20.500.12556/DKUM-11104 FIZIKALNO OZADJE KLIMATSKIH MODELOV IN UPORABA PRI POUKU FIZIKE PHYSICS OF CLIMATE MODELS AND APPLICATIONS IN TEACHING PHYSICS V zadnjem stoletju se je povprečna temperatura na Zemlji dvignila za 0,7 K. Segrevanje atmosfere je odvisno od mnogih parametrov. V diplomskem delu sem študirala fizikalno ozadje klimatskih modelov in pripravila predlog za uporabo pri pouku fizike. Najprej sem opisala naravne pojave, ki vplivajo na segrevanje atmosfere. Nato sem opisala fizikalne osnove klimatskih modelov ter prvi preprost Fourierev model. V osrednjem delu diplome sem izračunala povprečno temperaturo na Zemlji pri štirih različnih pogojih: - Zemlja brez atmosfere - Zemlja z enakomerno atmosfero - Zemlja obdana z zrakom - Zemlja poraščena z gozdom. Pokazala sem, kako koncentracije ogljikovega dioksida in ostalih toplogrednih plinov vplivajo na emisivnost in na povprečno temperaturo Zemljine atmosfere. Izračunane modele sem predstavila z računalniškim programom »Spreminjanje temperature«, ki računa povprečno temperaturo na Zemlji v odvisnosti od emisivnosti in je primeren za uporabo pri pouku fizike v šoli. In the last century the average temperature on Earth has risen for 0,7 K. The warming of the atmosphere depends on several parameters. In my diploma work I studied the physical background of climate models and prepared a proposal for use in teaching of physics. First I described natural events which affect the warming of atmosphere. Further on I described the physical principles of climate models and the first simple Fourier model. In the body of the diploma work I calculated the average temperature on Earth under four different conditions: - Earth without atmosphere - Earth with steady atmosphere - Earth encircled with air - Earth covered with forest. I indicated how the concentration of carbon dioxide and other greenhouse gases affect the emissions and the average temperature of Earth's atmosphere. I presented the calculated models with a computer program »Changing the temperature«, which calculates the average temperature on Earth as a function of emissivity and can be used in teaching physics in school. Klima energijsko ravnovesje gozd povprečna temperatura topla greda Climate energy balance forest average temperature greenhouse true true false [M. Strmšek] Slovenski jezik Angleški jezik Diplomsko delo 2009-06-30 20:17:10 2009-11-17 14:07:50 2022-04-11 23:30:23 2022-04-17 03:30:39 2009 0 Maribor 0 0000-00-00 NiDoloceno NiDoloceno NiDoloceno 0000-00-00 0000-00-00 0000-00-00 53(043.2) 17221640 URN:SI:UM:DK:9YRGUB2Z UNI_Stermsek_Mateja_2009.pdf UNI_Stermsek_Mateja_2009.pdf 1 C04E1F9D6C30506313B3ECA2B754738E b10fd1da17f7aea536719e40024ecb87d7496ffcd6b7e515f10589df0b69fdd5 06302b0b-7c03-11eb-bb7a-00155d0001ca 20.500.12556/dkum/aa9ef97a-5bd8-4ef1-8e32-ce913e64a55d https://dk.um.si/Dokument.php?lang=slv&id=9651 Fakulteta za naravoslovje in matematiko 0 0 0