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Similar correlations were obtained between spring hemispheric mean temperature and S, and between fall hemispheric mean temperature and F (Supplementary Table 1).
But warming raises mean temperature and increases the incidence of extreme temperatures and weather events.
Porosity or stack spacing, mean temperature, and temperature gradient over the stack were shortly discussed.
Three important performance measures were considered: temperature uniformity, mean temperature, and pressure drop.
We also observed inter-annual differences, with approximately 2 °C higher mean temperature and 30% lower mean precipitation in 2011 compared to 2010 at both field sites.
The unconditional Favre mean temperature and species mass fractions are also in reasonable agreement with measurements.
However, the bias adjustment method works better for surface mean temperature and less so for daily precipitation.
The current study found a positive association between previous August mean temperature and T. occidentalis growth.
The gray bars represent monthly mean temperature and the black bars represent monthly total precipitation.
Both mean temperature and mean daily thermal amplitude varied among the four tactics described above (Figures 2 and 3).
We used daily mean temperature and daily cumulative rainfall as explanatory variables of daily mortality.
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