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Wyświetlanie 1-2 z 2
Tytuł:
Maksymalny czas trwania głębokich niżówek letnich w środkowej Polsce i jego uwarunkowania
Maximum duration of extreme summer low flows in Central Poland and its determinants
Autorzy:
Edmund, Tomaszewski
Powiązania:
https://bibliotekanauki.pl/articles/945277.pdf
Data publikacji:
2007
Wydawca:
Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego
Tematy:
niżówka
Polska Centralna
głęboka niżówka letnia
recesja przepływu niżówkowego
prawdopodobieństwo
Opis:
Maximum duration of extreme summer flows in central Poland was estimated on the base of hydrometric data including twenty four hour flow series from the 1966-1983 period, which were published by IMGW. There were 29 water gauges located in Warta, Pilica and Bzura drainage basins (Fig. l) shortlisted for the analysis. Low flow periods were sectioned basing on a border flow SNQ - a principle was that the period with flows below the borderline had lasted at least 5 days, while low flows followed in succession had to be divided by periods of flows higher than SNQ being minimum 3 days long. Maximum summer flows were at that time very differentiated and their length fluctuated from 10 to 282 days (Fig. 2). According to that some kind of spatial order can be outlined here, the longest low flow periods appeared in Great Poland and Warsaw - Berlin Glacial Valley (Fig. 3). Maximum length of low flow was significantly correlated with the parameters, which illustrated flow recession time, mean time of low flow or extreme time constitution in total low flow and extreme low flow time (Fig. 4, 8). The parameters of maximum length probability distribution were estimated as well. On the base of those calculations was estimated the probability of not achieving the maximum, which was empirically confirmed. Values fluctuated from 90-99.2% usually being about 96% (Fig. 6). The greatest probability of lengthening of maximum low flow periods had Great Poland Rivers (Mogilnica, Wrześnica, Lutynia), while the smallest probability was characteristic for rivers, which origins are in uplands (Warta - Poraj, Pilica - Przedbórz).
Źródło:
Acta Universitatis Lodziensis. Folia Geographica Physica; 2008, 8
1427-9711
2353-6063
Pojawia się w:
Acta Universitatis Lodziensis. Folia Geographica Physica
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ekstremalne stany wód podziemnych w środkowej Polsce w wieloleciu 1951-2000
Extreme groundwater levels in Central Poland in 1951-2000
Autorzy:
Tomalski, Przemysław
Powiązania:
https://bibliotekanauki.pl/articles/945260.pdf
Data publikacji:
2007
Wydawca:
Uniwersytet Łódzki. Wydawnictwo Uniwersytetu Łódzkiego
Tematy:
stan wody
współczynnik autokorelacji
wody podziemne
środkowa Polska
niżówka
Opis:
W artykule omówiono skład fIzykochemiczny opadów atmosferycznych, wód gruntowych i roztworów porowych. Wody (roztwory) porowe uzyskano za pomocą metody ciśnieniowej z prób gruntów gliniasto-piaszczystych i piaszczystych, pobranych w regionie łódzkim i bełchatowskim. Ustalenie składu jonowego wód pozwoliło na określenie ich typów hydrochemicznych oraz wzajemnych związków między poszczególnymi rodzajami wód. Wskazano również na czynniki antropogeniczne wpływające na zmiany składu wód opadowych, porowych i gruntowych
The aim of this study is to present an analysis of sequence of extreme annual groundwater levels in central part of Poland. Data were obtained from 55 groundwater levels (Fig. I),which were monitored in Institute of Meteorology and Water Management. Every sequence has its own theoretically fitted distribution, counted autocorrelation and the number of statistically significant, subsequent coefficients (with shifts from I to 5).Annual minima are best approximated (Fig. 3) by Fisher's-Tippet's distribution (E3). Furthermore, in some cases log-normal, two- and three-parametric distributions (LN2 and LN3) were fitted. It is clearly seen in spatial distribution (Fig. 4) in Pilica river basin that the participation of Fisher's-Tippet's distribution is relatively smaller in this region than in the others. Mean autocorrelation of annual minima (Fig. 5) is equal to 0.59, which means that the levels have big inertia. Annual maxima are best approximated by (Fig. 6) log-normal, twoparametric distribution (LN2). Except this one, in some cases: Gumbell (El), three-parametric log-normal (LN3) and Pearson type III distribution (P3) are fitted. On the north of the investigated area in the spatial arrangement the concentration of LN3 distribution can be clearly seen. The sequences of maximum groundwater levels are characterized by much smaller inertia than sequences of minimum values. Looking at their spatial arrangements (Fig. 8) it cannot be omitted that high RaI values (> 0.8) concern the same region, but not the same wells as in case of minima. Low RaI values « 0.2) are rather evenly distributed. Basing on the approximated distributions, water levels of given probability (of 50% and 10%) of exceeding (for maximum values) and unreachables (for minimum values) were calculated. It allowed to create diagrams (Fig. 9) of the frequency of week-long floods and low flows during the long lasting period. After slightly dry 50s the shortages were supplemented and wet years began (late 60s to the beginning of 80s). Following years belong to a dry period with its apogee in 1990-1993. Afterwards we observe some years of supplementation of aquifers and the beginning of floody period just before the beginning of a new millennium. As in case of other hydrometeorological characteristics we can observe its cyclic nature.
Źródło:
Acta Universitatis Lodziensis. Folia Geographica Physica; 2008, 8
1427-9711
2353-6063
Pojawia się w:
Acta Universitatis Lodziensis. Folia Geographica Physica
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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