Stana Simic

Dr. Stana Simic

Institute of Meteorology, University of Natural Resources and Life Sciences, Vienna, Peter-Jordan-Straße 82, Vienna A-1190, Austria

Research Focus & Metrics

Academic Career Length

28Years (1999-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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5 November 2007 in Photochemistry and Photobiology
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Journal Article
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GSGunther Seckmeyer
Gunther Seckmeyer
DPDarius Pissulla
Darius Pissulla
MGMerle Glandorf
Merle Glandorf
DHDiamantino Henriques
Diamantino Henriques
BJBjorn Johnsen
Bjorn Johnsen
FCFernanda Carvalho
Fernanda Carvalho

3 September 2019 in Scientific Reports
Verified
Journal Article
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RMRichard McKenzie
Richard McKenzie
GBGermar Bernhard
Germar Bernhard
BLBen Liley
Ben Liley
PDPatrick Disterhoft
Patrick Disterhoft
SRSteve Rhodes
Steve Rhodes
SSStana Simic
Stana Simic
The Montreal Protocol on Substances that Deplete the Ozone Layer has been hailed as the most successful environmental treaty ever (https://www.unenvironment.org/news-and-stories/story/montreal-protocol-triumph-treaty). Yet, although our main concern about ozone depletion is the subsequent increase in harmful solar UV radiation at the Earth’s surface, no studies to date have demonstrated its effectiveness in that regard. Here we use long-term UV Index (UVI) data derived from high-quality UV spectroradiometer measurements to demonstrate its success in curbing increases in UV radiation. Without this landmark agreement, UVI values would have increased at mid-latitude locations by approximately 20% between the early 1990s and today and would approximately quadruple at mid-latitudes by 2100. In contrast, an analysis of UVI data from multiple clean-air sites shows that maximum daily UVI values have remained essentially constant over the last ~20 years in all seasons, and may even have decreased slightly in the southern hemisphere, especially in Antarctica, where effects of ozone depletion were larger. Reconstructions of the UVI from total ozone data show evidence of increasing UVI levels in the 1980s, but unfortunately, there are no high-quality UV measurements available prior to the early 1990s to confirm these increases with direct observations.

21 November 2009 in Geophysical Research Letters
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AAAntti Arola
Antti Arola
Stelios KazadzisStelios Kazadzis
Stelios Kazadzis
ALAnders Lindfors
Anders Lindfors
Nickolay A. KrotkovNickolay A. Krotkov
Nickolay A. Krotkov
JKJ. Kujanpää
J. Kujanpää
SKS. Kinne
S. Kinne

23 September 2008 in Atmospheric Chemistry and Physics
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Journal Article
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PWPhilipp Weihs
Philipp Weihs
MBM. Blumthaler
M. Blumthaler
HRHarald Rieder
Harald Rieder
AKA. Kreuter
A. Kreuter
SSStana Simic
Stana Simic
ATA. Tanskanen
A. Tanskanen
A measurement campaign was performed in the region of Vienna and its surroundings from May to July 2007. Within the scope of this campaign erythemal UV was measured at six ground stations within a radius of 30 km. First, the homogeneity of the UV levels within the area of one satellite pixel was studied. Second, the ground UV was compared to ground UV retrieved by the ozone monitoring instrument (OMI) onboard the NASA EOS Aura Spacecraft. During clear-sky conditions the mean bias between erythemal UV measured by the different stations was within the measurement uncertainty of ±5%. Short term fluctuations of UV between the stations were below 3% within a radius of 20 km. For partly cloudy conditions and overcast conditions the discrepancy of instantaneous values between the stations is up to 200% or even higher. If averages of the UV index over longer time periods are compared the difference between the stations decreases strongly. The agreement is better than 20% within a distance of 10 km between the stations for 3 h averages. The comparison with OMI UV showed for clear-sky conditions higher satellite retrieved UV values by, on the average, approximately 15%. The ratio of OMI to ground measured UV lies between 0.9 and 1.5. and strongly depends on the aerosol optical depth. For partly cloudy and overcast conditions the OMI derived surface UV estimates show larger deviation from the ground-based reference data, and even bigger systematic positive bias. Here the ratio OMI to ground data lies between 0.5 and 4.5. The average difference between OMI and ground measurements is +24 to +37% for partly cloudy conditions and more than +50% for overcast conditions.

Daniela HaluzaDaniela Haluza
Daniela Haluza
SSStana Simic
Stana Simic
JHJan Hoeltge
Jan Hoeltge
RCRenate Cervinka
Renate Cervinka
Hanns MoshammerHanns Moshammer
Hanns Moshammer
Connectedness to nature (CN) influences motivation to have contact with outdoor natural environments. Spending leisure time in natural environments is beneficial for human health and well-being. Besides these positive effects, health risks of open-air activities are mainly related to unprotected sun light exposure-associated acute and chronic skin hazards. Thus, we conducted a cross-sectional, representative telephone survey among Austrian residents to study the association of perceived CN level with sun-exposure knowledge, tanning habits, and sun protective behaviour. In total, 1,500 study subjects (50.5% females) participated in this questionnaire survey. Although knowledge about tanning and motives to tan were similar among genders, females performed more photoprotective measures and were more connected to nature (all p < 0.001) compared to males. Older age and outdoor sport were significant gender-independent predictor variables influencing perceived CN level. Additionally, level of education was relevant in male CN, whereas non-smoking and higher knowledge were predictive of female CN. This survey provides so far unreported empirical data on the relationship between nature connectedness and skin health-relevant recreational habits of Austrian residents. The findings suggest to integrate hitherto neglected gender-specific Public (Skin) Health promotion when counselling on the manifold health advantages of outdoor activities.

15 August 2001 in Geophysical Research Letters
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Journal Article
Open access
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PWPhilipp Weihs
Philipp Weihs
JLJ. Lenoble
J. Lenoble
MBM. Blumthaler
M. Blumthaler
TMT. Martin
T. Martin
GSG. Seckmeyer
G. Seckmeyer
SSStana Simic
Stana Simic
We compare three different methods for determining an average ‘effective‧ UV albedo. These methods are applied to spectral irradiance data from a measurement campaign held in the German Alps during the spring of 1999. The first method is based on the comparison of measurements of absolute levels of UV irradiance with model calculations. The second method takes advantage of changes in the spectral slope of spectral UV irradiance, which is a function of the surface albedo. In the third method, the surrounding area is partitioned into snow‐covered and snow‐free regions, and the effective albedo estimated by applying a higher or lower reflectivity to each facet before integrating over the surroundings. We present the differences and the correlations between the various methods as well as the results for the different locations.