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Annual average trend of maximum and minimum temperature shows that in general, maximum temperature over the observed period indicates stronger increasing trend than minimum temperature (Fig. 5).
The mean daily maximum temperature over the entire period was 80°F.
We calculated annual cumulated sums (sums of daily values) of mean and maximum temperature over April-May (following [ 61, 62, 11]), as these months represent the reproductive period [ 58, 63].
In addition, a 23.6% (RR: 1.236, 95% CI: 1.029 1.485) increase in daily digestive mortality in Chongqing and an 8.0% (RR: 1.080, 95% CI: 1.004 1.161) increase in respiratory mortality in Harbin were both significantly correlated with a 1°C increase in the daily maximum temperature over the threshold.
A heat wave is then defined as the longest period of consecutive days satisfying the following conditions: the daily maximum temperature is above T1 for at least 3 days, the daily maximum temperature is above T2 for every day of the entire period, and the average of daily maximum temperature over the entire period is above T1.
Applying the methodology used in previously conducted European multi-city studies [ 2, 5, 16], we modelled the marginal relationship between total daily mortality and maximum temperature over average lag 0 2 by means of 4 degrees of freedom (df) natural cubic splines (NCS), also specifying a first-order autoregressive correlation structure within summer in the Poisson GEE model.
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A statistical analysis of the current situation, particularly in Algeria, shows that minimum temperatures have been rising faster than maximum temperatures over a number of decades.
Daily maximum temperatures over most of the region range from the mid-80s F (upper 20s C) from December to April to the upper 80s F (low 30s C) from May to November.
T avg (PIFL is the average of daily average temperatures and T max (PIFL is the average of daily maximum temperatures over this period 1Significance codes: * p < 0.05, ** p < 0.01, *** p < 0.001 2Akaike Information Criterion (lower is better).
On the other hand, before the onset of the active MJO, the higher maximum temperatures over the sea than over the land in the early morning were considered to result from the nighttime radiative cooling of the land surface.
However, it is important to note that the temperature estimates derived from means of the daily minimum and maximum temperatures over each month that were further averaged over 50 years.
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