Bug (river)

Template:Short description Template:About

The Bug or Western BugTemplate:Efn is a major river in Central Europe that flows through Belarus (border), Poland, and Ukraine, with a total length of Template:Convert.<ref name=yearbook>Statistical Yearbook of the Republic of Poland 2017, Statistics Poland, p. 85-86</ref> A tributary of the Narew, the Bug forms part of the border between Belarus and Poland for Template:Convert and part of the border between Ukraine and Poland for Template:Convert.<ref name="floodwise"/><ref name=statistics>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

The Bug is connected with the Dnieper by the Dnieper–Bug Canal. Out of its Template:Convert drainage basin, half is in Poland,<ref name=yearbook/> just over a quarter in Belarus, and slightly under a quarter in Ukraine.<ref name="floodwise"/>

HistoryEdit

According to Zbigniew Gołąb, the Slavic hydronym Bug as *bugъ/*buga derives from the Proto-Indo-European verbal root *bheug- (with cognates in old Proto-Germanic *bheugh- etc. with the meaning 'bend, turn, move away'), with the hypothetical original meaning 'pertaining to a (river) bend', and derivatives in Russian búga 'low banks of a river overgrown with bushes', Polish bugaj 'bushes or woods in a river valley or on a steep river bank', and Latvian bauga 'marshy place by a river'.<ref>Template:Citation</ref>

Traditionally (e.g., by the drafters of the Curzon Line), the Bug River has been considered the ethnographic border between the East and West as well as the border between Orthodox (Ukrainians, Belarusians) and Catholic (Poles) peoples.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Template:Verify source

The Bug was part of the frontier between the territories occupied by Austria, Russia, and Prussia after the Third Partition of Poland in 1795, the southern half of the eastern border of the Duchy of Warsaw and Lithuanian Provisional Governing Commission (1809–1815), Congress Poland and Russia proper (1815–1867), of the Vistula Land and Russia proper (1867–1913), and of the Regency Kingdom of Poland and BPR (1917–1918). The Bug also formed part of the dividing line between German Wehrmacht and Soviet Red Army zones specified in a secret clause of the German–Soviet Frontier Treaty of 28 September 1939 following the September 1939 invasion of Poland in the Second World War.

Geographic characteristicsEdit

File:Łazienki - Pałac na wodzie - 20.jpg

Allegory of the Bug River, a statue on the terrace of the Łazienki Palace in Royal Baths Park, Warsaw, Poland

The Bug is a left tributary of the Narew. It flows from the Lviv Oblast in the west of Ukraine northwards into the Volyn Oblast, before passing along the Ukraine-Polish and Polish-Belarusian border and into Poland, where it follows part of the border between the Masovian and Podlaskie Voivodeships. It joins the Narew at Serock, a few kilometers upstream of the artificial Zegrze Lake, which was constructed in 1963 with a hydroelectric complex.<ref name="floodwise">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

This part of the Narew between the confluence and the Vistula is sometimes referred to as Bugo-Narew but on December 27, 1962, the Prime Minister of Poland's act abolished the name "Bugo-Narew", soon after Zegrze Lake was completed.<ref name="Monitor">Template:In lang "Monitor Polski" 1963, nr 3, poz. 6</ref>

On the Bug, a few kilometers from the Vysokaye in Kamenets District of the Brest Region, is the westernmost point of Belarus.<ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> It is also connected with the Dnieper via the Mukhavets, a right-bank tributary, by the Dnieper-Bug Canal.

BasinEdit

The total basin area of the Bug is Template:Convert of which half, Template:Convert or, 50%, is in Poland.<ref name=yearbook/> Somewhat more than a quarter, Template:Convert or 29%, is in Belarus, and a bit under a quarter, Template:Convert or 22% lies in Ukraine.<ref name="floodwise"/>

The climate of the Bug basin is temperate.<ref name="floodwise"/>

The basin experiences annual high-water levels during spring flooding due to thawing snow, after which a low flow period starts and lasts until October or mid-November. Occasional summer floods often occur in the headlands, where mountains influence favorable flash-flood conditions. In Autumn the water level increases are inconsiderable; in some years they do not happen at all. During the winter the river can have temporary ice-outs that sometimes provoke ice jams, causing an increase of the level up to Template:Convert. The resultant water levels are changeable due to the instability of ice cover.<ref name="floodwise"/>

FloodingEdit

Significant floods during the last 60 years in Belarus were registered in 1958, 1962, 1967, 1971 and 1974.<ref name="floodwise"/> The largest spring flood was observed in 1979, when the maximum water discharge was 19.1 cubic metres per second on 24 March 1979, at the village of Chersk; 166 cubic metres per second near the village of Tyukhinichi (Lyasnaya river) on 31 March 1979; and 269 cubic metres per second near Brest on 1 April 1979. A similar spring flood occurred in 1999 when the spring run-off in March–May exceeded the average annual value by almost half again (48%).

The last time the Bug flooded in Poland and Ukraine was in 2010 and the last time it flooded in Belarus was in 1999.<ref name="floodwise"/>