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The assumption of constant meteorological and geological conditions in the Hertta Database is the largest source of error in our research, as it affects the utilisable amount of groundwater, which has a direct influence on the amount of heat and the heat load results.
However, the time period of 3 h used in this study had nearly constant meteorological conditions and the total of 12 trials on the same course was, therefore, in an acceptable range regarding these limitations.
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To further distinguish between effects of weather and catchment properties, a catchment relaxation time was calculated using temporally constant average meteorological input.
The unique and global optima are analytically found, with the optimal tilt angle of the cone explicitly expressed through the zenith angle of the Sun and meteorological constants for the isotropic sky model.
The results from the meteorological analyses showed a constant increase in temperature with a high variability of rainfall between 1986 and 2012.
We confirmed that both perceptions of pastoralists and meteorological records showed a constant increase in temperature, a downward trend in rainfall coupled with frequent droughts.
There was collinearity among the meteorological factors, especially between constant and air pressure, average temperature and maximum temperature, and minimum temperature and relative humidity.
Inherent in this approach is the assumption that the relationship between the meteorological variables and fire risk will remain constant, which may not be the case if the future climate, management activities or natural ecosystem development with aging alters forest conditions.
However, no meteorological variables showed significant change; they were almost constant among the different grid-spacing simulations.
Woodhouse et al. (2013) suggests that plume height differences on these occasions could be accounted for by changes in the meteorological conditions with the volcanic source conditions held constant.
The T s – S– r1 diagram (Fig. 1) is obtained by inserting T s -values within a meteorological plausible range into Eq. (7) and keeping selected values for r1 constant.
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