1[1]Changnon S A, Roger A, Pielke Jr et al. Human factors explain the increased losses from weather and climate extremes. Bull. of the Amer. Mete. Soci., 2000, 81(3): 437-442.
2[2]IPCC: Climate Change 2001, The Scientific Basis, Observed Climate Variability and Change. In: J T Houghton, Y Ding, J Griggs et al., Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, 881.
3[3]Easterling D R, J L Evans, PYa Groisman et al. Observed variability and trends in extreme climate events: a brief review. Bull. of the Ameri. Mete. Soci., 2000, 81(3): 417-425.
4[4]Harmel R D, C W Richardson, C L Hanson et al. Evaluating the adequacy of simulating maximum and minimum daily air temperature with the normal distribution. Journal of App. Mete., 41: 744-753.
5[5]Michael J Janis. Observation-time-dependent biases and departures for daily minimum and maximum air temperature.Journal of App. Mete., 2002, 41: 588-602.
6[6]Tomsett A C, Ralf Toumi. Diurnal temperature range and rainfall probability over the United Kingdom. Geo. Res.Letters, 2000, 27(9): 1279-1582.
7[7]Karl T R, R W Knight, N Plummer. Trends in high-frequency climate variability in the twentieth century. Nature,1995, 377: 217-220.
8[8]Moberg A, P D Jones, M Barriendos et al. Day-to-day temperature variability trends in 160-275-year long European instrumental records. J. Geophys. Res., 2000, 105(D18): 22849-22868.
9[9]Gruza G, E Rankova, V Razuvaev. Indicators of climate change for the Russian federation. Clim. Change, 1999, 42:219-242.
10[10]Frich P, L V Alexander, P Della-Marta et al. Observed coherent changes in climatic extremes during the second half of the 20th century. Clim. Res., 2001.
