摘要:Daily temperature (mean, minimum and maximum) and atmospheric precipitation data from 857
stations are used to analyze variations in the space–time distribution of extreme temperatures
and precipitation across Russia during the past six decades. The seasonal numbers of days
(N) when daily air temperatures (diurnal temperature range, precipitation) were higher or
lower than selected thresholds are used as indices of climatic extremes. Linear trends in
N are calculated for each station for the time period of interest. The seasonal numbers of days
(for each season) with maximum temperatures higher than the 95th percentile have
increased over most of Russia, with minimum temperatures lower than the 5th percentile
having decreased. A tendency for the decrease in the number of days with abnormally high
diurnal temperature range is observed over most of Russia. In individual regions
of Russia, however, a tendency for an increasing number of days with a large
diurnal amplitude is found. The largest tendency for increasing number of days
with heavy precipitation is observed in winter in Western Siberia and Yakutia.