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Inter-annual variability of pre-monsoon surface air temperatures over India using the North American Multi-Model Ensemble models during the global warming era

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Abstract

In the present study, the efficacy of the North American Multi-Model Ensemble (NMME) seasonal prediction models initialized by February month in simulating the climatological features and inter-annual variability of Summer (March through May; MAM) Surface Air Temperature (SSAT) over India is validated with the observations during 1981–2018. Among the six models, the CanCM4i model can capture the observed increasing trend of maximum, minimum, and mean temperatures over the Indian landmass with slight variation (trend values: 0.84 °C/38 years, 1.1 °C/38 years, and 0.96 °C/38 years). But, statistical analysis reveals that the CanCM4i model has more clod bias than the rest of the models (with less mean bias and RMSE) and in good agreement (slightly) with the observations. Most of the NMME models unable to simulating the extremely warm and cold events over the Indian region. Around 20–30% of extreme events are captured well like in the observations than in the normal years (high threat score). Furthermore, the dominant leading modes (by EOF1 and EOF2) of climate variability over India indicate that all NMME models underestimate (overestimate) the total variance of the first (second) dominant mode of SSAT than the observation except the Gem-NEMO model. Gem-NEMO model has a better total variance for EOF1 (63.84%) and EOF2 (11.23%) than other models. The IC3 (IC3-CanCM4, IC3-CanSIPS, IC3-Gem5-NEMO) models reasonably captured the association between principal component-1 and sea surface temperature (SST) anomalies over the eastern Pacific and positively over the south Atlantic region as in the observations. The NMME models have shown the SST anomalies over the eastern Pacific, Indian, and Atlantic Oceans, which are against to the observations except for the Gem-NEMO model. Thus, there is a large diversity in the representation of climatology features, inter-annual variability, and two dominant modes of variability of SSAT over India in present generation coupled seasonal prediction models.

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Data availability

NMME models output initialized by February (FEBIC) is available from https://iridl.ldeo.columbia.edu/SOURCES/.Models/.NMME/. Monthly maximum and minimum temperature data downloaded from CRUv4.04 https://crudata.uea.ac.uk/cru/data/hrg/cru_ts_4.04/cruts.2004151855.v4.04/.

Monthly SST data is available from OISST (https://www.psl.noaa.gov/data/gridded/data.noaa.oisst.v2.html). GPCP data is available from https://psl.noaa.gov/data/gridded/data.gpcp.html. Monthly zonal and meridional winds at 850 hPa obtained from ERA-interim (https://www.ecmwf.int/en/forecasts/datasets/reanalysis-datasets/era-interim).

Code availability

Not applicable.

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Acknowledgements

We thank the Prof. U C Mohanty, IIT Bhubaneswar, School of Earth Ocean and Climate Sciences, Weather and Climate Prediction Lab, and Indian Institute of tropical meteorology (IITM) for providing computational power. We are very grateful to the institutions participating in the NMME multi-model ensemble operational system for giving the hind-cast experiment data (https://iridl.ldeo.columbia.edu/SOURCES/.Models/.NMME/). Python and PyFerret are used for preparing the plots of the manuscript. Finally, all observational data sources are duly acknowledged. Anonymous reviewers are acknowledged for their insightful comments and suggestions for improving the manuscript.

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All authors contributed to the study conception and design. NRK and DAR performed material preparation, data collection, analysis, and manuscript preparation. All authors commented on previous versions of the manuscript. All authors read and approved the final manuscript.

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Correspondence to Dandi A. Ramu.

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Karrevula, N.R., Ramu, D.A., Nageswararao, M.M. et al. Inter-annual variability of pre-monsoon surface air temperatures over India using the North American Multi-Model Ensemble models during the global warming era. Theor Appl Climatol 151, 133–151 (2023). https://doi.org/10.1007/s00704-022-04269-0

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