Abstract
The present work considers the Struma River water flow on Bulgarian territory as a starting point for evalua-tion of maximum and minimum water flow using an original integral method. The risk assessment is deter-mined by specific indices like the index Mmax,i for the deviation of the maximum water flow from the calcu-lated norm of the maximum flow Qmax,0 and the index Mmin,i for the deviation of the minimum water flow from calculated norm of the minimum flow Qmin,0. The new integral approach introducing specific indicators for risk assessment like the indices Mmin,i and Mmax,i has been checked at three sampling locations of the Na-tional monitoring net along the Struma River: Pernik (in the beginning), Krupnik (in the middle) and Marino pole (at the border in Greece) for the period 1948-2006. A significant trend towards decreasing of Mmax,i in-dex is outlined for the three points. On contrary, a significant trend towards increasing of Mmin,i index is found at Krupnik and Marno pole sampling points.
Highlights
The transboundary Struma River flows in the western part of Bulgaria and has a catchment area of 107.97 km2 and length of 290 km
The risk assessment is determined by specific indices like the index Mmax,i for the deviation of the maximum water flow from the calculated norm of the maximum flow Qmax,0 and the index Mmin,i for the deviation of the minimum water flow from calculated norm of the minimum flow Qmin,0
After Krupnik, the Struma River flow formation depends on the Mediterranean climate impact (Krupnik point – Marino pole point)
Summary
The transboundary Struma River flows in the western part of Bulgaria and has a catchment area of 107.97 km and length of 290 km. The catchment follows a mountain pattern and is characterized by a relatively low forestation level. The river water sources are in the high mountain part of the Vitosha and Rila Mountains. The Struma River flows through Bulgaria and Greece to the Aegean. The Struma River catchment area is a part of a region that experiences the influence of European continental climate. The southernmost part of the river valley serves as a corridor for the Mediterranean climate impact. After Krupnik, the Struma River flow formation depends on the Mediterranean climate impact (Krupnik point – Marino pole point)
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