| Summary: | Black carbon affects the atmosphere, clouds, and the albedo of snow. These effects of black carbon are a fact but exactly what they entail is not well known. The atmosphere, the albedo in ice crystals and snow (due to warming of the snows’ surface), clouds’ life time and cloud cover are all influenced because black carbon absorbs radiation, thus altering the radiative forcing (RF).Many models and measurements have been done to evaluate the effects of black carbon but they show very different results. This literature study examines papers and articles to see what and how much we know about black carbon and its climate effects. I conclude that there have been great differences in results that are evident due to the span that black carbon is thought to change the RF in the atmosphere (results ranging from +0.4 to +1.2 Wm-2), and snow (+0.007 to +0.054 Wm-2), as well as the albedo in snow (results ranging from -0.02 to -0.17, only including the results from studies with BC concentration of 1000 ng/g for increased comparability). I as well as many others suggest that models tend to get very different results because they use different starting conditions and equations and because models handle aerosols and clouds in different ways. This is largely because of a lack of information, especially concerning aerosols and clouds. Sot påverkar atmosfären, moln och albedot i snö. Dessa effekter av sot är ett faktum, men exakt vad de innebär är inte väl känt. Atmosfären, albedo i iskristaller och snö, uppvärmningen av snö och isytor, molns livstid och molntäckets utbredning påverkas av sot eftersom sot absorberar strålning, vilket förändra strålningsdrivningen och kan förånga moln, och att sot kan vara nuklider som kan skapa moln.Många modeller och mätningar har gjorts för att utvärdera effekterna av sot men de visar mycket olika resultat. Denna litteraturstudie undersöker artiklar för att se vad och hur mycket vi vet om sot och dess klimatpåverkan. Jag drar slutsatsen att det har finns stora skillnader i resultat vilket ...
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