Anthropogenic footprint of climate change in the June 2013 northern India flood
During 13–17 June 2013, heavy rainfall occurred in the northern Indian state of Uttarakhand and led to one of the worst floods in history and massive landslides, resulting in more than 5000 casualties and a huge loss of property. In this study, meteorological and climatic conditions leading up to this rainfall event in 2013 and similar cases were analyzed for the period of 1979–2012. Attribution analysis was performed to identify the natural and anthropogenic influences on the climate anomalies using the historical single-forcing experiments in the Coupled Model Intercomparison Project Phase 5. In addition, regional modeling experiments were carried out to quantify the role of the long-term climate trends in affecting the rainfall magnitude of the June 2013 event. It was found that (a) northern India has experienced increasingly large rainfall in June since the late 1980s, (b) the increase in rainfall appears to be associated with a tendency in the upper troposphere towards amplified short waves, and (c) the phasing of such amplified short waves is tied to increased loading of green-house gases and aerosols. In addition, a regional modeling diagnosis attributed 60–90 % of rainfall amounts in the June 2013 event to post-1980 climate trends.
KeywordsExtreme events Climate and weather interactions Greenhouse gas (GHG) forcing Synoptic wave train CMIP5 WRF model Cold air intrusion
PRECL Precipitation data and NCEP Reanalysis data were provided by the NOAA/OAR/ESRL PSD, Boulder, Colorado, USA, from their Web site at http://www.esrl.noaa.gov/psd/. We would like to thank Sunny and Henry Lin for their assistance. J.-H. Yoon is supported by the Office of Science of the U.S. Department of Energy as part of the Earth System Modeling program. PNNL is operated for the Department of Energy by Battelle Memorial Institute under Contract DEAC05-76RLO1830.
- Dubey CS, Shukla DP, Ningreichon AS, Usham AL (2013) Orographic control of the Kedarnath disaster. Curr Sci 105:1474–1476Google Scholar
- Hong C, Hsu H, Lin N, Chiu H (2011) Roles of European blocking and tropical-extratropical interaction in the 2010 Pakistan flooding. Geophys Res Lett 38:L13806Google Scholar
- Joseph S et al (2014) North Indian heavy rainfall event during June 2013: diagnostics and extended range prediction. Clim Dyn (in press). doi: 10.1007/s00382-014-2291-5
- Najar N, Masood S (2014) India and Pakistan strain as flooding kills hundreds. The New York Times. http://www.nytimes.com/2014/09/09/world/asia/hundreds-dead-in-flooding-in-india-and-pakistan.html?_r=0
- Singh D et al (2014) Severe precipitation in Northern India in June 2013: causes, historical context, and changes in probability. Bull Am Meteorol Soc 95:58–61Google Scholar
- Wang S, Davies RE, Gillies RR, Jin J (2011a) Changing monsoon extremes and dynamics: example in Pakistan. In: Zhao J, Higgins W (eds) NOAA NWS, science and technology infusion climate bulletin, pp 61–68Google Scholar