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We control the plume strength by prescribing its excess temperature and buoyancy flux.
Leng, W. & Zhong, S. J. Controls on plume heat flux and plume excess temperature.
The second parameter is the plume excess temperature, which is based on ref. 56.
In summertime, such anthropogenic heat gain accounts for a mere 1percentt of the heat island's excess temperature.
Unfortunately, not every plume with estimated buoyancy flux also has an estimate for excess temperature and vice versa.
The excess temperature profiles from a localized heat source are studied for various physical conditions.
Similar(22)
At present there are regional variations in excess temperature-related deaths and these are likely to persist, they added.
Putirka, K. Excess temperatures at ocean islands: implications for mantle layering and convection.
The maximum capacity of many energy resources gets negatively affected by excess temperatures.
Cells may experience both short-term (efficiency loss) and long-term (irreversible damage) degradation due to excess temperatures.
It is shown that asymmetric operation requires spatial distribution of the feed for the exothermic reaction in order to prevent excess temperatures and to ensure stable operation.
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