2011
DOI: 10.5937/geopan1102036g
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Influence of hail suppression on the hail trend in Vojvodina, Serbia

Abstract: The influence of hail suppression by silver iodide seeding on the trend in the number of hail days (the hail trend) in Vojvodina was studied in two cases; (1) from 1967 to 2002 when there was no hail suppression and (2) from 2003 to 2010 when hail suppression existed on the whole territory. The hail trend in Vojvodina was calculated on the basis of all observed data from all synoptic and climatological stations in the period 1967 to 2010. Previous two cases show that the hail trend was increasing when there wa… Show more

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Cited by 14 publications
(9 citation statements)
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“…In [19] very similar results of the aridity trends for De Martonne aridity and Pinna combinative indices for the territory of Vojvodina in the same period from 1949 to 2006 were obtained. It seems that aridity trend in Vojvodina really did not change in the long interval of 58 years, which is opposite to trends in temperature [43,44], precipitation [45], and hail [63], which are very variable. Very similar results of aridity trends have been obtained for the rest of Serbia's territory; for Kosovo and Metohija [20] and Central Serbia [21], where it is also found that there is no trend.…”
Section: Trendmentioning
confidence: 83%
See 1 more Smart Citation
“…In [19] very similar results of the aridity trends for De Martonne aridity and Pinna combinative indices for the territory of Vojvodina in the same period from 1949 to 2006 were obtained. It seems that aridity trend in Vojvodina really did not change in the long interval of 58 years, which is opposite to trends in temperature [43,44], precipitation [45], and hail [63], which are very variable. Very similar results of aridity trends have been obtained for the rest of Serbia's territory; for Kosovo and Metohija [20] and Central Serbia [21], where it is also found that there is no trend.…”
Section: Trendmentioning
confidence: 83%
“…In case p is greater than the significance level α, the H 0 (there is no trend) cannot be rejected. MK tests are widely used in environmental sciences, for example: temperature, precipitation, sunshine hours, cloud cover, relative humidity and wind speed [59]; temperature and precipitation [57]; precipitation [60]; extreme temperatures [43,44,58,61]; hail [62][63][64]; aridity [19,21,65]; evapotranspiration [66]; and atmospheric deposition [67]; because it is simple, robust, and can cope with missing values.…”
Section: Forestry Aridity Indexmentioning
confidence: 99%
“…MK tests are used widely in the environmental sciences, assisting in measurements and analyses of temperature, precipitation, sunshine hours, cloud cover, relative humidity and wind speed [68]; temperature and precipitation [66]; precipitation [69]; extreme temperatures [42,43,67,70]; hail [71][72][73][74]; aridity [17][18][19]32,75]; evapotranspiration [76]; and atmospheric deposition [77]. MK tests are simple, robust, and can cope with missing values.…”
Section: Discussionmentioning
confidence: 99%
“…(4), the probability p takes values between 0 and 100 in %. In fact, p is used to test the level of confidence in the hypothesis (Gavrilov et al, 2010(Gavrilov et al, , 2011(Gavrilov et al, , 2013(Gavrilov et al, , 2015. If the computed value p is lower than the chosen significance level, α (e. g., α=5%), the H 0 (there is no trend) should be rejected, and the H a (there is a significant trend) should be accepted; and if p is greater than the significance level, the H 0 cannot be rejected.…”
Section: Methodsmentioning
confidence: 99%