Pano, Niko, authorAvdyli, Bardhyl, authorColorado State University, publisher2020-02-062020-02-062009https://hdl.handle.net/10217/200713http://dx.doi.org/10.25675/10217/2007132009 annual AGU hydrology days was held at Colorado State University on March 25 - March 27, 2009.Includes bibliographical references.Buna is one of the biggest and most important rivers of the Mediterranean basin. Outflowing from Scutary Lake this river joins Drini River so forming a complicated and particular hydrographical system. In these conditions it is impossible to calculate Buna River discharge when it flows out of Scutary Lake by the dependence Q2 = ƒ(H2) because Buna discharge – Q2, in its outflowing from the lake depends not only on the water levels – H2, but also on the water levels – H2 and Drini discharge – Q4. Many particular hydrometeorological studies are made of Scutary hydrographical complex (Pano N., Saraçi R.1963; PanoN., Abdyli B,1984, 2002). A particular way to calculate Buna discharge in its outflowing from Scutary Lake is presented in this paper. This particular way considers specific hydraulic conditions of this river. Multi-annual cycle discharge is calculated by this way.born digitalproceedings (reports)engCopyright and other restrictions may apply. User is responsible for compliance with all applicable laws. For information about copyright law, please see https://libguides.colostate.edu/copyright.Text