Latitude: 42.683737 | Longitude: 19.84094 | Country: Montenegro | Year: 2018 |
F | 4.24056 | km2 | Surface area of the drainage basin |
Fm | 2.04056 | km2 | Surface area of smaller portion of the drainage basin |
Fv | 2.2 | km2 | Surface area of greater portion of the drainage basin |
O | 8.27097 | km | The length of the watershed |
Lv | 1.13015 | km | Natural length of the main watercourse |
Lb | 1.2 | km | Surface area of greater portion of the drainage basin |
Liz | ["1.53027 ","2.09790 ","2.29707 ","2.26314 ","2.30188 ","1.96121 ","1.67482 ","1.45506 "] | km | Contour line length |
f | ["0.33899 ","0.69756 ","0.51660 ","0.49337 ","0.56858 ","0.54668 ","0.49229 ","0.34768 ","0.23881 "] | km2 | The area between the two neighboring contour lines |
h0 | 800 | m | Altitude of the first contour line |
Δh | 100 | m | Equidistance |
Hmin | 779 | m | Lowest altitude in the drainage basin |
Hmax | 1584 | m | Highest altitude in the draigane basin |
ΣL | 1.13015 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
Lm | 1.09757 | km | The shortest distance between the fountain - head and mouth |
fp | 0.2071 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
fpp | 0.2443 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
fo | 0.5486 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
fs | 0.531408047 | m | Part of the surface area of the drainage basin under the forest |
ft | 0.453821473 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
fg | 0.014770480 | m | Part of the surface area of the drainage basin which is bare or under the soils without grass vegetation |
Hb | 115 | mm | The volume of the torrent rain |
Up | 100 | years | Incidence |
to | 9.0 | °C | Average annual air temperature |
Hgod | 1183.7 | mm | Average annual quantity of precipitation |
18.69 % | Sand, gravel and incoherent soils |
0 % | Saline soils... |
0 % | Decomposed limestone and marls |
50.99 % | Serpentines, red sand stones, flishe deposits |
0 % | Podzols and parapodzols, decomposed schist |
30.32 % | Solid and Schist limestone, Terra Rosa and Humic soil |
0 % | 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 |
1.48 % | Plough-lands |
1.36 % | Orchards and vineyards |
32.88 % | Mountain pastures |
11.14 % | Meadows |
11.26 % | Degraded forests |
41.88 % | Well-constituted forests |
1.46 % | Depth erosion |
1.52 % | 80% of the river basin under rill and gully erosion |
6.58 % | 50% of the river basin under rill and gully erosion |
5.64 % | 100% of the river basin under surface erosion |
17.14 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
2.82 % | 50% of the river basin under surface erosion |
8.88 % | 20% of the river basin under surface erosion |
0 % | There are smaller slides in the watercourse beds |
1.48 % | The river basin mostly under plough-land |
54.48 % | The river basin under forests and perennial vegetation |
A | 1.4271018448878 | / | Coefficient of the river basin form |
m | 0.15481732210181 | / | Coefficient of the watershed development |
B | 3.5338 | km | Average river basin width |
a | 0.075197615409286 | / | (A)symmetry of the river basin |
G | 0.26650961193805 | / | Density of the river network of the basin |
K | 1.0296837559336 | / | Coefficient of the river basin tortuousness |
Hsr | 1118.6156132681 | m | Average river basin altitude |
Dsr | 339.6156132681 | m | Average elevation difference of the river basin |
Isr | 36.743614050974 | % | Average river basin decline |
Hleb | 805 | m | The height of the local erosion base of the river basin |
Er | 178.56247814031 | / | Coefficient of the erosion energy of the river basin's relief |
W | 1.3973735629116 | m | Analytical presentation of the water retention in inflow |
S1 | 0.80245 | / | Coefficient of the region's permeability |
S2 | 0.6966724866 | / | Coefficient of the vegetation cover |
2gDF1/2 | 168.09505273417 | m km s-1 | Energetic potential of water flow during torrent rains |
Qmax | 187.39977395426 | m3 s-1 | Maximal outflow from the river basin |
T | 1 | / | Temperature coefficient of the region |
Z | 0.39528977480512 | / | Coefficient of the river basin erosion |
Wgod | 3919.1158657626 | m3 god-1 | Production of erosion material in the river basin |
Ru | 0.30116259118955 | / | Coefficient of the deposit retention |
Ggod | 1180.2910893052 | m3 god-1 | Real soil losses |
Ggod km-2 | 278.33377886533 | m3 km-2 god-1 | Real soil losses per km2 |