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Ferguson et al. (2009) studied the potential for mixing and re-equilibration of water by examining heat and fluid flow along crustal scale faults along tectonic geothermal systems and found that significant mixing with shallow groundwater will occur resulting in an under-prediction of maximum circulation temperature by 10 35 % using silica and chalcedony geothermometers.
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The following metrics were assessed: minimum, average, and maximum temperature, maximum heat index, the exponential temperature transformation, SSC (categorical), and deviation from normal maximum temperature (categorical).
The maximum room temperature and the temperature difference from ambient are 45.5 °C and 12.25 °C for forced circulation and 41.75 °C and 8.5 °C for natural circulation respectively.
Maximum summer temperature in these ports rarely exceeds 77 °F (25 °C).
For the conditions investigated, limitation of the maximum furnace temperature to 1273 K yields that 48%, 56%, and 70% are the highest possible inlet oxygen concentrations if the external circulation flux rate is limited to 10, 20, and 30 kg/m2/s, respectively.
36C - Record maximum April temperature, Mogadishu, Somalia.
In fact, liquid helium (LHe4) brings it just about to its maximum conductance temperature: around -250°C.
41.2C - Record maximum February temperature, 1954-2012, Tak province (2005).
There is another maximum of temperature associated with this.
Maximum body temperature was 38.7 °C.
Maximum oral temperature was 37.7°C.
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