Abstract
Indian Summer Monsoon (IMS) prevails during June–July-August-September (JJAS) and 80% of the annual precipitation is received during JJAS. The spatial and temporal variability of ISMR and surface temperature has been influencing agriculture and water resources. The changes in earth’s surface temperature is affecting the patterns of weather and climate and influencing the agriculture. The Coupled Model Inter comparison Project 5 (CMIP5) models output data is generally of higher resolution with different emission experiments and therefore rainfall and surface temperature over India is analyzed under CMIP5 which may be used for agricultural purposes.
The Indian Summer Monsoon Rainfall (ISMR) in simulation of BCC-CSM1.1(m), CCSM4, CESM1(BGC), CESM1(CAM5), CESM1(FASTCHEM), CESM1(WACCM), and MPI-ESM-MR for the period of 2006–2050 under RCPs 4.5 and 8.5 at 99% confidence shows possibility of excessrainfall over homogeneous monsoon regions of NWI, NEI, WCI and PI, while deficit rainfall over NWI, NEI, WCI, CNI and PI. At 99% and 95% confidence levels, deficit rainfall is found over CNI, NWI and PI. The CMIP5 model GISS-E2-H, BCC-CSM1.1 m and GISS-E2-H-CC for Tmax; GFDL-CM3, MRI-CGM3 and MRI-ESM1 for Tmin; and CESM1 (CAM5) for T under Representative Concentration Pathways (RCPs) 4.5 and 8.5 for the period of 2021–2055 shows possible significant warming of 0.5°C–0.7°C at 99% confidence level over homogeneous temperature regions of NC, NW, and WC. The warming of 0.2°C–0.5°C might be possible at other locations.
These future projections may be used in crop simulation models which may assist adaptation to climate change-through changes in farming practices, cropping patterns, and use of new technologies.
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References
Chaturvedi, et al. (2012). Multi-model climate change projections for India under representative concentration pathways. Current Science, 103, 791–802.
Kripalani, R., Kulkarni, A., Sabade, S., & Khandekar, M. (2003). Indian monsoon variability in a global warming scenario. Natural Hazards, 29, 189–206.
Kripalani, R. H., et al. (2007a). Response of the East Asian summer monsoon to doubled atmosphericCO2: Coupled climate model simulations and projections under IPCC AR4. Theoretical and Applied Climatology, 87, 1–28.
Kripalani, R. H., et al. (2007b). South Asian summer monsoon precipitation variability: Coupled climate model simulations and projections under IPCC AR4. Theoretical and Applied Climatology, 90, 133–159.
Kumar, R., et al. (2002). Climate change in India: Observations and model projections. In P. R. Shukla et al. (Eds.), Climate change and India: Issues, concerns and opportunities (pp. 24–75). New Delhi: Tata McGraw-Hill Publishing Co Ltd..
Kumar, R., et al. (2003). Future climate scenarios. In P. R. Shukla et al. (Eds.), Climate change and India: Vulnerability assessment and adaptation (pp. 69–127). Hyderabad: Universities Press.
Kumar, R., et al. (2013). High-resolution climate change scenarios for India for the 21st century. Current Science, 90(3), 10.
Lal, M., et al. (1994). Effect of global warming on Indian monsoon simulated with a coupled ocean-atmosphere general circulation model. Current Science, 66, 430–438.
Lal, M., et al. (1995). Effect of transient increase in greenhouse gases and sulphate aerosols on monsoon climate. Current Science, 69, 752–763.
Lal, M., et al. (2001). Future climate change: Implications for Indian summer monsoon and its variability. Current Science, 81, 1196–1207.
May, W. (2004). Simulation of the variability and extremes of daily rainfall during the Indian summer monsoon for present and future times in a global time-slice experiment. Climate Dynamics, 2, 183–204.
Meehl, G. A., & Washington, W. M. (1993). South Asian summer monsoon variability in a model with doubled atmospheric carbon dioxide concentration. Science, 260, 1101–1104.
Menon, A., et al. (2013a). Enhanced future variability during India’s rainy season. Geophysical Research Letters, 40(12), 3242–3247.
Menon, A., et al. (2013b). Consistent increase in Indian monsoon rainfall and its variability across CMIP-5 models. Earth System Dynamics, 4, 287–300.
Pattnayak, K. C., et al. (2015). Projections of rainfall and surface temperature from CMIP5 models under RCP4.5 and 8.5 over BIMSTEC countries. In EGU general assembly conference abstracts (Vol. 17, p. 556). EGU General Assembly, held 12–17 April, 2015 in Vienna, Austria. id.556.
Rupa Kumar, K., & Ashrit, R. G. (2001). Regional aspects of global climate change simulations: Validation and assessment of climate response over Indian monsoon region to transient increase of greenhouse gases and sulfate aerosols. Mausam, Special Issue on Climate Change, 52, 229–244.
Sarthi, P., et al. (2012). Possible changes in the characteristics of Indian summer monsoon under warmer climate. Global and Planetary Change, 92–93, 17–29.
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Parth Sarthi, P. (2019). Future Changes in Rainfall and Temperature Under Emission Scenarios over India for Rice and Wheat Production. In: Sheraz Mahdi, S. (eds) Climate Change and Agriculture in India: Impact and Adaptation. Springer, Cham. https://doi.org/10.1007/978-3-319-90086-5_1
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