Open Access Open Access  Restricted Access Subscription Access

Spatio-temporal changes in temperature over India


Affiliations
1 Space Applications Centre, Ahmedabad 380 015, India
 

A study was taken up to identify annual changes in temperature at a scale of 1° × 1°. For this study, daily (maximum and minimum) temperature data for 45 years (1969–2013) at a grid size of 1° × 1°, prepared by the India Meteorological Department, Pune were used. The identification of change was based on statistical trend analysis. From the analysis, it can be concluded that the dominant tendency over the India land mass is of warming, and colder months of the year show more warming. Analysis of temperature difference (TD) brought out the existence of contiguous and large spatial clusters of shrinking and expanding TD. Further analysis is required to factor the variability in temperature due to anthropogenic changes.

Keywords

Annual changes, spatio-temporal patterns, temperature difference, trend analysis
User
Notifications
Font Size

  • Jones, P. D. and Moberg, A., Hemispheric and large-scale surface airtemperature variations: an extensive revision and an update to2001. J. Clim., 2003, 16, 206–223.
  • del Rio, S., Penas, A. and Fraile, R., Analysis of recent climatic variationsin Castile and Leon (Spain). Atmos. Res., 2005, 73, 69–85.
  • Brunet, M. et al., Temporal and spatial temperature variability and changeover Spain during 1850–2005. J. Geophys. Res., 2007,112, D12117; doi: 10.1029/2006JD008249.
  • Wagholikar, N. K., Sinha Roy, K. C., Sen, P. N. and Kumar, P. P., Trendsin seasonal temperatures over the India region. J. EarthSyst. Sci., 2014, 123(4), 673–687.
  • Turkes, M. and Sumer, U. M., Spatial and temporal patterns of trendsand variability in diurnal temperature ranges of Turkey.Theor. Appl. Climatol., 2004, 77, 195–227.
  • Hamdi, M. R., Abu-Allaban, M., Al-Shayeb, A., Jaber, M. and Momani, N. M., Climate change in Jordan: a comprehensive examination approach. Am. J. Environ. Sci., 2009, 5, 58–68.
  • Tabari, H., Somee, B. S. and Zadeh, M. R., Testing for long-term trendsin climatic variables in Iran. Atmos. Res., 2011, 100, 132–140.
  • Pramanik, S. K. and Jagannathan, P., Climatic changes in India rainfall. Indian J. Meteorol. Geophys., 1954, 4, 291–309.
  • Rupa Kumar, K., Krishankumar, K. and Pant, G. B., Diurnal asymmetryof surface temperature trends over India. Geophys.Res. Lett., 1994, 21, 677–680.
  • Kothawale, D. R. and Rupa Kumar, K., On the recent changes in surfacetemperature trends over India. Geophys. Res. Lett., 2005,32, L18714; doi: 10.1029/2005GL023528.
  • Arora, M., Goel, N. K. and Singh, P., Evaluation of temperature trendsover India. Hydrol. Sci. J., 2005, 50, 81–93.
  • Dhorde, A., Dhorde, A. and Gadgil, A. S., Long-term temperature trendsat four largest cities of India during the twentieth century. J. Indian Geophys. Union, 2005, 13, 85–97.
  • Dash, S. K. and Hunt, J. C. R., Variability of climate change in India. Curr. Sci., 2007, 93, 782–788.
  • Dash, S. K. and Mamgain, A., Changes in the frequency of categories oftemperature extremes in India. J. Appl. Meteorol. Climatol., 2011, 50, 1842–1858.
  • Srivastava, A. K., Rajeevan, M. and Kshirsagar, S. R., Development ofa high resolution daily gridded temperature data set (1969–2005) for the Indian region. Atmos. Sci. Lett., 2009; doi:10.1002/asl.232.
  • Hingane, L. S., Rupa Kumar, K. and Rama Murthy, B. V., Longterm trendsof surface air temperature in Inida. J. Climatol., 1985,5, 521–528.
  • Raso, J. M., The recent evolution of mean annual temperature in Spain. In Advances in historical climatology in Spain (ed. Martin, J.), Oikos-Tau, Spain, 1997, pp. 201–223.
  • Karl, T. R. et al., Asymmetric trends of daily maximum and minimum temperature. In Papers in Natural Resources. 1993, Paper 185 (http://digitalcommons.unl.edu/natrespapers/185).
  • Easterling, D. R. et al., Maximum and minimum temperature trendsfor the globe. Science, 1997, 277, 364–367; doi:10.1126/science.277.5324.364.
  • Watterton, I. G., The diurnal cycle of surface air temperature in simulatedpresent and dobled CO2 climates. Climate Dyn., 1997,13, 533–545.
  • Stone, D. A. and Weaver, A. J., Factors contributing to diurnal temperaturerange trends in twentieth and twenty-first century simulationsof the CCCma coupled model. Climate Dyn., 2003, 20, 435–445.
  • Lewis, S. C. and Karoly, D. J., Evaluation of historical diurnal temperaturerange trends in CMIP5 models. J. Climate, 2013, 26, 9077–9089.
  • Venkataraman, C., Habib, G., Eiguren-Fernandez, A., Miguel, A. H. and Friedlander, S. K., Residential Biofuels in South Asia: carbonaceousaerosol emissions and climate impacts. Science,2005, 307, 1454–1456.
  • Rengarajan, R., Sarin, M. M. and Sudheer, A. K., Carbonaceous andinorganic species in atmospheric aerosols during wintertime overurban and high-altitude sites in north India. J. Geophys. Res.,2007, 112, D21307; doi: 10.1029/2006JD008150.
  • Ramanathan, V. et al., Atmospheric brown clouds: hemispherical andregional variations in long-range transport, absorption and radiativeforcing. J. Geophys. Res., 2007, 112, D22S21; doi:10.1029/2006JD008124.
  • Gustafsson, Ö. et al., Brown clouds over south Asia: biomass or fossilfuel combustion? Science, 2009, 323, 495–498.
  • Ram, K., Sarin, M. M. and Tripathi, S. N., A 1 year record of carbonaceous aerosolsfrom an urban location (Kanpur) in the Indo- Gangeticplain: characterization, sources and temporal variability. J. Geophys. Res., 2010, 115, D24313; doi: 10.1029/2010JD014188.
  • Ram, K., Sarin, M. M. and Tripathi, S. N., Temporal trends in atmospheric PM2.5, PM10, EC, OC, WSOC and optical properties ofaerosols from Indo-Gangetic plain: Impact of biomass burning emissions. Environ. Sci. Technol., 2012, 46, 686–695.
  • Singh, S., Singh, R. and Rao, V. U. M., Temporal dynamics of dew andfog events and their impact on wheat productivity in semi-arid regionof India. In Third International Conference on Fog, Fog Collectionand Dew, NetSys Int. (Pty) Ltd., Cape Town, South Africa, 11–15 October 2004 (http://www.up.ac.za/academic/geog/meteo/EVENTS/fogdew2003/PAPERS/C65.pdf)
  • Singh, S. and Singh, D., Recent fog trends and its impact on wheat productivityin NW plains in India. In 5th International Conference onFog, Fog Collection and Dew Münster, Germany, 25–30 July2010.
  • Jenamani, R. K., Alarming rise in fog and pollution causing a fall inmaximum temperature over Delhi. Curr. Sci., 2007, 93, 314–322.

Abstract Views: 357

PDF Views: 141




  • Spatio-temporal changes in temperature over India

Abstract Views: 357  |  PDF Views: 141

Authors

Markand Oza
Space Applications Centre, Ahmedabad 380 015, India
C. M. Kishtawal Kishtawal
Space Applications Centre, Ahmedabad 380 015, India

Abstract


A study was taken up to identify annual changes in temperature at a scale of 1° × 1°. For this study, daily (maximum and minimum) temperature data for 45 years (1969–2013) at a grid size of 1° × 1°, prepared by the India Meteorological Department, Pune were used. The identification of change was based on statistical trend analysis. From the analysis, it can be concluded that the dominant tendency over the India land mass is of warming, and colder months of the year show more warming. Analysis of temperature difference (TD) brought out the existence of contiguous and large spatial clusters of shrinking and expanding TD. Further analysis is required to factor the variability in temperature due to anthropogenic changes.

Keywords


Annual changes, spatio-temporal patterns, temperature difference, trend analysis

References





DOI: https://doi.org/10.18520/cs%2Fv109%2Fi6%2F1154-1158