prikaz prve stranice dokumenta Analiza podataka o ozonu u graničnom sloju atmosfere otoka Visa
  Download
PDF 1.24 MB
undergraduate thesis
Analiza podataka o ozonu u graničnom sloju atmosfere otoka Visa
Osijek: Josip Juraj Strossmayer University of Osijek, Department of Chemistry, 2015. urn:nbn:hr:182:892391
Škobić, Marija
Josip Juraj Strossmayer University of Osijek
Department of Chemistry
Department of General, Inorganic and Physical Chemistry and Methodology of Chemistry

Cite this document

Škobić, M. (2015). Analiza podataka o ozonu u graničnom sloju atmosfere otoka Visa (Undergraduate thesis). Retrieved from https://urn.nsk.hr/urn:nbn:hr:182:892391

Škobić, Marija. "Analiza podataka o ozonu u graničnom sloju atmosfere otoka Visa." Undergraduate thesis, Josip Juraj Strossmayer University of Osijek, Department of Chemistry, 2015. https://urn.nsk.hr/urn:nbn:hr:182:892391

Škobić, Marija. "Analiza podataka o ozonu u graničnom sloju atmosfere otoka Visa." Undergraduate thesis, Josip Juraj Strossmayer University of Osijek, Department of Chemistry, 2015. https://urn.nsk.hr/urn:nbn:hr:182:892391

Škobić, M. (2015). 'Analiza podataka o ozonu u graničnom sloju atmosfere otoka Visa', Undergraduate thesis, Josip Juraj Strossmayer University of Osijek, Department of Chemistry, accessed 23 March 2023, https://urn.nsk.hr/urn:nbn:hr:182:892391

Škobić M. Analiza podataka o ozonu u graničnom sloju atmosfere otoka Visa [Undergraduate thesis]. Osijek: Josip Juraj Strossmayer University of Osijek, Department of Chemistry; 2015 [cited 2023 March 23] Available at: https://urn.nsk.hr/urn:nbn:hr:182:892391

M. Škobić, "Analiza podataka o ozonu u graničnom sloju atmosfere otoka Visa", Undergraduate thesis, Josip Juraj Strossmayer University of Osijek, Department of Chemistry, Osijek, 2015. Available at: https://urn.nsk.hr/urn:nbn:hr:182:892391

Please login to the repository to save this object to your list.
Metadata
TitleAnaliza podataka o ozonu u graničnom sloju atmosfere otoka Visa
Title (english)Analysis of data ozone in boindary layer atmosphere on the island Vis
AuthorMarija Škobić
MentorElvira Kovač-Andrić (mentor)
GranterJosip Juraj Strossmayer University of Osijek
Department of Chemistry
(Department of General, Inorganic and Physical Chemistry and Methodology of Chemistry)
Osijek
Defense date and country2015-09-28, Croatia
Scientific / art field,
discipline and subdiscipline		NATURAL SCIENCES
Chemistry
Abstract
Koncentracija ozona u stratosferi rezultat je dinamičke ravnoteže između kemijskih procesa nastajanja te procesa njegove razgradnje. Prisutnost ozona u nižim slojeva atmosfere (troposfera) u obliku je fotokemijskog smoga koji narušava zdravlje i smanjuje vidljivost. Najvažniji učinak na ultraljubičasto zračenje ima ozon, a danas antropogeni faktori dovode do znatnih promjena ozona koje se očituju u stvaranju ozonskih rupa i fotosmoga. U ovom će se završnom radu analizirati uloga ozona u atmosferi, njegova obilježja prostorne raspodjele te godišnji hod. Na mjernoj postaji na otoku Visu (Hum) tijekom 2014. godine mjerena je koncentracija ozona. Mjerenje koncentracije ozona ima tipični godišnji hod s niskim zimskim vrijednostima i višim ljetnim vrijednostima zbog povećanog utjecaja Sunčevog zračenja koje sudjeluje u procesu stvaranja prizemnog ozona. Također, u dnevnom hodu koncentracije ozona izraženiji je jutarnji minimum i podnevni maksimum. Meteorološki parametri koji imaju najveći utjecaj na koncentraciju ozona su relativna vlažnosti i temperatura, a brzina vjetra i smjer vjetra nemaju veći utjecaj.
Abstract (english)
Concentration of ozone in the stratosphere is a result of a dynamic balance between chemical processes of its formation and its destruction. The presence of ozone in the lower atmosphere (troposphere) is manifested in the form of photochemical smog that has a bad influence on health and reduces visibility. Ozone has the most important effect on ultraviolet radiation, and anthropogenic factors have lead to significant changes in ozone level, which are manifested in creating ozone holes and photochemical smog. In this thesis the role of ozone in the atmosphere, its characteristics of spatial distribution and the annual mean will be analyzed. During 2014, concentration of ozone at the Measuring station on the island of Vis (Hum) was measured. Typical annual mean of ozone concentration has low values in winter and higher values in summer because of increased influence of solar radiation that participates in the formation of ground-level ozone. Also, daily mean of ozone concentration has more stressed morning minimum and midday maximum. Relative humidity and temperature are meteorological parameters which have a great impact on ozone concentration while wind speed and direction don't have a momentous impact on ozone concentration.
Keywords
Keywords (english)
Languagecroatian
URN:NBNurn:nbn:hr:182:892391
Study programmeTitle: Chemistry
Study programme type: university
Study level: undergraduate
Academic / professional title: sveučilišni/a prvostupnik/prvostupnica (baccalaureus/baccalaurea) kemije (sveučilišni/a prvostupnik/prvostupnica (baccalaureus/baccalaurea) kemije)
Type of resourceText
File originBorn digital
Access conditionsOpen access
Terms of useLicence In copyright icon
RepositoryRepository of the Department of Chemistry, Osijek
Created on2016-07-15 10:25:21