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Sensible heat flux (QH) is a critical driver of surface and boundary layer meteorological processes, especially in urban areas. Aerodynamic resistance methods (ARM) to model QH are promising because, in principle, all that is needed is surface temper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=core_ac_uk__::b5a77eccb7f6a3a8b98c80ba0c2cdfe2
https://centaur.reading.ac.uk/77578/1/QJ170347_Ben_Centaur.pdf
https://centaur.reading.ac.uk/77578/1/QJ170347_Ben_Centaur.pdf