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Tytuł:
Flow Rate Determination as a Function of Rainfall for the Ungauged Suhareka River
Autorzy:
Kusari, Laura
Osmanaj, Lavdim
Shehu, Hana
Bungu, Samir
Powiązania:
https://bibliotekanauki.pl/articles/2086389.pdf
Data publikacji:
2022
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
catchment area
regression coefficient
CN parameter
rainfall intensity
flow curve
rainfall
flood
Opis:
For ungauged rivers, when there are no hydrological measurements and there is a lack of data on perennial flow rates, the latter one to be determined based on other hydrological data. The river Suhareka catchment represents a similar case. Since there is no data on Suhareka’s flow rates, the authors of this study aimed for the flow rate determination based on rainfall measurements. From the available data on annual precipitation (monthly sums) provided by the Kosovo Hydrometeorological Institute for the Suhareka hydrometric station, the observed monthly rainfall data for 30 years were analysed. Those gaps were initially filled by connecting the hydrometric station in Suhareka with those of Prishtina, Prizren and Ferizaj, and as a result a fairly good fit was ensured. Moreover, the intensity-duration-frequency curves were formed using the expression of Sokolovsky, as a mathematical model of the dependence I (T, P). For a transformation of rainfall into flow, the American method SCS was used. As a result, the equation for the Suhareka River basin was derived, which enabled the determination of maximum inflows, for different return periods. The results obtained through this paper, indicates that even for ungauged river basins the peak flows can be determined from available rainfall data.
Źródło:
Journal of Ecological Engineering; 2022, 23, 4; 110--121
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Characteristics of Measured Rainfall Rate at Ogbomoso, Nigeria for Microwave Applications
Autorzy:
Semire, F. A.
Raji, T. I.
Powiązania:
https://bibliotekanauki.pl/articles/309068.pdf
Data publikacji:
2011
Wydawca:
Instytut Łączności - Państwowy Instytut Badawczy
Tematy:
characteristics
Ogbomoso
rainfall
Opis:
Characteristics of rainfall rate useful in the estimation of attenuation due to rain are presented. Rain data collected at Ogbomoso between January-October, 2009 were used in the analysis. Result shows that power law relationship exists between the equiprobable rain rates of two different integration times. The value of conversion factor CE and CR obtained for Ogbomoso are 0.28(60) and 0.64(90) respectively. Our result then shows that different conversion factor is required for different location even within the same climatic region.
Źródło:
Journal of Telecommunications and Information Technology; 2011, 2; 85-89
1509-4553
1899-8852
Pojawia się w:
Journal of Telecommunications and Information Technology
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Organic compounds in rainfall at Hornsund, SW Spitsbergen: qualitative results
Autorzy:
Krawczyk, Wiesława Ewa
Skręt, Urszula
Powiązania:
https://bibliotekanauki.pl/articles/2052041.pdf
Data publikacji:
2005
Wydawca:
Polska Akademia Nauk. Czytelnia Czasopism PAN
Tematy:
Arctic
Svalbard
Hornsund
organic compounds
rainfall
chemistry
Źródło:
Polish Polar Research; 2005, 26, 1; 65-76
0138-0338
2081-8262
Pojawia się w:
Polish Polar Research
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Emporal and spatial variability of rainfall in modelling of stormwater outflows
Autorzy:
Nowogoński, Ireneusz
Powiązania:
https://bibliotekanauki.pl/articles/395997.pdf
Data publikacji:
2019
Wydawca:
Uniwersytet Zielonogórski. Oficyna Wydawnicza
Tematy:
rainfall
storm water
runoff
drainage
modeling
SWMM
opady
woda deszczowa
spływ
drenaż
modelowanie
Opis:
The article presents issues related to modeling of the rainfall-runoff phenomenon. As factors influencing the simulation results, the velocity and direction of precipitation relative to the drainage basin were indicated. The possibility of underestimating the crosssections of rainwater channels as a result of overlapping rain wave directions and the dominant flow direction in the rainwater channel network was pointed out. The research results to date indicate a reduction in the symptoms of this phenomenon as the complexity of the channel network increases. The final verification was based on the actual catchment. Calculations were made using the Epa SWMM 5.1.013 software. The results are presented in a graphic form to illustrate the variability of stormwater outflow.
Źródło:
Civil and Environmental Engineering Reports; 2019, 29, 4; 267-278
2080-5187
2450-8594
Pojawia się w:
Civil and Environmental Engineering Reports
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Comparison of water needs of true millet in the region of Bydgoszcz and Wroclaw
Autorzy:
Rolbiecki, S.
Chmura, K.
Powiązania:
https://bibliotekanauki.pl/articles/61162.pdf
Data publikacji:
2015
Wydawca:
Polska Akademia Nauk. Stowarzyszenie Infrastruktura i Ekologia Terenów Wiejskich PAN
Tematy:
rainfall
water need
millet
Bydgoszcz town
Wroclaw city
water deficit
rainfall deficiency
Źródło:
Infrastruktura i Ekologia Terenów Wiejskich; 2015, III/2
1732-5587
Pojawia się w:
Infrastruktura i Ekologia Terenów Wiejskich
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Simulated impacts of rainfall extremes on yield responses of various barley varieties in a temperate region
Autorzy:
Yoon, C.Y.
Kim, S.
An, K.N.
Powiązania:
https://bibliotekanauki.pl/articles/2083065.pdf
Data publikacji:
2021
Wydawca:
Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:
barley
rainfall
simulation
food cost
grain
yield
Opis:
As population rises, more people need to be fed. With increasing income, the potential exists for increases in the demand for cereals (i.e., barley). Since barley has a high level of tolerance to environmental stressors, this crop has been recommended as a potential crop for food security in marginal environments. In this study, a crop growth Agricultural Land Management Alternatives with Numerical Assessment Criteria model, was parameterized and used to simulate the yields of two barley types grown in a temperate environment at a latitude of 35°N. In order to apply this crop model to barley, 19 years of field data were used to model calibration and validation. As a result, the ALMANAC model accurately simulated yields for both barley types. The validated model was used to predict yields under three diverse seasonal rainfall scenarios associated with different patterns of the Central Pacific El Niño influence. According to the simulation results, excessively high seasonal rainfall decreased barley yields. Crop price and annual revenue of the two barley types were also evaluated using a non-linear regression model. For the malt type, the food price was higher with a higher rainfall, while naked barley had a higher revenue under the conditions of a lower rainfall.
Źródło:
International Agrophysics; 2021, 35, 2; 119-129
0236-8722
Pojawia się w:
International Agrophysics
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Evaluation of Rainfall-Runoff Erosivity Factor for Cameron Highlands, Pahang, Malaysia
Autorzy:
Abdulkadir, T. S.
Mustafa, M. R.
Yusof, K. W.
Hashim, A. M.
Powiązania:
https://bibliotekanauki.pl/articles/123050.pdf
Data publikacji:
2016
Wydawca:
Polskie Towarzystwo Inżynierii Ekologicznej
Tematy:
rainfall
erosivity factor
soil erosion
USLE/RUSLE
runoff
Opis:
Rainfall-runoff is the active agent of soil erosion which often resulted in land degradation and water quality deterioration. Its aggressiveness to induce erosion is usually termed as rainfall erosivity index or factor (R). R-factor is one of the factors to be parameterized in the evaluation of soil loss using the Universal Soil Loss Equation and its reversed versions (USLE/RUSLE). The computation of accurate R-factor for a particular watershed requires high temporal resolution rainfall (pluviograph) data with less than 30-minutes intensities for at least 20 yrs, which is available only in a few regions of the world. As a result, various simplified models have been proposed by researchers to evaluate R-factor using readily available daily, monthly or annual precipitation data. This study is thus aimed at estimating R-factor and to establish an approximate relationship between R-factor and rainfall for subsequent usage in the estimation of soil loss in Cameron highlands watershed. The results of the analysis showed that the least and peak (critical) R-factors occurred in the months of January and April with 660.82 and 2399.18 MJ mm ha-1 h-1year-1 respectively. Also, it was observed that erosivity power starts to increase from the month of January through April before started falling in the month of July. The monthly and annual peaks (critical periods) may be attributed to increased rainfall amount due to climate change which in turn resulted to increased aggressiveness of rains to cause erosion in the study area. The correlation coefficient of 0.985 showed that there was a strong relationship rainfall and R-factor.
Źródło:
Journal of Ecological Engineering; 2016, 17, 3; 1-8
2299-8993
Pojawia się w:
Journal of Ecological Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Rainfall estimates from radar vs. raingauge measurements. Warsaw case study
Autorzy:
Jakubiak, B.
Licznar, P.
Malinowski, S. P.
Powiązania:
https://bibliotekanauki.pl/articles/207576.pdf
Data publikacji:
2014
Wydawca:
Politechnika Wrocławska. Oficyna Wydawnicza Politechniki Wrocławskiej
Tematy:
raingauge measurements
Z-R relationship
urban hydrology
rainfall
odbiciowość radarowa
zależność R-H
hydrologia miejska
opady
Opis:
Contemporary models of urban hydrology and especially hydrodynamic models of stormwater systems demand on supply with high resolution spatial and temporal precipitation information. A plausible solution of precipitation information acquiring over urban catchments is seen in coupling of radar signals and raingauge networks measurements. Suitability of this approach is tested in the case of standard C-band weather radar and the dense network of fast-response raingauges. Rainfall rate estimated based on dependence on the reflectivity factor (Z-R relationship) in single pixels of the radar image are compared to rainfall rates measured by 25 raingauges located in Warsaw, Poland. In the analyzed period, 23 precipitation days with rain from convective clouds and cloud systems are detected. The main conclusion is that despite the fact that adopted Z-R relationship holds well in statistical sense (i.e. the whole period long empirical probability distribution functions (PDFs) of estimated and measured rainfall rates are in good agreement), instantaneous measurements and estimates as well as short-term (one day) PDFs differ remarkably. These differences are not systematic, they vary from the raingauge to raingauge and from day to day. Moreover, the most remarkable differences are associated with the highest rainrates which should be carefully considered prior radar data use as input for urban hydrology modelling.
Źródło:
Environment Protection Engineering; 2014, 40, 2; 159-170
0324-8828
Pojawia się w:
Environment Protection Engineering
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Mathematical modelling of rainfall runoff from small catchments of the northwest coast of the Black Sea
Autorzy:
Moniushko, M.
Daus, M.
Zakharova, M.
Powiązania:
https://bibliotekanauki.pl/articles/108582.pdf
Data publikacji:
2015
Wydawca:
Instytut Meteorologii i Gospodarki Wodnej - Państwowy Instytut Badawczy
Tematy:
spatial model
radar data
ground data
rainfall
discharge
runoff
hydrograph
Opis:
This article is devoted to the use of a mathematical model of a flood runoff for calculating rainfall runoff hydrographs from small catchments of the northwest coast of the Black Sea. The described model was tested and applied for the following catchments located in various geographical conditions, with various amounts of initial data: experimental catchments in Zacarpathian, the northwest of the Black Sea region – Ukraine and the Republic of Moldova, small catchments of the northern part of Vietnam, etc. This work was carried out on the basis of Moldavian Water-Balance Station databases. The development of a complex approach to a mathematical simulation of the formation of the processes of rain floods from small catchments is also given further investigation in this article. A brief description of the structure of a flood runoff spatial model from small catchments then provided. As well as this, the advantages of using radiolocation measurement of rainfall in the mathematical modeling of the formation of a flood runoff are shown. The results of construction runoff hydrographs confirm the possibility of applying this spatial model with the use of radar information. The optimization of model parameters was made with the data of 123 floods. The values of the quality criterion S/σ turned out not to exceed the value 0.8 in 81% of the considered cases of floods.
Źródło:
Meteorology Hydrology and Water Management. Research and Operational Applications; 2015, 3, 1; 45-50
2299-3835
2353-5652
Pojawia się w:
Meteorology Hydrology and Water Management. Research and Operational Applications
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Rainfall-river discharge modelling for flood forecasting using Artificial Neural Network (ANN)
Autorzy:
Obasi, Arinze A.
Ogbu, Kingsley N.
Orakwe, Chukwuemeka L.
Ahaneku, Isiguzo E.
Powiązania:
https://bibliotekanauki.pl/articles/292776.pdf
Data publikacji:
2020
Wydawca:
Instytut Technologiczno-Przyrodniczy
Tematy:
artificial neural network (ANN)
rainfall
flood forecasting
river discharge
Opis:
This study is aimed at evaluating the applicability of Artificial Neural Network (ANN) model technique for river discharge forecasting. Feed-forward multilayer perceptron neural network trained with back-propagation algorithm was employed for model development. Hydro-meteorological data for the Imo River watershed, that was collected from the Anambra-Imo River Basin Development Authority, Owerri – Imo State, South-East, Nigeria, was used to train, validate and test the model. Coefficients of determination results are 0.91, 0.91 and 0.93 for training, validation and testing periods respectively. River discharge forecasts were fitted against actual discharge data for one to five lead days. Model results gave R2 values of 0.95, 0.95, 0.92, 0.96 and 0.94 for first, second, third, fourth, and fifth lead days of forecasts, respectively. It was generally observed that the R2 values decreased with increase in lead days for the model. Generally, this technique proved to be effective in river discharge modelling for flood forecasting for shorter lead-day times, especially in areas with limited data sets.
Źródło:
Journal of Water and Land Development; 2020, 44; 98-105
1429-7426
2083-4535
Pojawia się w:
Journal of Water and Land Development
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Laboratory determination of potential interception of young deciduous trees during low-intense precipitation
Autorzy:
Klamerus-Iwan, A.
Sporysz, M.
Powiązania:
https://bibliotekanauki.pl/articles/38420.pdf
Data publikacji:
2014
Wydawca:
Instytut Badawczy Leśnictwa
Tematy:
deciduous tree
rainfall
intensity
simulated rainfall
potential interception
raindrop size
Fagus sylvatica
Quercus robur
laboratory determination
precipitation
Opis:
The research issue focuses on potential interception, which is the maximum amount of water that can be stored on plant surface. Tests under controlled conditions remain the best way to enhance knowledge on interception determinants in forest communities. Such tests can provide data for identification of mathematical models based on ecological criteria. The study presented in this paper concerned tree interception under simulated rain in a range from 2 to 11 mm/h. To perform the experiment a set of sprinklers was designed and built. The study included two deciduous species: beech (Fagus sylvatica L.) and oak (Quercus robur L.). Descriptive characteristic and nonlinear estimation were suggested for the obtained data. Interdependence of potential interception, the intensity of rain and the size of raindrops were described using exponential equation. The intensity and drop size of simulated rainfall significantly influence the obtained values of potential interception. Data analysis shows a decrease of interception value with an increase of intensity of simulated rainfall for both analysed species. Every run of the experiment that differed in the intensity and size of raindrops reached an individual level of potential interception and time needed to realize it. The formation of ability of plants to intercept water depends both on the dynamics and the time of spraying.
Źródło:
Folia Forestalia Polonica. Series A . Forestry; 2014, 56, 1
0071-6677
Pojawia się w:
Folia Forestalia Polonica. Series A . Forestry
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Ocena struktury czasowo-przestrzennej opadów z wkorzystaniem wybranych wskaźników do identyfikacji zdarzeń ekstremalnych
Evaluation of spatio-temporal rainfall patterns with selected indicators for extreme event identification
Autorzy:
Szalińska, W.
Otop, I.
Powiązania:
https://bibliotekanauki.pl/articles/338269.pdf
Data publikacji:
2012
Wydawca:
Instytut Technologiczno-Przyrodniczy
Tematy:
opad
wartości wskaźnikowe
zdarzenia ekstremalne
extreme events
indicators
rainfall
Opis:
Intensywne opady mogą powodować zagrożenie oraz poważne skutki hydrologiczne (powodzie, wezbrania), zarówno lokalnie, jak i w skali regionalnej. Stopień zagrożenia powodowanego opadami zależy od wielu czynników, m.in. od wysokości opadów, czasu trwania, zasięgu przestrzennego oraz sposobu zagospodarowania danego obszaru. Celem badań było opracowanie zbioru wartości wskaźnikowych dobowych sum opadów, umożliwiających ocenę struktury czasowo-przestrzennej opadów pod kątem identyfikacji zdarzeń ekstremalnych, wpływających na zagrożenie hydrologiczne. Opracowany zbiór wskaźników obejmował wskaźniki aprioryczne i statystyczne. Wartości progowe wskaźników statystycznych wyznaczono na podstawie wieloletnich danych obserwacyjnych, analizując sumy, czas trwania i rozkład przestrzenny opadów. Wybrany zbiór wskaźników wykorzystano do oceny struktury czasowo-przestrzennej opadów w dorzeczu górnej i środkowej Odry w okresie czerwiec-lipiec 2009 oraz maj-czerwiec 2010 r. Wyznaczone wskaźniki mogą być wykorzystane w bieżącej ocenie warunków opadowych, a wraz z uwzględnieniem morfologii terenu i zagospodarowania danego obszaru - do oceny stopnia zagrożenia hydrometeorologicznego.
Intensive rainfall events can cause severe hydrological threats and flooding. The scale of hydrological impact depends on the amount of precipitation, duration and spatial range. The aim of this work was to develop a set of indicators for the evaluation of daily sums of rainfall in order to identify extreme events triggering hydrological hazards. Indicator threshold values were assumed a priori or estimated from long-term observation dataset. A selected set of indicators was used to evaluate spatial and temporal structure of two precipitation events: June-July 2009 and May-June 2010. The obtained results showed the magnitude of extreme rainfall, frequency and duration as well as location of extreme events forming hydrological hazard in 2009 and 2010 in the upper and middle Odra River basin. Developed set of indicators can be used operationally to evaluate current rainfall situation and, in combination with the information on hydrological and catchment conditions, to assess hydrological risk.
Źródło:
Woda-Środowisko-Obszary Wiejskie; 2012, 12, 2; 269-282
1642-8145
Pojawia się w:
Woda-Środowisko-Obszary Wiejskie
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Impact of rainfall variability on maize yield in the KwaZulu-Natal, North-West and Free State provinces of South Africa (1987–2017)
Autorzy:
Mapfumo, Phrasia
Chagwiza, Clarietta
Antwi, Michael
Powiązania:
https://bibliotekanauki.pl/articles/1891733.pdf
Data publikacji:
2020-12-28
Wydawca:
Uniwersytet Przyrodniczy w Poznaniu. Wydawnictwo Uczelniane
Tematy:
climate change
rainfall
mean maize yield
correlation
ANOVA
South Africa
Opis:
Climate change has increased temperature, caused drought in places like North West Province, and reduced crop yield. This study investigated the climate change impact (rainfall) on maize yield (1987 -2017). The objectives were to determine the climate change impact on maize yield for Kwazulu-Natal, North West, and Free State Provinces of South Africa, assess the difference in climate change impact on maize yield between the three provinces. Rainfall and maize data were collected from WeatherSA and DAFF, respectively. A Pearson Correlation Analysis revealed a weak negative correlation between rainfall and maize for KwaZulu-Natal and Free State Provinces. However, for North West Province there was a weak positive correlation between maize yield and rainfall. Rainfall determines yield, if excessive, it becomes detrimental to crop yield. Climate change affected negatively on maize yield, rainfall above maize requirement was not beneficial to crop yield and drought reduced yield too. ANOVA results revealed that the group mean yield between the Provinces was different, with KwaZulu-Natal having the highest mean yield. The climate change impact on maize varied between provinces, KwaZulu-Natal Province was least affected, however, North West Province was the most negatively impacted with drought events leading to reduced maize yield.
Źródło:
Journal of Agribusiness and Rural Development; 2020, 58, 4; 359-367
1899-5241
Pojawia się w:
Journal of Agribusiness and Rural Development
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Czasowo-przestrzenne zróżnicowanie opadów atmosferycznych we Wrocławiu
Space-time distribution of precipitation in the city of Wroclaw
Autorzy:
Kotowski, A.
Dancewicz, A.
Kaźmierczak, B.
Powiązania:
https://bibliotekanauki.pl/articles/237309.pdf
Data publikacji:
2010
Wydawca:
Polskie Zrzeszenie Inżynierów i Techników Sanitarnych
Tematy:
opad deszczu
wysokość opadu
intensywność opadu
sieć pomiarowa
rainfall
precipitation amount
rainfall intensity
network of gauging stations
Opis:
Przeprowadzone badania czasowo-przestrzennego zróżnicowania opadów we Wrocławiu na podstawie wieloletnich pomiarów wykazały, że obecna sieć pomiarowo-obserwacyjna nie sprosta zapotrzebowaniu na informacje, niezbędne do projektowania bądź modernizacji, w tym modelowania hydrodynamicznego, systemów odwodnieniowych. Dotyczy to zwłaszcza intensywnych opadów krótkotrwałych stwarzających duże zagrożenie funkcjonowania kanalizacji deszczowej i ogólnospławnej. W pracy wykazano znaczne różnice ilościowe wysokości i intensywności opadów w różnych rejonach Wrocławia. W szczególności w rejonie stacji meteorologicznej Wrocław-Strachowice (na zachodzie miasta) występują wyższe wartości natężeń opadów o ok. 20% w stosunku do rejonu stacji Wrocław-Swojec (na wschodzie). Wnioskowanie oparte na materiałach pochodzących z dwóch stacji może zatem powodować niedoszacowanie natężeń opadów w rejonach północnym i południowym miasta, na co wskazują wyższe wartości opadów dobowych na Psim Polu czy Oporowie. Należy zatem zwiększyć liczbę stacji automatycznie rejestrujących wysokość opadów w czasie, co w efekcie przyczyni się do lepszej ochrony całej aglomeracji wrocławskiej przed lokalnymi wylewami z kanalizacji czy podtopieniami.
Analysis of the space-time distribution of precipitation for the city of Wroclaw obtained from many years' measurements has demonstrated that the existing net-work of gauging stations fails to provide reliable data for the design or modernization, and primarily for the hydrodynamic modeling of draining systems. This finding holds true particularly for high-intensity rainfalls of a short duration, as they pose a real threat to the functioning of the storm water drain and combined sewage systems. The results of the study have revealed considerable differences in the amount and intensity of precipitation between particular parts of the city. Within the area of the Wroclaw-Strachowice station (in the western part of the city) the amount of precipitation received was by approx. 20% higher as compared to that within the Wroclaw-Swojec station (in the eastern part of the city). Drawing conclusions based on the data obtained from the two meteorological stations may lead to the underestimation of the precipitation amounts received in the northern and southern parts of the city, as can be inferred from the higher values of daily precipitation amounts measured in Wroclaw-Psie Pole and Wroclaw-Oporów. It is therefore recommendable to increase the number of stations that will provide automatic records of the precipitation amounts received with time. This will guarantee a more efficient protection of the municipality of Wroclaw against local flooding or outflow from the sewerage system.
Źródło:
Ochrona Środowiska; 2010, 32, 4; 37-46
1230-6169
Pojawia się w:
Ochrona Środowiska
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Analysis of trend rainfall: Case of North-Eastern Algeria
Analiza tendencji opadów – przykład północno-wschodniej Algierii
Autorzy:
Mrad, D.
Djebbar, Y.
Hammar, Y.
Powiązania:
https://bibliotekanauki.pl/articles/293235.pdf
Data publikacji:
2018
Wydawca:
Instytut Technologiczno-Przyrodniczy
Tematy:
climate change
Mann–Kendall test
North-Eastern Algeria
rainfall
trend
opad
północno-wschodnia Algieria
test Manna–Kendalla
zmiana klimatu
Opis:
The climatic change is a reality largely recognized today in the scientific community. Nevertheless, its impact on precipitation, especially on annual, monthly and seasonally rainfall in arid and semi-arid regions is not yet certain. Indeed, very few studies have dealt with this matter in Algeria. In this context to examine spatial distribution of annual and seasonal rainfall an attempt has been made using the inverse distance weighting (IDW) method. Trends and magnitude estimate of change in rainfall series were detected by Mann–Kendall tests and Sen's test slope, has been applied to the data registered of 35 stations in the watershed Constantinois Seybouse Mellegue (CSM) North-Eastern Algeria over a period of 43 years (1969–2012). Results from spatial plot of annual rainfall showed that the rainfall increases with altitude, but is higher for the stations exposed to moist winds. It also increases from east to west and conversely decreases as one moves away from the coast to the south. From statistical method showed that there are increase trends at 95% confidence at annual scale in some rainfall stations with high altitude and coastal stations during winter season.
Zmiana klimatu jest faktem powszechnie uznawanym obecnie przez społeczność naukową. Mimo to jej wpływ na opady, szczególnie na roczny, miesięczny i sezonowy opad na obszarach klimatu suchego i półsuchego, nie jest jeszcze dobrze rozpoznany. Do tej pory tylko kilka badań w Algierii dotyczyło tej kwestii. W związku z tym podjęto próbę zbadania przestrzennego rozmieszczenia rocznych i sezonowych opadów za pomocą metody odwrotnej odległości (IDW – ang. inverse distance weighting). Trendy i wielkość oszacowanych zmian w seriach opadów analizowano testem Manna–Kendalla, a test nachylenia Sena użyto do danych zgromadzonych w 35 posterunkach opadowych w zlewni Constantinois Seybouse Mellegue (CSM) w północno- -wschodniej Algierii w ciągu 43 lat (1969–2012). Wyniki analiz przestrzennego rozkładu rocznych opadów wykazały, że opad rośnie wraz z wysokością nad poziomem morza i jest większy w stanowiskach eksponowanych na wilgotne wiatry. Opad rośnie ze wschodu na zachód, a maleje od wybrzeża w kierunku południowym. Metody statystyczne ujawniły rosnący (przedział ufności 95%) trend opadów w niektórych posterunkach na dużych wysokościach i w posterunkach przybrzeżnych w okresie zimy.
Źródło:
Journal of Water and Land Development; 2018, 36; 105-115
1429-7426
2083-4535
Pojawia się w:
Journal of Water and Land Development
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-15 z 61

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