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The gridded PRISM datasets were overlaid with county boundaries to compute mean temperature and precipitation values for each county (e.g., Figure 2a b).
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For each day and probe, the following parameters were computed: mean temperature, mean RH, Tmax, Tmin, RHmax, and RHmin.
From the hourly observations, we computed daily mean temperature and daily average relative humidity.
Uniformly good agreement between measured and computed mean temperatures, mean soot volume fractions and (where available) radiative fluxes is found across all flames.
We analyzed the changes in temperature on the days preceding estrus and found that an acceptable predictor of estrus could be computed as follows: 1) calculate the mean temperature at dawn for the past 5 days; 2) if today's temperature at dawn exceeds the mean of the preceding 5 days plus 3 standard deviations, then estrus will occur tomorrow.
The July mean temperature is 83 °F (28 °C).
The mean temperature this summer will be 14.4C.
log mean temperature difference.
Daily mean temperature.
log mean temperature.
Logarithmic mean temperature difference.
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