"RIV/61989592:15310/09:00010057!RIV10-MSM-15310___" . "Ogrin, Darko" . . . "15310" . "[C6D66EE85C7F]" . . "1"^^ . . . "0354-0596" . "SI - Slovinsk\u00E1 republika" . . . . "2"^^ . "Dela" . . . "Portable thermal camera as a tool in topoclimatic research" . "31" . "334418" . "P(2B06101)" . . . "portable thermal camera; thermal monitoring; active surface; emisivity; surface temperature; topoclimate"@en . "RIV/61989592:15310/09:00010057" . . "Portable thermal camera as a tool in topoclimatic research"@en . "14"^^ . "Vysoudil, Miroslav" . . . "Portable thermal camera as a tool in topoclimatic research"@en . "The article presents possibilities of portable infrared camera as a tool of topoclimate research refine on the base of most extended active surfaces differences in the landscape. In the account was turned daily time, aspect and morphography of monitored areas, and active surface character. Experimental measurement was carried out in Koper (SI) and Olomouc (CZ) surroundings during spring and summer months. The geographical location, inhomogeneity and thus different active surface physical properties constitute main reasons timely and spatial differences its surface tempereture. The surface temperature influents temperature regime of surface atmosphere layer contiguous. The both, inhomogeneity and different active surface physical properties also influent directly the value of its emissivity. The informations about surface temperature provide satellite, aerial and surface thermal images. The portable thermal camera monitoring represents one of possible way how to obtain surface thermal images in topoc" . "Portable thermal camera as a tool in topoclimatic research" . . "31" . . . "The article presents possibilities of portable infrared camera as a tool of topoclimate research refine on the base of most extended active surfaces differences in the landscape. In the account was turned daily time, aspect and morphography of monitored areas, and active surface character. Experimental measurement was carried out in Koper (SI) and Olomouc (CZ) surroundings during spring and summer months. The geographical location, inhomogeneity and thus different active surface physical properties constitute main reasons timely and spatial differences its surface tempereture. The surface temperature influents temperature regime of surface atmosphere layer contiguous. The both, inhomogeneity and different active surface physical properties also influent directly the value of its emissivity. The informations about surface temperature provide satellite, aerial and surface thermal images. The portable thermal camera monitoring represents one of possible way how to obtain surface thermal images in topoc"@en .