200553134en
dc.identifier.scopus105021021870en
dc.identifier.urihttps://hdl.handle.net/1885/733797252
dc.language.isoenen
dc.rights© 2026 The Authorsen
dc.sourceAdvances in Atmospheric Sciencesen
dc.subjectCMIP6 projectionsen
dc.subjectglobal land monsoonen
dc.subjectglobal warming levelsen
dc.subjectrainfall cessationen
dc.subjectrainfall onseten
dc.subjectrainy season lengthen
dc.titleImpacts of 1.5°C and 2.0°C Global Warming on the Onset, Cessation, and Length of the Rainy Season in Global Land Monsoon Regionsen
dc.typeJournal articleen
dspace.entity.typePublicationen
local.bibliographicCitation.lastpage102en
local.bibliographicCitation.startpage87en
local.contributor.affiliationTaguela, Thierry N.; University of Illinois at Chicagoen
local.contributor.affiliationRaji, Ibraheem; University of Illinois at Chicagoen
local.contributor.affiliationAkinsanola, Akintomide A.; University of Illinois at Chicagoen
local.contributor.affiliationSinghai, Priyanshi; University of Oklahomaen
local.contributor.affiliationAdeyeri, Oluwafemi E.; Fenner School of Environment & Society Academic, Fenner School of Environment & Society, ANU College of Systems and Society, The Australian National Universityen
local.contributor.affiliationWainwright, Caroline M.; University of Leedsen
local.contributor.affiliationBarimalala, Rondrotiana; NORCEen
local.identifier.citationvolume43en
local.identifier.doi10.1007/s00376-025-4386-9en
local.identifier.pureff69a1e6-4a51-4751-a3d5-fecbf49c2720en
local.identifier.urlhttps://www.scopus.com/pages/publications/105021021870en
local.type.statusPublisheden

Downloads