The paper presents temporal and spatial differentiation of monthly and annual sums of atmospheric precipitation at three stations located in Cracow’s surroundings along a longitudinal profile: Garlica Murowana (representing the Cracow- Częstochowa Upland), Cracow-Botanical Garden (in the Vistula river valley) and Gaik-Brzezowa (in the Wieliczka Foothills, a part of the Carpathian Foothills), in the years 1971-2005. In summer, the precipitation was by 20% higher in Gaik-Brzezowa and in winter by 25% lower in Garlica than at other two stations. The highest mean annual precipitation sum was characteristic for Gaik: 747.5 mm (Table 1). The largest variability is typical for the precipitation in Garlica, especially in cold half-year (Figure 1). The highest annual precipitation sums were noted in 2001 in Garlica (865.2 mm) and Cracow (845.9 mm) and in 1974 in Gaik (1178.7 mm), while the lowest annual sums occurred everywhere in 1993 (446.1, 482 and 524.8 mm, respectively). The precipitation sums show large inter-annual variability, high irregularity and lack of any clear tendency (Table 2, Figure 2). Mean annual number of days with precipitation reached 132 mm in Garlica, 168 mm in Gaik and 216.4 mm in Cracow but in case of the days with daily precipitation sum ≥5 mm ...
Meteorological conditions have a considerable impact on water relations and the state of forest hydrogenic habitats. Variation in atmospheric precipita-tion and air temperatures are of particular relevance. The presented meteoro-logical parameters obtained between 1986 and 2008 from the meteorological station in Zielonka included: annual and halfyear precipitation sums; drought frequencies; number of days by quantity; mean annual and half-year air tempera-tures; number of days of different temperature categories; duration of the mete-orological growing season; beginning and completion of the meteorological growing season. The study results indicated the occurrence of changes in the values of the above-specified parameters. From 1987 to 2007 the mean precipitation value was 541 mm. In Zielonka nearly 5 droughts in a year and 2–3 during the summer half-years were noted. In recent years, a decrease in days with precipitation below 1 mm and above 20 mm was recorded. The mean annual air temperatures and mean temperatures of the winter and summer halfyears show a rising tendency. This is the result of changes in the number of days with extreme temperatures. In recent years, the number of days with the average temperature between -5.0 and 15.0°C has decreased while the number of days with temperature above ...
The aim of the study was an intercomparison of precipitation measurementswith classic (Hellmann) and automatic (tipping-bucket) rain gauges. Basing on theprecipitation data some agricultural factors were calculated. With the obtained results,prospects for automatic data use for agricultural enterprise were evaluated,along the homogenious series maintaining.The investigation was based on data obtained in years 2000-2004 fromclassic and automatic (Eijkelkamp) weather stations set in Mochełek near Bydgoszcz.It was supposed that in agrometeorological research the fundamental intervalof a factor is its ten-days value. Series of number from 15 to 180 (a ten-daysmeans in monts, seasons, warm and cold half-a-year and a year) obtained fromclassic and automatic measurements were compared. A particular consideration ofcorrelative results was done to assign mathematical formulas that would allow usethe Hellmann and tipping-bucket rain gauges data series exchangeably. ...
Meteorological conditions have a potential impact on forest economy. Var-iation in atmospheric precipitation and air temperatures are of particular relev-ance. The presented meteorological parameters obtained between 1987 (1986) and 2008 from the meteorological station in Zielonka included: annual, half-year and monthly precipitation sums; snow cover characteristic, drought frequencies; number of days by quantity; mean annual, half-year and monthly air temperatures; number of days of different temperature categories; duration of the meteorological growing season; beginning and completion of the meteorological growing season, period without slight frost. The study results indicated the occurrence of changes in the values of the above-specified parameters. From 1987 to 2008 the mean precipitation value was 531mm. In Zielonka nearly 5 droughts in a year and 2-3 during the summer half-years were noted. In recent years, a de-crease in days with precipitation below 1mm was recorded. The mean annual air temperatures and mean temperatures of the winter and summer half-years show a rising tendency. This is the result of changes in the number of days with extreme temperatures. In recent years, the number of days with the average temperature between -5.0 and 15.0°C has decreased while the number of days with temperature above +15.0°C has increased. The ...
The distribution of precipitation is a particularly important factor in periods of critical crop plants which the greatest demand for water. At this work a number of meteorological characteristics associated with precipitation got in Puczniew station in years 1972-2002 were analysed: annual and six-month sums of precipitation; changeability of sums of annual and six-month precipitation (with using the division of years and months on extremely dry, very dry, dry, average, wet, very wet and extremely wet surface); number of days with precipitation (in periods < 10 mm, 10.1 -20 mm, 20,1-30,0,0 mm, 30.1-40.0 mm and above 60.0 mm); appearing of rainless periods. In examined 31-years from1972 to 2002 the averaged annual sum of falls in Puczniew amounted to 540.7 mm. From performed analysis we obtained none of years extremely dry and particularly humid: 2 years stayed ranked to dry, 27 - up to averages, 2 - to humid. Years 1983 and 1989 were dry, however year 1977 was humid and 2001 very humid. On average within one year it appeared about 3 rainless periods, appearing mostlyin summer year (59% of cases), and dominating droughts have lengths from 9 up to 17 days (90%). ...
An important effect of temperature increase due to global warming is the possibility of decreasing agricultural efficiency of atmospheric precipitation as well as the change in the fundamental components of water balance due to increase in evaporation, which is accompanied by the absence of clear precipitation trends in the temperate European zones. The subject of this article is to determine the values of atmospheric precipitation, which during the drought phase should be supplemented with irrigation values so that it does not lower the moisture of the active soil layer in terms of the recent mean levels. We should also take into account different temperature scenarios (1.0, 1.5 and 2.0°C). The multiple-step regression model that has been calculated taking into account the level of soil moisture, air temperature and precipitation indicates that for a mean 10-day period (decade) during the growing season (April-October) the values obtained are 2.2, 3.6 and 5.2 mm, as well as 46, 76 and 109 mm in the entire growing season respectively. This particular model was devised for the city of Poznan and its vicinities, which is situated in north-western Poland. ...
The aim of this study was to determine of influence of atmospheric precipitations in flow to sewer system on temperature and the amount of raw sewage flowing into the sewage treatment plant. Studies carried out in the sewer system with a length of 15 km and a diameter of from 200 to 315 mm. Were chosen two characteristics winter study periods. The first period was from 01 to 31 January 2011 year and the second period was from 01 to 29 February 2012 year. The analysis found that as a result of accidental water inflow (rain water) occurred lowering the temperature of the influent wastewater to the treatment plant from 2.1 to 2.2 °C. Water flowing random (rainy water) is defined as the share of accidental waters in the total volume of waste water treatment plants result in an increased volume of sewage from 37.5 to 40.0%. To prevent negative phenomena which are reducing the temperature of plants and their increased volume as a result of the entry of rain water drains should be taken to detect and elimination of illegal connections residential gutters and sealed sewer system. ...
The objective of the work, carried out as part of research programme on current change of the regional climate, was to confirm the hypothesis about the increasing frequency and intensity of droughts occurring during the high water needs of corn, during the period of June and July, in the region of Pomorze and Kujawy in the years 1981-2010. Furthermore, the aim was to confirm a significant relationship between indicators characterizing meteorological and agricultural droughts. Material for the research was data from five meteorological measuring points located in the region. Statistical methods used in climatological studies were applied, particularly the method of trends. The average multi-annual totals (1981-2010) of rainfall in the period of high water needs of corn (June-July) in the region of the Pomorze and Kujawy were characterized by spatial variability amounts to 22.6%. The frequency of meteorological drought in June through July is 26.7-33.3%. In the analyzed period there were no significant changes in the frequency and intensity of these droughts with the passage of years. Rainfall shortages in corn production extend to maximum of -91 to -124 mm, depended on the locality. The shortages did not show any significant changes in the years of the study. ...
The study aimed to determine the differences in lawn irriga-tion needs resulting from the topographical heterogeneity of the city of Bydgoszcz and surrounding areas. To gather the data, me-teorological measurements were carried out in the period from May to September 2012-2014, in areas diversified in terms of the degree of urbanization and land cover: the center of a large city, urban peripheries and rural area. Based on the calculated water needs of the lawn, the range of rainfall deficits during the lawn growing period was determined. It was found that seasonal rain-fall totals in the compared locations were at a similar level, but a large temporal variability of this indicator was observed in indi-vidual seasons. In terms of evapotranspiration, clear differences were noted between the analysed locations. On average, the high-est amounts of potential evapotranspiration were found in the city center, which may be the result of the urban heat island phenome-non forming over this area. However, the lowest water loss due to evapotranspiration took place in the rural area. As a result of these, the analysis showed that the lawn's irrigation needs were characterized by both temporal and spatial variability. By far the greatest irrigation needs occurred in urban ...