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2006 | 09 | 2 |

Tytuł artykułu

Estimation of lag times of rainfall events for three small river basins

Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
Lag time of runoff – Lag is one of the characteristic values in rainfall-runoff modeling and lag time of sediment yield – LagS is an important characteristic in the procedure of predicting the suspended sediment rate (sedimentgraph). The relationship between the lag times (LagS/Lag) is used for estimating sediment routing coefficient – B, which is a key parameter of the instantaneous unit sedimentgraph (IUSG). The IUSG formula is needed to transform the sediment produced during rainfall into sedimentgraph. The relationship LagS/Lag was examined for a three small basins (two of which are located in Poland, and one in Germany). The ratio LagS/Lag, estimated for events from the investigated basins, has been in the range from 0.49 to 1.11. A statistical significant correlation has been found between the value of LagS/Lag and rainfall depth in one of the basins.

Słowa kluczowe

Wydawca

-

Rocznik

Tom

09

Numer

2

Opis fizyczny

http://www.ejpau.media.pl/volume9/issue2/art-30.html

Twórcy

autor
  • Warsaw Agricultural University, Nowoursynowska 159, 02-776 Warsaw, Poland
autor
autor

Bibliografia

  • Banasik K.; 1994. Model Sedymentogramu Wezbrania Opadowego w Małej Zlewni Rolniczej. [Sedimentgraph Model of Rainfall Events in Small Agricultural Basin]. Publication of Warsaw Agricultural University – SGGW; 120 pp.; [in Polish with an English summary].
  • Banasik K., Barszcz M., Pudzianowska J., Czempińska-Switalska Z.; 2002. Wyznaczanie czasu opóŸnienia odpływu wezbraniowego w zlewni rzeki Gzówki. [Estimation of lag time of runoff for a small agricultural catchment]. Acta Scientiarum Polonorum. Architektura; (1-2)/2002: 53-62; [in Polish].
  • Banasik K., Walling D.E.; 1996. Predicting sedimentgraphs for a small agricultural catchment. Nordic hydrology; 27(4): 275-294.
  • Ignar S., Banasik K.; 1994. An influence of the method for effective rain determination on the parameters of Nash model. Annuals of Warsaw Agricultural University-SGGW. Land Reclamation; 27: 77-80.
  • Kennedy R.J., Watt W.E.; 1967. The relationship between lag time and the physical characteristics of drainage basins in Southern Ontario. IASH Publication; 85: 866-874.
  • Nash J.E.; 1957. The form of the instantaneous unit hydrograph. International Association of Scientific Hydrology; 59: 202-213.
  • Nash J.E.; 1960. A unit hydrograph study with particular reference to British catchments . Proc. Instr. Civ. Eng; 17(5).
  • Röttcher K.; 2001. Hochwasser für kleine Einzugsgebiete im Mittelgebirge am Beispiel der Bauna. [Flood defence of small catchments areas in low mountain regions by the example of the case study “Bauna”]. Kasseler Wasserbau-Mitteilungen; 11/2001. Herkules Verlag; 184 pp.; [in German].
  • Simas M.J., Hawkins R.H.; 1999. Lag time characteristics for small basins in the U.S. NRCS-USDA [National Resources Conservation Service-United States Department of Agriculture]. Manuscript.
  • Sobirey A., Tönsmann F.; 2001. Schwebstoffmessungen zur Prognose morphologischer Änderungen in einem Mittelgebirgsfliessgewässer. [Forecasting the morphological modifications of a low mountain range brook by suspended load measurements]. Kasseler Wasserbau-Forschungsberichte; 14/2001. Herkules Verlag; 40 pp.; [in German].
  • Tönsmann F.; 1995. Studie zum Hochwasserschutz an der Bauna. Kurzfassung. [A study of flood defence on the Bauna river. Short version]. Kasseler Wasserbau-Materialien; 3. Herkules Verlag Kassel; [in German].
  • USDA-SCS (Soil Conservation Service); 1985. National Engineering Handbook. Hydrology, Waszyngton, D.C.

Typ dokumentu

Bibliografia

Identyfikatory

Identyfikator YADDA

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