Summary
Trends in extreme temperatures have been investigated for the Belgrade temperature record (1975–2003) to assess how an increase in the mean summer temperatures is related to changes in the extreme maximum and minimum temperatures. The rising mean summer temperatures at Belgrade are associated with a substantial increase in the occurrence of extreme maximum temperatures. Two statistical models for climate change (changing mean with constant standard deviation, and changing mean and standard deviation) indicated that the changing mean was dominant, because the observed trend in standard deviation was small.
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References
RC Balling JA Skindlow DA Phillips (1990) ArticleTitleThe impact of increasing summer mean temperatures on extreme maximum and minimum temperatures in Phoenix, Arizona. J Climate 3 1491–1494 Occurrence Handle10.1175/1520-0442(1990)003<1491:TIOISM>2.0.CO;2
DR Easterling B Horton (1997) ArticleTitleMaximum and minimum temperature trends for the globe. Science 227 364–367 Occurrence Handle10.1126/science.277.5324.364
DR Easterling LG Evans PY Groisman TR Karl KE Kunkel P Ambenje (2000) ArticleTitleObserved variability and trends in extreme climate events: A brief review. Bull Amer Meteor Soc 3 417–425 Occurrence Handle10.1175/1520-0477(2000)081<0417:OVATIE>2.3.CO;2
DY Gong YZ Pan JA Wang (2004) ArticleTitleChanges in extreme daily temperatures in summer in eastern China during 1955–2000. Theor Appl Climatol 77 25–37 Occurrence Handle10.1007/s00704-003-0019-2
PY Groisman TR Karl DR Easterling RW Knight PF Jamason KJ Hennessy R Suppiah CM Page J Wibig K Fortuniak VN Razuvaev A Douglas E Førland PM Zhai (1999) ArticleTitleChanges in the probability of heavy precipitation: Important indicators of climatic change. Climatic Change 42 243–283 Occurrence Handle10.1023/A:1005432803188
J Hansen I Fung A Lacis D Rind S Lebedeff R Ruedy G Russel P Stone (1988) ArticleTitleGlobal climate changes as forecast by Goddard Institute for Space Studies three-dimensional model. J Geophys Res 93 9341–9354
TR Karl G Kukla VN Razuvayev MJ Changery RG Quayle RR Heim DR Easterling CB Fu (1991) ArticleTitleGlobal warming: Evidence for asymmetric diurnal temperature change. Geophys Res Lett 18 2253–2258
RW Katz BG Brown (1992) ArticleTitleExtreme events in a changing climate: Variability is more important than averages. Climatic Change 21 289–302 Occurrence Handle10.1007/BF00139728
LO Mearns RW Katz SH Schneider (1984) ArticleTitleExtreme high-temperature events: Changes in their probabilities with changes in mean temperature. J Climate Appl Meteor 23 1601–1613 Occurrence Handle10.1175/1520-0450(1984)023<1601:EHTECI>2.0.CO;2
Nicholls N, Gruza GV, Jouzel J, Karl TR, Ogallo LA, Parker DE (1996) Observed climate variability and change. In: Houghton JT, Filho LGM, Callander BA, Harris N, Kattenberg A, Maskell K (eds) Climate Change 1995: The Science of Climate Change. Cambridge, UK: Cambridge University Press, pp 133–192
LF Tarleton RW Katz (1995) ArticleTitleStatistical explanation for trends in extreme summer temperatures at Phoenix, Arizona. J Climate 8 1704–1708 Occurrence Handle10.1175/1520-0442(1995)008<1704:SEFTIE>2.0.CO;2
Tukey JW (1977) Exploratory data analysis. Reading, MA: Addison-Wesley, 668 pp
M Unkašević (1990) ArticleTitleThe yearly averaged air temperature in Belgrade from 1888 to 1987. Atmosfera 3 305–313
M Unkašević (1991) ArticleTitleEvidence of the urban heat island in Belgrade (Yugoslavia). Beitr Phys Atmosph 1 55–63
WMO (2001) Report on the Activities of the Working Group on Climate Change Detection and Related Rapporteurs 1998–2001. Tech Note No 47 WMO Geneva 2001
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Unkašević, M., Vujović, D. & Tošić, I. Trends in extreme summer temperatures at Belgrade. Theor. Appl. Climatol. 82, 199–205 (2005). https://doi.org/10.1007/s00704-005-0131-6
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DOI: https://doi.org/10.1007/s00704-005-0131-6