Variability of Indian summer monsoon droughts in CMIP5 climate models

• Published in: Climate dynamics 2019-08, Vol.53 (3-4), p.1937-1962
• Main Authors: Preethi, B., Ramya, R., Patwardhan, S. K., Mujumdar, M., Kripalani, R. H.
• Format: Article
• Language: English
• Subjects: Amplification; Analysis; Area; Atmospheric precipitations; Climate; Climate models; Climate variability; Climatology; Computer simulation; Drought; Drought conditions; Drought index; Droughts; Earth and Environmental Science; Earth Sciences; Equatorial regions; Geophysics/Geodesy; Historic temperatures; India; Indian Ocean; Monsoon circulation; Monsoon climates; Monsoon rainfall; Monsoon trough; Monsoons; Oceanography; Pacific Ocean; Precipitation; Precipitation variability; Rain; Rain and rainfall; Rainfall; Rainfall simulators; Rainfall variability; Sea surface; Sea surface temperature; South Asia; Spatial variability; Spatial variations; Standardized precipitation index; Summer; Summer monsoon; Surface temperature; Wind
• ISSN: 0930-7575; 1432-0894
• DOI: 10.1007/s00382-019-04752-x

Variability of Indian summer monsoon droughts is investigated by computing all-India drought indices namely Percent of Normal Precipitation, Standardized Precipitation Index and percentage area of India under moderate and severe drought conditions. Observations for recent decades, post 1960, exhibit declining trend in monsoon rainfall with frequent occurrence and intensification of droughts along with an increase in percentage of area under moderate and severe drought conditions, in association with variations in sea surface temperature (SST). Historical simulations from CMIP5 models suggest that two models, ACCESS1.0 and INMCM4, could well simulate monsoon rainfall variability, particularly the frequent occurrence of droughts and spatial variability of rainfall during drought years in recent historical period (1961–2005). Future projections of all-India drought indices from these two models indicate frequent droughts during near and mid future (2010–2069) with respect to the recent historical period. Intensification of severe droughts for near and mid future are suggested to be more pronounced over north-central India. The reduction in rainfall in the near and mid future is dynamically consistent with a westward shift in large-scale monsoon circulation, particularly the monsoon trough over South Asia. Interestingly, future projections of monsoon teleconnections indicate a weakening (strengthening) of in-phase (out-of-phase) relationship of all-India drought intensity with the equatorial eastern Pacific and the Indian Ocean (western Pacific) SST. Whereas, a strengthening of in-phase relationship between percentage of area under drought conditions and the equatorial eastern Pacific SST is projected for near and mid future with respect to the recent historical period. These drought features are consistent in both the models.