Trends in Extreme Rainfall Events in Tasmania, Australia
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Trends in Extreme Rainfall Events in Tasmania, Australia

Authors: Orpita U. Laz, Ataur Rahman

Abstract:

Climate change will affect various aspects of hydrological cycle such as rainfall. A change in rainfall will affect flood magnitude and frequency in future which will affect the design and operation of hydraulic structures. In this paper, trends in subhourly, sub-daily, and daily extreme rainfall events from 18 rainfall stations located in Tasmania, Australia are examined. Two nonparametric tests (Mann-Kendall and Spearman’s Rho) are applied to detect trends at 10%, 5%, and 1% significance levels. Sub-hourly (6, 12, 18, and 30 minutes) annual maximum rainfall events have been found to experience statistically significant upward trends at 10% level of significance. However, sub-daily durations (1 hour, 3 and 12 hours) exhibit decreasing trends and no trends exists for longer duration rainfall events (e.g. 24 and 72 hours). Some of the durations (e.g. 6 minutes and 6 hours) show similar results (with upward trends) for both the tests. For 12, 18, 60 minutes and 3 hours durations both the tests show similar downward trends. This finding has important implication for Tasmania in the design of urban infrastructure where shorter duration rainfall events are more relevant for smaller urban catchments such as parking lots, roof catchments and smaller sub-divisions.

Keywords: Climate change, design rainfall, Mann-Kendall test, trends, Spearman’s Rho, Tasmania.

Digital Object Identifier (DOI): doi.org/10.5281/zenodo.1097044

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References:


[1] L. Coates, “An overview of fatalities from some natural hazards in Australia,” in Proc. Conference on Natural Disaster Reduction: Engineers Australia, Canberra, ACT, Australia, 1996, pp. 49–54.
[2] R. Suppiah, and K. J. Hennessy, “Trends in total rainfall, heavy rain events and number of dry days in Australia,” International Journal of Climatology, vol.18, issue. 10, pp. 1141-1164, Aug. 1998.
[3] K. E. Kunkel, K. Andsager, and D. R. Easterling, “Long-term trends in extreme precipitation events over the conterminous United States and Canada,” Journal of Climate, vol. 12, issue. 8, pp. 2515 – 2527, Aug. 1999.
[4] K. E. Kunkel, et al., "Observations and regional climate model simulations of heavy precipitation events and seasonal anomalies: A comparison," Journal of Hydrometeorology, vol. 3.3, issue. 3, pp. 322 – 334, June. 2002.
[5] K. E. Kunkel, D. R. Easterling, K. Redmond, and K. Hubbard, “Temporal variations of extreme precipitation events in the United States: 1895–2000,” Geophysical Research Letters, vol. 30, issue. 17, p. 1900, Sep. 2003.
[6] R. Joseph, M. Ting, and P. Kumar, “Multiple-scale spatio-temporal variability of precipitation over the coterminous United States,” Journal of Hydrometeorology, vol. 1, issue. 5, pp. 373-392, Oct. 2000.
[7] M. Brunetti, M. Colacino, M. Maugeri, and T. Nanni, “Trends in the daily intensity of precipitation in Italy from 1951 to 1996,” International Journal of Climatology, vol. 21, issue. 3, pp. 299-316, March. 2001.
[8] S. K. Aryal, B. C. Bates, E. P. Campbell, Y. Li, M. J. Palmer, and N. R. Viney, “Characterizing and modeling temporal and spatial trends in rainfall extremes,” Journal of Hydrometeorology, vol. 10, issue. 1, pp. 241-253, Feb. 2009.
[9] M. N. Khaliq, T. B. Ouarda, P. Gachon, L. Sushama, and A. St-Hilaire, “Identification of hydrological trends in the presence of serial and cross correlations: A review of selected methods and their application to annual flow regimes of Canadian rivers,” Journal of Hydrology, vol. 368, issue. 1, pp. 117-130, Apr. 2009.
[10] K. E. Trenberth, “Atmospheric moisture residence times and cycling: Implications for rainfall rates and climate change,” Climatic change, vol. 39, issue. 4, pp. 667-694, Aug. 1998.
[11] L. V. Alexander, et al., “Global observed changes in daily climate extremes of temperature and precipitation,” Journal of Geophysical Research: Atmospheres (1984–2012), vol. 111, issue. D5, March. 2006.
[12] P. Y. Groisman, et al., “Trends in intense precipitation in the climate record,” Journal of climate, vol. 18, issue. 9, pp. 1326-1350, May. 2005.
[13] G. Meehl, et al., Global climate projections, in Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, edited by S. Solomon et al., Cambridge Univ. Press, Cambridge, U. K. 2007, pp. 747–845.
[14] P. G. Oguntunde, J. Friesen, N. van de Giesen, and H. H. Savenije, “Hydroclimatology of the Volta River Basin in West Africa: Trends and variability from 1901 to 2002,” Physics and Chemistry of the Earth, Parts A/B/C, vol. 31, issue. 18, pp. 1180-1188, 2006.
[15] M. Cannarozzo, L. V. Noto, and F. Viola, “Spatial distribution of rainfall trends in Sicily (1921-2000),” Physics and Chemistry of the Earth, Parts A/B/C, vol. 31, issue. 18, pp. 1201-1211, 2006.
[16] K. Adamowski, and J. Bougadis, “Detection of trends in annual extreme rainfall,” Hydrological Processes, vol. 17, issue. 17, pp. 3547-3560, Dec. 2003.
[17] A. Mailhot, S. Duchesne, D. Caya, and G. Talbot, “Assessment of future change in intensity–duration–frequency (IDF) curves for Southern Quebec using the Canadian Regional Climate Model (CRCM),” Journal of hydrology, vol. 347, issue. 1, pp. 197-210, Dec. 2007.
[18] R. Hardwick Jones, S. Westra, and A. Sharma, “Observed relationships between extreme sub‐daily precipitation, surface temperature, and relative humidity,” Geophysical Research Letters, vol. 37, issue. 22, Nov. 2010.
[19] G. Lenderink, and E. Van Meijgaard, “Increase in hourly precipitation extremes beyond expectations from temperature changes,” Nature Geoscience, vol. 1, issue. 8, pp. 511-514, July. 2008.
[20] A. Dai, X. Lin, and K. L. Hsu, “The frequency, intensity, and diurnal cycle of precipitation in surface and satellite observations over low-and mid-latitudes,” Climate dynamics, vol. 29, issue. 7, pp. 727-744, Dec. 2007.
[21] P. Leahy, G. Kiely, and T. M. Scanlon, “Managed grasslands: A greenhouse gas sink or source?,” Geophysical Research Letters, vol. 31, issue. 20, L20507, Oct. 2004.
[22] B. M. Reich, “Short-duration rainfall-intensity estimates and other design aids for regions of sparse data,” Journal of Hydrology, vol. 1, issue. 1, pp. 3-28, March. 1963.
[23] C. W. Landsea, G. A. Vecchi, L. Bengtsson, and T. R. Knutson, “Impact of Duration Thresholds on Atlantic Tropical Cyclone Counts,” Journal of Climate, vol. 23, issue. 10, pp. 2508-2519, May. 2010.
[24] T. R. Knutson., C. Landsea, and K. A. Emanuel, “Tropical cyclones and climate change: A review,” InGlobal Perspectives on Tropical Cyclones: From Science to Mitigation, Singapore, World Scientific Publishing Company, May. 2010, pp. 243-284.
[25] K. Arnbjerg-Nielsen, “Significant climate change of extreme rainfall in Denmark,” Water Science & Technology, vol. 54, issue. 6-7, pp. 1-8, 2006.
[26] B. Yu, and D. T. Neil, “Long‐term variations in regional rainfall in the south‐west of Western Australia and the difference between average and high intensity rainfalls,” International Journal of Climatology, vol.13, issue. 1, pp. 77-88, Jan. 1993.
[27] N. Nicholls, and A. Kariko, “East Australian rainfall events: Interannual variations, trends, and relationships with the Southern Oscillation,” Journal of Climate, vol. 6, issue. 6, pp. 1141-1152, June. 1993.
[28] M. Haylock, and N. Nicholls, “Trends in extreme rainfall indices for an updated high quality data set for Australia, 1910-1998,” International Journal of Climatology, vol. 20, issue. 13, pp. 1533-1541, Nov. 2000.
[29] J. Li, J. Feng, and Y. Li, “A possible cause of decreasing summer rainfall in northeast Australia,” International Journal of Climatology, vol. 32, issue. 7, pp. 995-1005, June. 2012.
[30] K. Haddad, A. Rahman, and J. Green, “Design rainfall estimation in Australia: a case study using L moments and generalized least squares regression,” Stochastic Environmental Research and Risk Assessment, vol. 25, issue. 6, pp. 815-825, Aug. 2011.
[31] S. Westra, and S. A. Sisson, “Detection of non-stationarity in precipitation extremes using a max-stable process model,” Journal of Hydrology, vol. 406, issue. 1-2, pp. 119-128, Aug 2011.
[32] Y. R. Chen, B. Yu, and G. Jenkins, “Secular variation in rainfall and intensity-frequency-duration curves in Eastern Australia,” Journal of Water and Climate Change, vol. 4, issue. 3, pp. 244-251, 2013.
[33] M. R. Grose, S. P. Corney, J. J. Katzfey, J. Bennett, and N. L. Bindoff, “Improving projections of rainfall trends through regional climate modeling and wide-ranging assessment,” in The 19th International Congress on Modelling and Simulation (MODSIM2011), Perth, Western Australia, Dec. 2011, pp. 2726-2732.
[34] M. R. Grose, et al, “Assessing rainfall trends and remote drivers in regional climate change projections: The demanding test case of Tasmania,” in IOP Conference Series: Earth and Environmental Science, vol. 11, issue. 1, IOP Publishing, Aug.2010, p. 012038.
[35] J. Langford, ‘Weather and climate’, in: J. L. Davies (ed.), Atlas of Tasmania, Department of Lands and Surveys, Hobart, Australia, 1965, pp. 2-11.
[36] Bureau of Meteorology, Climate of Tasmania. AGPS, Canberra, 1993, p. 30.
[37] D. J. Shepherd, “Some characteristics of Tasmanian rainfall,” Australian Meteorological Magazine, vol. 44, issue. 4, pp. 261-274, 1995.
[38] CSIRO, Climate projections for Australia. CSIRO Atmospheric Research, Melbourne, 2001. http://www.cmar.csiro.au/e-print/open/ projections2001.pdf
[39] C. R. Godfred-Spenning, and T. T. Gibson, A synoptic climatology of rainfall in HEC catchments, Antarctic CRC, 1995.
[40] R. Srikanthan, and B. J. Stewart, “Analysis of Australian rainfall data with respect to climate variability and change,” Australian Meteorological Magazine, vol. 39, issue. 1, pp. 11-20, 1991.
[41] C. Bryant, Understanding bushfire: trends in deliberate vegetation fires in Australia, Canberra, Australia: Australian Institute of Criminology, p. 56, 2008.
[42] J. O'Donnell, and A. Livingston, Catchment Management in Tasmania- A Hydro-Electric Commission Perspective, 1992.
[43] C. J. White, et al., Climate Futures for Tasmania: extreme events technical report, 2010.
[44] H. B. Mann, Non-parametric tests against trends, Econometrica, 13, pp. 245-259, 1945.
[45] M. G. Kendall, Rank Correlation Methods. Griffin, London, 1975.
[46] S. Yue, P. Pilon, and G. Cavadias, “Power of the Mann–Kendall and Spearman's rho tests for detecting monotonic trends in hydrological series,” Journal of hydrology, vol. 259, issue. 1, pp. 254-271, March. 2002.