Latitude: 42.608963 | Longitude: 19.927246 | Country: Montenegro | Year: 2018 |
| F | 2.93072 | km2 | Surface area of the drainage basin |
| Fm | 1.26131 | km2 | Surface area of smaller portion of the drainage basin |
| Fv | 1.66941 | km2 | Surface area of greater portion of the drainage basin |
| O | 8.8377 | km | The length of the watershed |
| Lv | 2.6891 | km | Natural length of the main watercourse |
| Lb | 3.73001 | km | Surface area of greater portion of the drainage basin |
| Liz | ["0.259726 ","0.7709245 ","0.7897265 ","0.7963905 ","0.8544795 ","0.953394 ","1.075335 ","1.129429 ","1.2246205 ","1.302132 ","1.5839155 ","1.560719 ","1.4873385 ","1.46047 ","1.3958955 ","1.351942 ","1.3419545 ","1.2875715 ","1.209958 | km | Contour line length |
| f | ["0.019194 ","0.0530775 ","0.0605325 ","0.046683 ","0.056154 ","0.071862 ","0.107583 ","0.074088 ","0.0976395 ","0.0867615 ","0.1995735 ","0.11592 ","0.1190385 ","0.213948 ","0.14385 ","0.134085 ","0.194523 ","0.1463595 ","0.1594845 "," | km2 | The area between the two neighboring contour lines |
| h0 | 900 | m | Altitude of the first contour line |
| Δh | 50 | m | Equidistance |
| Hmin | 890 | m | Lowest altitude in the drainage basin |
| Hmax | 2211 | m | Highest altitude in the draigane basin |
| ΣL | 7.9001 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
| Lm | 2.30494 | km | The shortest distance between the fountain - head and mouth |
| fp | 0.045477513895907 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
| fpp | 0.42678120262759 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
| fo | 0.527741283476503 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
| fs | 0.5026 | m | Part of the surface area of the drainage basin under the forest |
| ft | 0.422 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
| fg | 0.0754 | m | Part of the surface area of the drainage basin which is bare or under the soils without grass vegetation |
| Hb | 89.4 | mm | The volume of the torrent rain |
| Up | 100 | years | Incidence |
| to | 8.1 | °C | Average annual air temperature |
| Hgod | 1182.3 | mm | Average annual quantity of precipitation |
| 0.68 % | Sand, gravel and incoherent soils |
| 0.68 % | Saline soils... |
| 1.38 % | Decomposed limestone and marls |
| 1.38 % | Serpentines, red sand stones, flishe deposits |
| 6.88 % | Podzols and parapodzols, decomposed schist |
| 3.44 % | Solid and Schist limestone, Terra Rosa and Humic soil |
| 6.88 % | Brown forest soils and Mountain soils |
| 0 % | Epieugleysol and Marshlands |
| 4.35 % | Good structured Chernozems and alluvial well-structured deposits |
| 74.33 % | Bare, compact igneous |
| 7.04 % | Bare lands |
| 0.5 % | Plough-lands |
| 2.01 % | Orchards and vineyards |
| 20.1 % | Mountain pastures |
| 20.1 % | Meadows |
| 15.08 % | Degraded forests |
| 35.18 % | Well-constituted forests |
| 8.16 % | Depth erosion |
| 0 % | 80% of the river basin under rill and gully erosion |
| 0 % | 50% of the river basin under rill and gully erosion |
| 29.63 % | 100% of the river basin under surface erosion |
| 0 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
| 7.55 % | 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 |
| 3.82 % | The river basin mostly under plough-land |
| 50.84 % | The river basin under forests and perennial vegetation |
| A | 0.64086553121862 | / | Coefficient of the river basin form |
| m | 0.44311337256912 | / | Coefficient of the watershed development |
| B | 0.78571371122329 | km | Average river basin width |
| a | 0.27849811650379 | / | (A)symmetry of the river basin |
| G | 2.6956174591909 | / | Density of the river network of the basin |
| K | 1.1666681128359 | / | Coefficient of the river basin tortuousness |
| Hsr | 1583.2574787083 | m | Average river basin altitude |
| Dsr | 693.2574787083 | m | Average elevation difference of the river basin |
| Isr | 47.388430999891 | % | Average river basin decline |
| Hleb | 1321 | m | The height of the local erosion base of the river basin |
| Er | 321.37298223072 | / | Coefficient of the erosion energy of the river basin's relief |
| W | 1.1211873686047 | m | Analytical presentation of the water retention in inflow |
| S1 | 0.84467913087418 | / | Coefficient of the region's permeability |
| S2 | 0.71456 | / | Coefficient of the vegetation cover |
| 2gDF1/2 | 199.6567269289 | m km s-1 | Energetic potential of water flow during torrent rains |
| Qmax | 86.588361799373 | m3 s-1 | Maximal outflow from the river basin |
| T | 0.95393920141695 | / | Temperature coefficient of the region |
| Z | 0.17856779049295 | / | Coefficient of the river basin erosion |
| Wgod | 783.56905057397 | m3 god-1 | Production of erosion material in the river basin |
| Ru | 0.39013605212536 | / | Coefficient of the deposit retention |
| Ggod | 305.69853595854 | m3 god-1 | Real soil losses |
| Ggod km-2 | 104.30833923355 | m3 km-2 god-1 | Real soil losses per km2 |