Meteorological extremes and climatic change in Serbia

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Meteorological extremes and climatic change in Serbia (en)
Метеоролошки екстреми и климатске промене у Србији (sr)
Meteorološki ekstremi i klimatske promene u Srbiji (sr_RS)
Authors

Publications

Global warming impact on climate change in Serbia for the period 1961-2100

Vuković, Ana J.; Vujadinović, Mirjam; Rendulić, Sonja M.; Đurđević, Vladimir; Ruml, Mirjana; Babić, Violeta; Popović, Dunja P.

(Univerzitet u Beogradu - Institut za nuklearne nauke Vinča, Beograd, 2018)

TY  - JOUR
AU  - Vuković, Ana J.
AU  - Vujadinović, Mirjam
AU  - Rendulić, Sonja M.
AU  - Đurđević, Vladimir
AU  - Ruml, Mirjana
AU  - Babić, Violeta
AU  - Popović, Dunja P.
PY  - 2018
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/932
AB  - Serbia is situated at Balkan Peninsula, and currently majority of the territory is under warm temperate fully humid climate type with warm summers (Cfb type, according to Koppen-Geiger Climate Classification). Observed changes in climate conditions since 1961 until present time show significant increase in temperature change and change in precipitation patterns. Disturbances in heat conditions, which are recorded to affect human health, agricultural production and forest ecosystem, are priority in climate change analysis and application in adaptation planning. Future change analysis show accelerated increase of temperature by the end of the 21st century, which proves the needs for immediate measures for mitigation of negative impacts. Temperature increase averaged over the territory of Serbia is 1.2 degrees C for the period 1996-2015 with respect to the period 1961-1980, with highest increase of maximum daily temperature during the summer season, 2.2 degrees C. Using high resolution multi-model ensemble approach for analysis of the future changes with respect to the base period 1986-2005, in compliance with Intergovernmental Panel on Climate Change (IPCC) fifth assessment report (ARS), it is estimated that temperature may increase by 1.9 degrees C according to Representative Concentration Pathway 4.5 (RCP4.5) scenario and by 4.4 degrees C according to RCP8.5 by the end of the century. Spatial distribution of temperature increase, intensification of high precipitation events and decrease of summer precipitation, show intrusion of subtropical climate over the Serbia and increase of high temperature and high precipitation risks. Results presented in this paper, using high-resolution multi-model ensemble approach, provide climate change information for short term to long term planning in different sectors of economy and preservation of human health and environment.
PB  - Univerzitet u Beogradu - Institut za nuklearne nauke Vinča, Beograd
T2  - Thermal Science
T1  - Global warming impact on climate change in Serbia for the period 1961-2100
EP  - 2280
IS  - 6
SP  - 2267
VL  - 22
DO  - 10.2298/TSCI180411168V
UR  - conv_1384
ER  - 
@article{
author = "Vuković, Ana J. and Vujadinović, Mirjam and Rendulić, Sonja M. and Đurđević, Vladimir and Ruml, Mirjana and Babić, Violeta and Popović, Dunja P.",
year = "2018",
abstract = "Serbia is situated at Balkan Peninsula, and currently majority of the territory is under warm temperate fully humid climate type with warm summers (Cfb type, according to Koppen-Geiger Climate Classification). Observed changes in climate conditions since 1961 until present time show significant increase in temperature change and change in precipitation patterns. Disturbances in heat conditions, which are recorded to affect human health, agricultural production and forest ecosystem, are priority in climate change analysis and application in adaptation planning. Future change analysis show accelerated increase of temperature by the end of the 21st century, which proves the needs for immediate measures for mitigation of negative impacts. Temperature increase averaged over the territory of Serbia is 1.2 degrees C for the period 1996-2015 with respect to the period 1961-1980, with highest increase of maximum daily temperature during the summer season, 2.2 degrees C. Using high resolution multi-model ensemble approach for analysis of the future changes with respect to the base period 1986-2005, in compliance with Intergovernmental Panel on Climate Change (IPCC) fifth assessment report (ARS), it is estimated that temperature may increase by 1.9 degrees C according to Representative Concentration Pathway 4.5 (RCP4.5) scenario and by 4.4 degrees C according to RCP8.5 by the end of the century. Spatial distribution of temperature increase, intensification of high precipitation events and decrease of summer precipitation, show intrusion of subtropical climate over the Serbia and increase of high temperature and high precipitation risks. Results presented in this paper, using high-resolution multi-model ensemble approach, provide climate change information for short term to long term planning in different sectors of economy and preservation of human health and environment.",
publisher = "Univerzitet u Beogradu - Institut za nuklearne nauke Vinča, Beograd",
journal = "Thermal Science",
title = "Global warming impact on climate change in Serbia for the period 1961-2100",
pages = "2280-2267",
number = "6",
volume = "22",
doi = "10.2298/TSCI180411168V",
url = "conv_1384"
}
Vuković, A. J., Vujadinović, M., Rendulić, S. M., Đurđević, V., Ruml, M., Babić, V.,& Popović, D. P.. (2018). Global warming impact on climate change in Serbia for the period 1961-2100. in Thermal Science
Univerzitet u Beogradu - Institut za nuklearne nauke Vinča, Beograd., 22(6), 2267-2280.
https://doi.org/10.2298/TSCI180411168V
conv_1384
Vuković AJ, Vujadinović M, Rendulić SM, Đurđević V, Ruml M, Babić V, Popović DP. Global warming impact on climate change in Serbia for the period 1961-2100. in Thermal Science. 2018;22(6):2267-2280.
doi:10.2298/TSCI180411168V
conv_1384 .
Vuković, Ana J., Vujadinović, Mirjam, Rendulić, Sonja M., Đurđević, Vladimir, Ruml, Mirjana, Babić, Violeta, Popović, Dunja P., "Global warming impact on climate change in Serbia for the period 1961-2100" in Thermal Science, 22, no. 6 (2018):2267-2280,
https://doi.org/10.2298/TSCI180411168V .,
conv_1384 .
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