Latitude: 42.98746 | Longitude: 19.755437 | Country: Montenegro | Year: 2018 |
F | 9.88503 | km2 | Surface area of the drainage basin |
Fm | 3.52042 | km2 | Surface area of smaller portion of the drainage basin |
Fv | 6.36461 | km2 | Surface area of greater portion of the drainage basin |
O | 14.83463 | km | The length of the watershed |
Lv | 3.70578 | km | Natural length of the main watercourse |
Lb | 6.26708 | km | Surface area of greater portion of the drainage basin |
Liz | ["0.3181 ","1.31226 ","2.12829 ","4.51802 ","5.523 ","6.75476 ","7.30353 ","7.69399 ","8.05699 ","7.84416 ","4.52585 ","3.23553 ","3.35417 ","3.21198 ","3.23518 ","3.47135 ","3.26101 ","2.82166 ","2.96052 ","2.25237 ","1.84255 ","2.15 | km | Contour line length |
f | ["0.012686275 ","0.075166667 ","0.201147059 ","0.376539216 ","0.475588235 ","0.773588235 ","1.000970588 ","0.838009804 ","0.908764706 ","0.949941176 ","0.919607843 ","0.381372549 ","0.372745098 ","0.271343137 ","0.31872549 ","0.23422549 ", | km2 | The area between the two neighboring contour lines |
h0 | 600 | m | Altitude of the first contour line |
Δh | 50 | m | Equidistance |
Hmin | 580 | m | Lowest altitude in the drainage basin |
Hmax | 1757 | m | Highest altitude in the draigane basin |
ΣL | 10.10603 | km | The total length of the main watercourse with tributaries of 1st and 2nd class |
Lm | 2.52952 | km | The shortest distance between the fountain - head and mouth |
fp | 0 | m | A part of the river basin consisted of a very permeable products from rocks (limestone, sand, gravel) |
fpp | 0.1157 | m | A part of the river basin area consisted of medium permeable rocks (slates, marls, brownstone) |
fo | 0.8843 | m | A part of the river basin consisted of poor water permeability rocks (heavy clay, compact eruptive) |
fs | 0.676996973 | m | Part of the surface area of the drainage basin under the forest |
ft | 0.261297321 | m | Part of the surface area of the drainage basin which is under the grass, meadows, pastures and orchards |
fg | 0.061705706 | m | Part of the surface area of the drainage basin which is bare or under the soils without grass vegetation |
Hb | 157.6 | mm | The volume of the torrent rain |
Up | 100 | years | Incidence |
to | 8.9 | °C | Average annual air temperature |
Hgod | 983.7 | mm | Average annual quantity of precipitation |
11.39 % | Sand, gravel and incoherent soils |
0 % | Saline soils... |
0 % | Decomposed limestone and marls |
0 % | Serpentines, red sand stones, flishe deposits |
39.38 % | Podzols and parapodzols, decomposed schist |
0 % | Solid and Schist limestone, Terra Rosa and Humic soil |
29.54 % | Brown forest soils and Mountain soils |
0 % | Epieugleysol and Marshlands |
0 % | Good structured Chernozems and alluvial well-structured deposits |
19.69 % | Bare, compact igneous |
0 % | Bare lands |
6.17 % | Plough-lands |
5.86 % | Orchards and vineyards |
3.9 % | Mountain pastures |
16.37 % | Meadows |
44 % | Degraded forests |
23.69 % | Well-constituted forests |
1 % | Depth erosion |
0.89 % | 80% of the river basin under rill and gully erosion |
0.78 % | 50% of the river basin under rill and gully erosion |
0.67 % | 100% of the river basin under surface erosion |
16.37 % | 100% of the river basin under surface erosion, without visible furrows, ravines and land slides |
0.33 % | 50% of the river basin under surface erosion |
0.22 % | 20% of the river basin under surface erosion |
0 % | There are smaller slides in the watercourse beds |
6.17 % | The river basin mostly under plough-land |
73.57 % | The river basin under forests and perennial vegetation |
A | 0.7806056619659 | / | Coefficient of the river basin form |
m | 0.33249544895342 | / | Coefficient of the watershed development |
B | 1.5772943699458 | km | Average river basin width |
a | 0.57545399457564 | / | (A)symmetry of the river basin |
G | 1.022357038876 | / | Density of the river network of the basin |
K | 1.4650131250198 | / | Coefficient of the river basin tortuousness |
Hsr | 1055.6012384204 | m | Average river basin altitude |
Dsr | 475.6012384204 | m | Average elevation difference of the river basin |
Isr | 45.087627452825 | % | Average river basin decline |
Hleb | 1177 | m | The height of the local erosion base of the river basin |
Er | 211.29153209166 | / | Coefficient of the erosion energy of the river basin's relief |
W | 1.7265533765394 | m | Analytical presentation of the water retention in inflow |
S1 | 0.96529 | / | Coefficient of the region's permeability |
S2 | 0.6769417466 | / | Coefficient of the vegetation cover |
2gDF1/2 | 303.71062517259 | m km s-1 | Energetic potential of water flow during torrent rains |
Qmax | 267.47352216594 | m3 s-1 | Maximal outflow from the river basin |
T | 0.99498743710662 | / | Temperature coefficient of the region |
Z | 0.36980689582108 | / | Coefficient of the river basin erosion |
Wgod | 6835.5055602383 | m3 god-1 | Production of erosion material in the river basin |
Ru | 0.3876020693761 | / | Coefficient of the deposit retention |
Ggod | 2649.4561003802 | m3 god-1 | Real soil losses |
Ggod km-2 | 268.0271178115 | m3 km-2 god-1 | Real soil losses per km2 |