BACO-25 Admin

Comment

Oral

IAMAS

M18 - Monsoon systems: variability, processes, predictability, change and extremes

Robust increase in Indian summer monsoon intraseasonal variability in the warmer climate

1. Gopinadh  Konda*, Pusan National University

2. June-Yi  Lee, Pusan National University

3. Jasti   Chowdary, Indian Institute of Tropical Meteorology

4. C.  Gnanaseelan, Indian Institute of Tropical Meteorology

5. Anant  Parekh, Indian Institute of Tropical Meteorology

6. Naresh  Vissa, National Institute of Technology

7. Phani  Krishna, Indian Institute of Tropical Meteorology

*Presenting Author

Despite its significant societal and scientific importance, the projected changes in the characteristics of Intraseasonal Oscillations (ISOs) associated with Indian Summer Monsoon Rainfall (ISMR) under enhanced anthropogenic greenhouse gas emissions remain largely unexplored. This study utilizes downscaled and bias-corrected historical simulations and projections from 17 models of the Coupled Model Intercomparison Project Phase 6 (CMIP6) to investigate the future evolution of ISOs. Our findings reveal a twofold increase in ISO variability over India by the end of the 21st century under a high-emission scenario relative to the present, raising critical concerns about societal impacts. The increased magnitude of future precipitation anomalies associated with northward-propagating ISOs suggests a heightened possibility of active monsoon spells triggering extreme rainfall events. Additionally, the phase speed of these northward-propagating ISOs over the Bay of Bengal is projected to accelerate due to weakened air-sea coupling and feedback mechanisms. This acceleration reduces the northwest-southeast tilt of the precipitation band, altering the spatial structure of the ISOs. Furthermore, the strengthening of circulation-precipitation feedback and the warming of the Indian Ocean are projected to enhance the phase speed of monsoon ISOs, leading to more frequent active spells. This study underscores the critical role of regional ocean-atmosphere feedback in shaping future ISO characteristics, emphasizing the urgent need for improved understanding and prediction of these changes in the context of a warming climate.