Latitude: 42.888683 | Longitude: 19.611135 | Country: Montenegro | Year: 2021 |
| F | 28.28 | km2 | Surface area of the drainage basin |
| Fm | 11.93 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 16.35 | km2 | Surface area of greater portion of the drainage basin |
| O | 15.99 | km | The length of the watershed |
| Lv | 8.23 | km | Natural length of the main watercourse |
| Lb | 11.02 | km | Surface area of greater portion of the drainage basin |
| Liz | ["0.93 ","4.53 ","7.17 ","9.46 ","12.49 ","14.66 ","19.32 ","22.17 ","15.30 ","6.58 ","0.50 "] | km | Contour line length |
| f | ["0.1 ","0.209 ","0.648 ","1.276 ","1.595 ","2.392 ","2.741 ","4.037 ","5.423 ","5.074 ","3.688 ","1.097 "] | km2 | The area between the two neighboring contour lines |
| h0 | 1100 | m | Altitude of the first contour line |
| Δh | 100 | m | Equidistance |
| Hmin | 1094 | m | Lowest altitude in the drainage basin |
| Hmax | 2139 | m | Highest altitude in the draigane basin |
| ΣL | 27.17 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 7.55 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.15 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.01 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.84 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.53780 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.46220 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.00000 | m | Part of the surface area of the drainage basin which is bare or under the soils without grass vegetation |
| Hb | 252 | mm | The volume of the torrent rain |
| Up | 100 | years | Incidence |
| to | 5.05 | °C | Average annual air temperature |
| Hgod | 1962 | mm | Average annual quantity of precipitation |
| 0 % | Sand, gravel and incoherent soils |
| 0 % | Saline soils... |
| 0 % | Decomposed limestone and marls |
| 0 % | Serpentines, red sand stones, flishe deposits |
| 0 % | Podzols and parapodzols, decomposed schist |
| 0 % | Solid and Schist limestone, Terra Rosa and Humic soil |
| 100 % | Brown forest soils and Mountain soils |
| 0 % | Epieugleysol and Marshlands |
| 0 % | Good structured Chernozems and alluvial well-structured deposits |
| 0 % | Bare, compact igneous |
| 0 % | Bare lands |
| 0 % | Plough-lands |
| 0 % | Orchards and vineyards |
| 46.22 % | Mountain pastures |
| 0 % | Meadows |
| 0 % | Degraded forests |
| 53.78 % | Well-constituted forests |
| 1.11 % | Depth erosion |
| 1.11 % | 80% of the river basin under rill and gully erosion |
| 1.11 % | 50% of the river basin under rill and gully erosion |
| 21.44 % | 100% of the river basin under surface erosion |
| 21.44 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 0 % | 50% of the river basin under surface erosion |
| 0 % | 20% of the river basin under surface erosion |
| 0 % | There are smaller slides in the watercourse beds |
| 0 % | The river basin mostly under plough-land |
| 53.78 % | The river basin under forests and perennial vegetation |
| A | 0.37886391251519 | / | Coefficient of the river basin form |
| m | 0.43657131874805 | / | Coefficient of the watershed development |
| B | 2.5662431941924 | km | Average river basin width |
| a | 0.31258840169731 | / | (A)symmetry of the river basin |
| G | 0.96074964639321 | / | Density of the river network of the basin |
| K | 1.0900662251656 | / | Coefficient of the river basin tortuousness |
| Hsr | 1778.7390912306 | m | Average river basin altitude |
| Dsr | 684.7390912306 | m | Average elevation difference of the river basin |
| Isr | 39.996463932107 | % | Average river basin decline |
| Hleb | 1045 | m | The height of the local erosion base of the river basin |
| Er | 144.24360451571 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 2.1660308970888 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.907 | / | Coefficient of the region's permeability |
| S2 | 0.69244 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 616.38457948754 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 317.67942433713 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.7778174593052 | / | Temperature coefficient of the region |
| Z | 0.24212623335983 | / | Coefficient of the river basin erosion |
| Wgod | 16153.578151372 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.36301963847334 | / | Coefficient of the deposit retention |
| Ggod | 5864.066100562 | m3 god-1 | Real soil losses |
| Ggod km-2 | 207.35735857716 | m3 km-2 god-1 | Real soil losses per km2 |