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Determination and Changes in Winter Severity in the Period between 1961 and 2015
Zahradníček, Pavel ; Rožnovský, J. ; Brzezina, J. ; Štěpánek, Petr ; Farda, Aleš ; Chuchma, F. ; Potopová, V.
Values of the minimum air temperatures during cold periods, especially winter, have often negative impacts on a wide range of human activities. In the past there have been many cases when rapid decrease in air temperature caused damages to machines, halted traffic etc. Every winter or cold half-year can be assessed using several parameters. In this article, three climatological characteristics were used. First was the average air temperature. Second was the sum of effective air temperatures below 0°C and -5°C. Last characteristic, which determines the extremity of that particular period, is the absolute minimum air temperature. Space-time analysis was performed for all the three characteristics. Statistically, the most significant change was found in case of the average air temperature – there is a gradual warming since 1961. Air temperatures during winter are to a large extent affected by the continentality of the climate. In Bohemia, the warming is faster than in Moravia and the western part of the country has the lowest absolute minimum air temperatures. Using multiparametric analysis of climatological characteristics it was found that the coldest winter and coldest half-year from the analyzed years was in 1963. In contrast, mildest winter was in 2007. Current climatological models predict that winter temperatures by the end of 21st century will be higher by 2.4°C to 4.9°C, which would mean a significant change in the current winter conditions.\n
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Increase in Winter Air Temperatures in the Czech Republic between 1961 and 2010
Střeštík, Jaroslav ; Rožnovský, J. ; Štěpánek, Petr ; Zahradníček, Pavel
Based on the analysis of average monthly air temperatures between 1961 and 2010 it can be statistically proven that there is an increasing trend. The actual level of increase, however, is different for each season and is also specific for a particular region – there are differences between Bohemia and Moravia. In the summer, the average monthly air temperatures rise more significantly in Moravia, where there is a higher number of stations with increase of over 1°C compared to Bohemia. This is also true for the spring, for which the difference is not so profound, and is yet smaller in the autumn. In contrast, in the winter there is a more significant increase in Bohemia, where most stations show an increase of over 0.5°C. In Moravia the increase is usually only around 0.3 to 0.4°C. Differences between the increases of average air temperature can also be seen across the individual winter months. Highest increase was found in January, where some stations in Bohemia show an increase of over 1°C, a value that was not observed in Moravia, where some stations have an increase of less than 0.8°C. In December and February, the level of increase in general is much smaller. However, given the predicted increase of air temperatures in the future in general, it can be expected that in the upcoming decades the number of warm winters will increase. Such increase of air temperatures in the winter is likely to have negative impacts for the agriculture.
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Use of Euro-CORDEX Models for Drought Prediction with Respect to Black Frosts and Rain Deficit during the Cold Season
Potopová, V. ; Štěpánek, Petr ; Zahradníček, Pavel ; Farda, Aleš ; Türkot, L. ; Hiřmanová, D.
This paper focuses on the analysis of changes in the distribution of frequency, duration and magnitude of drought for various time scales for two future time periods, 2041 - 2070 and 2071 - 2100 and compared to the reference period 1981 - 2010 under the two Representative Concentration scenarios RCP4.5 and RCP8.5. Dry events are calculated and analysed according to the classification of the standardized precipitation evapotranspiration index (SPEI) and the standardized precipitation index (SPI). Estimates of future drought projections based on the SPI tend to underestimate risk, while risk of the SPEI drought magnitude increases by the end of the century, even if precipitation increases moderately.
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Analysis of Frosts Observed in the End of April 2016 and the Associated Damages for Fruit Farming
Zahradníček, Pavel ; Rožnovský, J. ; Štěpánek, Petr ; Chuchma, F.
Air temperatures below 0°C, the so-called vegetation period frosts, have always been a problem in the climate conditions of the Czech Republic. The 2015/2016 winter as relatively mild, as well as the following beginning of spring and April. Major damages were caused by sudden rapid drop in air temperatures in the period between 25th and 30th April 2016, as a result of very cold air from the North. Air temperature began to fall on 19th April 2016, but only ground temperatures were below freezing point. Between 25th and 30th April, however, even air temperatures measured at 2m above the ground dropped below 0°C. All over the country, the minimum temperatures were below 0°C, usually between -2 and -4°C. The lowest minimum ground air temperatures were below -5°C at 85% of the area of the Czech Republic. In Moravia, the minimum ground air temperature was below 0°C on five days, in Bohemia it was every day in the period between 25th and 30th April 2016. It should be emphasized that during the flowering time of fruit trees without leaves, the flowers form an active surface. Due to radiation the flower temperature is often even lower than the measured ground air temperature minimum. This analysis does not include the effects of terrain, which determines positions of frost basins.
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Drought periods in 2014
Zahradníček, Pavel ; Trnka, Miroslav ; Štěpánek, Petr ; Semerádová, Daniela ; Farda, Aleš
The first half of year 2014 was characterized by the occurrence of extreme weather. Episode without precipitation were alternated with thunderstorms, temperature were mostly above normal and was occurred first heat wave. The year began with a very mild winter, when amount of snow was only 27% of long term average and in agricultural region South Moravia only about 10%. The winter temperature was more than 2 degrees C higher than normal. March and April were characterized by low sum of precipitation mainly again in South Moravia, both months were about 70% of long term average. March and April temperature were significantly above normal (March about more than about 4 degrees C and April more than 2 degrees C). In contrast May was cold and rainy. In the middle of the month there were persistent rainfall, which caused an increase of river levels and flooding several areas. June was again very dry. These weather conditions led to the strong dry episodes during first half of the year.
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Physiological equivalent temperature as an indicator of the UHI effect with the city of Prague as an example
Zahradníček, Pavel ; Žák, M. ; Skalák, Petr
Description of an Urban Heat Island (UHI) using the difference in air temperature is one of the world's most studied characteristics. If, however, one wants to express how the temperature is perceived by humans, one must consider the overall effect of air temperature, wind speed, air humidity and radiation flows, which is expressed using temperature bioclimatological indexes. One of them is the socalled physiological equivalent temperature (PET), which is used for quantification of the overall effect of meteorological parameters combined with human energetic balance and which is perceived by humans. The RayMan (MATZARAKIS et al. 2007, 2010) microscale models in the city of Prague were used to simulate biometeorological conditions describing the effect on humans using PET.
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Drought monitor for the Czech Republic-www.intersucho.cz
Trnka, Miroslav ; Hlavinka, Petr ; Semerádová, Daniela ; Balek, Jan ; Možný, M. ; Štěpánek, Petr ; Zahradníček, Pavel ; Hayes, M. ; Eitzinger, Josef ; Žalud, Zdeněk
Because drought and its impacts are among the worst hydrometeorological extremes (including also Central European conditions), the aim of this paper is to describe the core and use of the Integrated drought monitoring system for the Czech Republic. Land-use, information about soil, vegetation characteristics and meteorological data are used as inputs to validated water balance SoilClim model, which is applied for estimates of actual and reference evapotranspiration and water saturation of the soil profile in % or soil moisture content in mm. Moreover the prognosis of expected soil moisture (based on probabilistic analysis) is calculated for next 1, 2, 4 and 8 weeks. Main results are weekly updated in form of drought occurrence maps, which are published in spatial resolution 500 m for whole territory of the Czech Republic and for all its 76 districts separately. Final maps with detail comments are available at drought topic dedicated web page (ANONYM 3 2014).
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Application of DSSAT model to simulated thermophilic crops in central and southern Europe
Potop, V. ; Mateescu, C.D. ; Türkott, L. ; Zahradníček, Pavel ; Boroneant, C. ; Constantinescu, F. ; Iamandei, M.
This study presents applications of DSSAT version 4.5 software package to simulate thermophilic crops. The results are used to identified adaptation options to reduce impacts of climate changes, pest and diseases in thermophilic crops in the central and southeastern Europe, specifically in Elbe River lowland and Romania. For the Czech Republic, experimental research at farm level includes: (1) testing thermophilic assortment of vegetables in Elbe lowland conditions; (2) monitoring the meteorological data, phenological phases, soil characteristics, leaf area and the amount of aboveground biomass on farmer vegetable fields. For Romania, the focus is put on crop water use efficiency under current and future climate scenarios for thermophilic species (maize) in different agricultural sites from south and south-eastern regions. CERES Maize and CROPGRO-vegetables modules embedded in DSSAT were used.
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Prediction of crop yields using satellite remote sensing
Lukas, V. ; Trnka, Miroslav ; Semerádová, Daniela ; Rajdl, Kamil ; Balek, Jan ; Štěpánek, Petr ; Zahradníček, Pavel ; Hlavinka, Petr ; Žalud, Zdeněk
Knowledge of the crop yield with sufficient lead time prior to harvest is crucial for both the farm management and the agro-food sector policy. The aim of this study was to test feasibility of developing crop yield forecasting model in Czech Republic for winter wheat, spring barley and oilseed rape based on 2000-2014 database of vegetation indices Normalized Difference Vegetation Index (NDVI) and Enhanced Vegetation Index (EVI2) from Moderate Resolution Imaging Spectroradiometer (MODIS) on Terra satellite in form of 16-days composites. An average yield data were collected for 14 selected districts in the Czech Republic that represent the regions with more intensive agricultural production among varying climate and topographic conditions. The viability of the concept was proven in years with significant yield decline i.e. 2000, 2003, 2006 and 2012, when yields of cereals were significantly affected by occurred drought periods. More stable regression results were achieved in the most productive areas such as Olomouc and Prerov, whilst models in highland regions were influenced by lower acreage of three modelled crops and higher prevalence of fodder crops. In most cases, EVI2 showed higher correlations to the crop yield together with using an average value of all composites during vegetation period.
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