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Warianty tytułu
Susza i gromadzenie wód powierzchniowych w obszarach półsuchych. Przykład zapory wodnej Hammam Boughrara (w północno-zachodniej Algierii)
Języki publikacji
Abstrakty
The dam of Hammam Boughrara is an embankment dam built in a transboundary basin, between Algeria and Morocco; it was type-approved and delivered in 1998. This dam was supposed to solve the lack of drinking water in Oran (Algeria's second largest city) and enhance the agricultural perimeter of the area. It should regulate an annual water volume of 59 million m3. However, the northwest Algeria has experienced a fairly severe drought since the 80s. This article aims to show the impact of this drought on the amount of surface water that can be mobilized by this dam. The rainfall series recorded at four stations, located within the basin of the dam, were examined using the proportional deviation from the average, the running average, the frequency analysis, the Pita’s index and the standardized precipitation index. These methods have shown a significant decrease of rain, starting from the hydrological year 1975/1976. These same approaches were also used to analyse series of flows spread over a longer period. This fact revealed three periods of drought which are 1940–1945, 1955–1967 and the most recent one highlighted by the rainfall series, starts at the year 1975/1976. The regularized water volume of the dam, calculated from the series of flow rates, is around 37 million m3. This value reflects a deficit of 40% of the regularized volume predicted by the designers of the dam.
Zaporę Hammam Boughrara zbudowano na granicy Algierii i Maroka i uruchomiono w 1998 r. Zapora miała na celu rozwiązać problem braku wody pitnej w Oranie (drugim co do wielkości mieście Algierii) i zwiększyć zasięg rolnictwa w regionie. Miała regulować rocznie zasoby wody o objętości 59 milionów m3. Północnozachodnie regiony Algierii doświadczają jednak silnej suszy od lat osiemdziesiątych XX wieku. Artykuł ma wykazać wpływ tej suszy na ilość wody, którą może gromadzić zbiornik. Serie opadowe notowane w czterech stacjach zlokalizowanych w zlewni zbiornika analizowano z wykorzystaniem proporcjonalnego odchylenia od średniej, ruchomej średniej, analizy częstości, wskaźnika Pity i wskaźnika standaryzowanego opadu. Stosowane metody wykazały istotne zmniejszenie ilości opadu począwszy od roku hydrologicznego 1975/1976. Takie samo podejście zastosowano do analizy serii szybkości przepływu, które obejmują dłuższy okres. Analiza ujawniła trzy okresy suszy, które przypadały na lata 1940–1945, 1955–1967 i ostatni wykazany przez serie opadów, który rozpoczął się w roku 1975/1976. Zasoby wody regulowane rocznie obliczone z serii przepływów wynoszą ok. 37 milionów m3. Ta ilość w istocie odzwierciedla deficyt gromadzonej wody, gdyż jest o 40% mniejsza niż objętość przewidywana przez projektantów zapory.
Wydawca
Czasopismo
Rocznik
Tom
Strony
3--10
Opis fizyczny
Bibliogr. 26 poz., rys., tab.
Twórcy
autor
- University Abou Bekr Belkaid, Faculty of Technology, BP 230, 13000 Tlemcen, Algeria
autor
- University Abou Bekr Belkaid, Faculty of Technology, BP 230, 13000 Tlemcen, Algeria
Bibliografia
- ASSANI A.A. 1999. Analyse de la variabilité temporelle des précipitations (1916–1996) à Lumbashi (Congo-Kinshasa) en relation avec certains indicateurs de la circulation atmosphérique (Oscillation australe) et océanique (El Nino/Lanina) [Analysis of the temporal variability of precipitation (1916–1996) in Lumbashi (Congo-Kinshasa) in relation to certain indicators of atmospheric circulation (Southern Oscillation) and oceanic]. Sécheresse.Vol. 10. No. 4 p. 245–252.
- BARBULESCU A., DEGUENON J. 2014. Change points detection and models for precipitation evolution. Case study, Rom. Journal of Physics. Vol. 59. No. 5–6 p. 590–600.
- BĄK B., ŁABĘDZKI L. 2014. Prediction of precipitation deficit and excess in Bydgoszcz Region in view of predicted climate change. Journal of Water and Land Development. No. 23 p. 11–19. DOI 10.1515/jwld-2014-0025.
- BERGAOUI M. 2001. Caractérisation de la sécheresse météorologique et hydrologique: cas du bassin versant de Siliana en Tunisie [Characterization of meteorological and hydrological drought: case of the Siliana watershed in Tunisia]. Sciences et changement planétaires/Sécheresse. Vol. 12. No. 4 p. 205–213.
- COBA 2001. Barrage de Hammam Boughrara, etude d’impact sur l’environnement [Dam of Hammam Boughrara, environmental impact assessment]. Consultores de Engenharia e Ambiente. Vol. 1. Caractérisation du projet et de l’environnement [Characterization of the project and the environment] p. 3–58.
- DJELLOULI F., BOUANANI A., BABA-HAMED K. 2016. Efficiency of some meteorological drought indices in different time scales, case study: Wadi Louza basin (NW-Algeria). Journal of Water and Land Development. No 31 p. 33–41. DOI 10.1515/jwld-2016-0034.
- GHENIM A.N., MEGNOUNIF A. 2013. Ampleur de la sécheresse dans le bassin d’alimentation du barrage Meffrouche (Nord-Ouest de l’Algérie) [Extent of drought in the catchment area of the Meffrouche dam (North-West of Algeria)]. Géographie Physique et Environnement. Vol. 7 p. 35–49.
- HUBERT P., CARBONAL J.P., CHAOUCHE A. 1989. Segmentation des séries hydrométriques – application à des séries de précipitations et de débits de l’Afrique de l’Ouest [Segmentation of hydrometric series – application to series of precipitation and flows of West Africa]. Journal of Hydrologie. Vol. 110 p. 349–367.
- IMANOV F.A., MAMMADOV A.S., HASANOVA N.I. 2012. Investigation of droughts in the Lankaran region of Azerbaijan. Journal of Water and Land Development. No. 16 p. 11–15.
- JEMAI S., ELLOUZE M., AGOUBI B., ABIDA H. 2016. Drought intensity and spatial variability in Gabes Watershed, southeastern Tunisia. Journal of Water and Land Development. No. 31 p. 63–72. DOI 10.1515/jwld-2016-0037.
- JOUILLIL I., BITAR K., SALAMA H., AMRAOUI A., MOKSSIT A., TAHIRI M. 2013. Secheresse meteorologique au basin hydraulique oum er rbia Durant les dernières decennies [Meteorological dryness at the hydraulic basin oum er rbia During the last decades]. Larhyss Journal. No. 12 p. 109–127.
- KANG H.M., YUSOF F. 2012. Homogeneity tests on a daily rainfall series in Peninsular Malaysia. International Journal of Contemporary Mathematical Sciences. Vol. 7. No. 1 p. 9–22.
- KEHAL S. 2001. Retrospectives et perspectives du dessalement en Algérie [Retrospectives and prospects of desalination in Algeria]. Desalination. Vol. 136 p. 35–42.
- KETTAB A. 2000. Les resources en eau en Algérie: strategies, enjeux et vision [Water resources in Algeria: Strategies, challenges and vision]. Desalination. Vol. 136 p. 25–33.
- KHEZAZNA A., AMARCHI H., DERDOUS O., BOUSAKHRIA F. 2017. Drought monitoring in the Seybouse basin (Algeria) over the last decades. Journal of Water and Land Development. No. 33 p. 79–88. DOI 10.1515/jwld-2017-0022.
- LUBES-NIEL H., MASSON J.M., PATUREL J.E., SERVAT E. 1998. Variabilité climatique et statistiques. Etude par simulation de la puissance et de la robustesse de quelques tests utilisés pour vérifier l’homogénéité de chroniques [Climatic variability and statistics. A simulation approach for estimating power and robustness of tests of stationarity]. Revue des Sciences de l’Eau. Vol. 3 p. 383–408.
- MEDDI H., MEDDI M. 2009. Variabilité des precipitations annuelles du Nord-Ouest de l’Algérie [Variability of annual precipitation in northwestern Algeria]. Secheresse. Vol. 20. No.1 p. 57–65.
- MEDDI M., TALIA A., MARTIN C. 2009. Evolution recente des conditions climatiques et des écoulements sur le bassin versant de la Macta (Nord-Ouest de l’Algérie) [Recent changes in climatic conditions and flows in the Macta watershed (north-western Algeria)]. Géographie Physique et Environnement. Vol. 3 p. 61–84. DOI 104000/physiogéo.686.
- MEDEJERB A., HENIA L. 2011. Variations spatio-temporelle de la secheresse climatique en Algérie Nord-Occidentale [Climatic spatio-temporal variation in North-Western Algeria]. Courrier du savoir. No. 11 p. 71–79.
- MCKEE T., DOESKEN N., KLEIST J. 1993. The relationship of drought frequency and duration to time scales. In: Proceeding of the eighth conference on applied climatology, Anaheim, California, 17–22 January 1993. Boston. American Metrological Society p. 197–184.
- MRAD D., DAIRI S., DJEBBAR Y. 2013. Impact of climatic variability on the water resources in the catchment Seybouse [online]. Seventeenth International Water Technology Conference. 5–7 November 2013. Istanbul pp. 6. [Access 1.07.2017]. Available at: http://iwtc.info/wpcontent/uploads/2013/11/213.pdf
- NOUACEUR Z., LAIGNEL B., TURKI I. 2013 Changements climatiques au Maghreb: Vers des conditions plus humides et plus chaudes sur le littoral algérien [Climate change in the Maghreb: Towards wetter and warmer conditions on the Algerian coast]. Géographie Physique et Environnement. Vol. 7 p. 307–323. DOI 10.4000/physio-geo. 3686.
- PARDE M 1946. La sécheresse 1941–1945 [The drought of 1941–1945]. Annales de l’Université de Grenoble (France). Vol. 22. No. 3 p. 99–103.
- PITA M.F 2000. Un nouvel indice de sécheresse pour les domaines méditerranéens. Application au bassin de Guadalquivir (Sud-Ouest de l’Espagne) [A new drought index for Mediterranean areas. Application to the Guadalquivir Basin (South-West of Spain)]. Publications de l’Association Internationale de Climatologie. Vol. 113 p. 225–234.
- WMO 2012. Standardized precipitation index user guide (M. Svoboda, M. Hayes and D. Wood). WMO-No. 1090. Geneva. World Meteorological Organization. ISBN 978-92-63-11090-9 pp. 16.
- WMO 2016. 2016. Handbook of drought indicators and indices (M. Svoboda and B.A. Fuchs). Integrated Drought Management Programme (IDMP), Integrated Drought Management Tools and Guidelines. Series 2. Geneva. World Meteorological Organization (WMO) and Global Water Partnership (GWP). ISBN 978-92-63-11173-9, 978-91-87823-24-4 pp. 45.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-cd0974e6-95a4-440a-afe8-00fd0546c6e0