Climate Change Impacts on the South American Monsoon System and Its Surface–Atmosphere Processes Through RegCM4 CORDEX-CORE Projections

• Published in: Earth systems and environment Vol. 5; no. 4; pp. 825 - 847
• Main Authors: Teodoro, Thales Alves, Reboita, Michelle Simões, Llopart, Marta, da Rocha, Rosmeri Porfírio, Ashfaq, Moetasim
• Format: Journal Article
• Language: English
• Published: Cham Springer International Publishing 01.12.2021; Springer Nature B.V
• Subjects: Atmosphere; Atmospheric models; Climate; Climate change; Climate Change/Climate Change Impacts; Climate models; Coupling; Earth and Environmental Science; Earth Sciences; Earth System Sciences; Energy balance; Environmental impact; Environmental Science and Engineering; Geography; Global climate; Global climate models; Heat; Monitoring/Environmental Analysis; Monsoons; Original Article; Precipitation; Rainy season; Regions; Summer; Surface water; Temperature; Wind; Brazil; Argentina; Amazon Basin; United States > US; Atlantic Ocean; Surface energy balance; Surface water balance; Climate change; SAMS; Coupling indices; Monsoon area
• ISSN: 2509-9426; 2509-9434
• DOI: 10.1007/s41748-021-00265-y

This study evaluates projected changes in surface water and energy balances and surface–atmosphere coupling in the South American Monsoon System (SAMS) for the end of the century (2080–2099). The analyses are based on two ensemble datasets, which follow Representative Concentration Pathway 8.5 in the future period, and cover four subdomains (Northern and Southern—NAMZ and SAMZ—Amazon, La Plata Basin—LPB, and Southern Southeast Brazil—SSB). One ensemble consists of three Global Climate Models (HadGEM2-ES, MPI-ESM-MR and NorESM1-M), while the other consists of their dynamically downscaled version at 25 km horizontal grid spacing using Regional Climate Model version 4 (RegCM4). As both ensembles are able in reproducing the annual cycle of the components of the surface water and energy balances in the present climate, they can be used in the study of future climate. During the wet season (November–March), both ensembles project a decrease in precipitation over NAMZ and SAMZ (an exception is RegCM4 that projects a slight increase in SAMZ), and an increase across the LPB and SSB. These changes do not cause retreat or expansion of the monsoon area over the continent, which is similar to the present climate (1995–2014). For the wet season, the ensembles are in line with the presence of a strong surface–atmosphere coupling in LPB and SSB, weak coupling in SAMZ and very weak coupling in NAMZ. For future climate, the coupling is even weaker in NAMZ, which may be a driver for the negative changes in precipitation. For the other subdomains, while the ensembles project similar signals of precipitation changes, they disagree with the surface-atmosphere coupling highlighting the uncertainties in future climate.