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Extreme daily precipitation in Belgrade and their links with the prevailing directions of the air trajectories

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Abstract

The main goal of this study was to present the statistical analysis of the daily precipitation exceeding 20 mm in Belgrade and their links with the prevailing directions of the air trajectories at 500, 1,500 and 5,000 m. For the extreme precipitation analysis, the generalised extreme value (GEV) distribution and generalised Pareto distribution (GPD) were used. The estimated return levels for 100- and 10-year return periods using GEV and GPD were obtained. Four-day backward trajectory simulations were conducted for days with precipitation exceeding 20 mm to investigate the regional transport of the air moisture towards Belgrade using the hybrid single-particle Lagrangian integrated trajectory model. The air trajectories were classified into 13 trajectory categories by the origin and direction of their approach to Belgrade. Three of the most frequent categories of air flow from south-west, south-east and north-west contributed to more than a half of the observed precipitation. Almost 74.5 % of precipitation totals in Belgrade fell during the warmer part of the year. These were directly connected with the intensive convection of colder and humid, usually maritime, air masses.

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References

  • Alexander LV et al (2006) Global observed changes in daily climate extremes of temperature and precipitation. J Geophys Res 111:D05109. doi:10.1029/2005JD006290

    Article  Google Scholar 

  • Anagnostopoulou C, Flocas H, Maheras P, Patrikas I (2004) Relationship between atmospheric circulation types over Greece and western–central Europe during the period 1958–1997. Int J Climatol 24:1745–1758

    Article  Google Scholar 

  • Anagnostopoulou C, Tolika K, Maheras P (2009) Classification of circulation types: a new flexible automated approach applicable to NCEP and GCM data sets. Theor Appl Climatol 96:3–15

    Article  Google Scholar 

  • Beirlant J, Goegebeur Y, Segers J, Teugels J (2004) Statistics of extremes: theory and applications. Wiley, Chichester

    Book  Google Scholar 

  • Bordi I, Fraedrich K, Petitta M, Sutera A (2007) Extreme value analysis of wet and dry periods in Sicily. Theor Appl Climatol 87:61–71

    Article  Google Scholar 

  • Brunetti M, Buffoni L, Maugeri M, Nanni T (2000) Precipitation intensity trends in northern Italy. Int J Climatol 20:1017–1031

    Article  Google Scholar 

  • Coles SG (2001) An introduction to statistical modeling of extreme values. Springer, London

    Google Scholar 

  • Deidda R (2010) A multiple threshold method for fitting the generalized Pareto distribution to rainfall time series. Hydrol Earth Syst Sci 14:2559–2575

    Article  Google Scholar 

  • Djordjević D, Tošić I, Unkašević M, Djurašković P (2010) Water-soluble main ions in precipitation over the southeastern Adriatic region: chemical composition and long-range transport. Environ Sci Pollut Res (ESPR) 17:1591–1598

    Article  Google Scholar 

  • Draxler RR (2006) The use of global and mesoscale meteorological model data to predict the transport and dispersion of tracer plumes over Washington, D.C. Weather Forecast 21:383–394

    Article  Google Scholar 

  • Draxler RR, Hess GD (1997) Description of the Hysplit_4 modeling system, NOAA Tech Memo ERL ARL-224, Dec, 24 pp

  • Draxler RR, Hess GD (1998) An overview of the Hysplit_4 Modeling System for trajectories, dispersion, and deposition. Aust Meteorol Mag 47:295–308

    Google Scholar 

  • Draxler RR, Rolph GD (2011) HYSPLIT (HYbrid Single-Particle Lagrangian Integrated Trajectory) model access via NOAA ARL READY Website (http://ready.arl.noaa.gov/HYSPLIT.php). NOAA Air Resources Laboratory, Silver Spring, MD

  • Hellström C (2005) Atmospheric conditions during extreme and non-extreme precipitation events in Sweden. Int J Climatol 25:631–648

    Article  Google Scholar 

  • Hsu Y, Holsen TM, Hopke PK (2003) Locating and quantifying PCB Sources in Chicago: receptor modeling and field sampling. Environ Sci Technol 37(4):681–690

    Article  Google Scholar 

  • Huth R (2001) Disaggregating climatic trends by classification of circulation patterns. Int J Climatol 21:135–153

    Article  Google Scholar 

  • Kalnay E, Kanamitsu M, Kistler R, Collins W, Deaven D, Gandin L, Iredell M, Saha S, White G, Woollen J, Zhu Y, Chelliah M, Ebisuzaki W, Higgins W, Janowiak J, Mo KC, Ropelewski C, Wang J, Leetmaa A, Reynolds R, Jenne R, Joseph D (1996) The NCEP/NCAR 40-Year Reanalysis Project. Bull Am Meteorol Soc 77:437–471

    Article  Google Scholar 

  • Katz RW, Parlange MB, Naveau P (2002) Statistics of extremes in hydrology. Adv Water Resour 25:1287–1304

    Article  Google Scholar 

  • Klein Tank AMG, Können GP (2003) Trends in indices of daily temperature and precipitation extremes in Europe, 1946–99. J Clim 16:3665–3680

    Article  Google Scholar 

  • Klein Tank AMG, Zwiers FW, Zhang X (2009) Guidelines on Analysis of extremes in a changing climate in support of informed decisions for adaptation. WCDMP-72, WMO-TD 1500, Geneva, Switzerland

  • Kyselý J, Huth R (2006) Changes in atmospheric circulation over Europe detected by objective and subjective methods. Theor Appl Climatol 85:19–36. doi:10.1007/s00704-005-0164-x

    Article  Google Scholar 

  • Levene H (1960) Contributions to probability and statistics. Stanford University Press, Stanford, pp 278–292

    Google Scholar 

  • Maheras P, Flocas HA, Chr A, Patrikas I (2002) On the vertical structure of composite surface cyclones in the Mediterranean region. Theor Appl Climatol 71:199–217

    Article  Google Scholar 

  • Peterson TC, Folland C, Gruza G, Hogg W, Mokssit A, Plummer N (2001) Report on the activities of the Working Group on Climate Change Detection and Related Rapporteurs 1998–2001. World Meteorological Organisation Rep. WCDMP-47, WMO-TD 1071, Geneva, Switzerland, 143 pp

  • Poissant L (1999) Potential sources of atmospheric total gaseous mercury in the St. Lawrence River valley. Atmos Environ 33:2537–2547

    Article  Google Scholar 

  • Radinović Dj (1987) Mediterranean cyclones and their influence on the weather and climate. PSMP Report Series, No. 24, WMO, 131 pp

  • Reiss R, Thomas M (2001) Statistical analysis of extreme values from insurance, finance, hydrology and other fields. Birkhauser, New York

    Google Scholar 

  • Rolph GD (2011) Real-time Environmental Applications and Display sYstem (READY) Website (http://ready.arl.noaa.gov). NOAA Air Resources Laboratory, Silver Spring, MD

  • Santos CS, Delabie JHC, Fernandes GW (2008) A 15-year post evaluation of the fire effects on ant community in an area of Amazonian forest. Rev Bras Entomol 52:82–87

    Article  Google Scholar 

  • Sjöstrom DJ, Welker JM (2009) The influence of air mass source on the seasonal isotopic composition of precipitation, eastern USA. J Geochem Explor. doi:10.1016/j.gexplo.2009.03.001

  • Smith RL (2003) Statistics of extremes, with applications in environment, insurance and finance. http://www.stat.unc.edu/postscript/rs/semstatrls.ps, 62 pp

  • Tolika K, Chr A, Maheras P, Kutiel H (2007) Extreme precipitation related to circulation types for four case studies over the Eastern Mediterranean. Adv Geosci 12:87–93

    Article  Google Scholar 

  • Trigo IF, Bigg GR, Davies TD (2002) Climatology of cyclogenesis mechanisms in the Mediterranean. Mon Weather Rev 130:549–569

    Article  Google Scholar 

  • Unkašević M, Radinović DJ (2000) Statistical analysis of daily maximum and monthly precipitation at Belgrade. Theor Appl Climatol 66:241–249

    Article  Google Scholar 

  • Unkašević M, Tošić I (2011) A statistical analysis of the daily precipitation over Serbia: extremes and indices. Theor Appl Climatol 106:69–78

    Article  Google Scholar 

Download references

Acknowledgments

This study was supported by the Serbian Ministry of Science, under grant 176013. The authors gratefully acknowledge the NOAA Air Resources Laboratory (ARL) for the provision of the HYSPLIT transport and dispersion model and/or READY website (http://www.arl.noaa.gov/ready.php) used in this publication.

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Correspondence to I. Tošić.

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Tošić, I., Unkašević, M. Extreme daily precipitation in Belgrade and their links with the prevailing directions of the air trajectories. Theor Appl Climatol 111, 97–107 (2013). https://doi.org/10.1007/s00704-012-0647-5

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