Bar köl
| Bar köl | |
|---|---|
 | |
| Poloha | |
| Světadíl | Asie |
| Stát |  Čína |
| Autonomní oblast | Sin-ťiang |
  | |
| Zeměpisné souřadnice | 43°38′35″ s. š., 92°48′50″ v. d. |
| Rozměry | |
| Rozloha | 140 km² |
| Ostatní | |
| Nadm. výška | 1585 m n. m. |
 multimediální obsah na Commons | |
| Některá data mohou pocházet z datové položky. | |
Bar köl je hořkoslané jezero na severozápadě Číny v mezihorské pusté kotlině na severozápadním úpatí hřbetu Karlik ve východním Ťan-šanu. Má rozlohu 140 km². Rozloha bažin a promáčené půdy v okolí jezera je 250 km². Leží v nadmořské výšce 1585 m.
Pobřeží
Pobřeží je bažinaté. Přibližně 20 km na východ leží město Barkol.
Literatura
- V tomto článku byly použity informace z Velké sovětské encyklopedie, heslo „Баркёль“.
Externí odkazy
Obrázky, zvuky či videa k tématu Bar köl na Wikimedia Commons
Média použitá na této stránce
Autor: Uwe Dedering, Licence: CC BY-SA 3.0
Location map of China.
EquiDistantConicProjection : Central parallel :
- N: 36.0° N
Central meridian :
- E: 104.0° E
Standard parallels:
- 1: 30.0° N
- 2: 42.0° N
Latitudes on the central meridian :
- top: 57.0° E
- center: 37° 29′ N
- bottom: 17.96° N
The green-brown waters of Barkol Lake sit within the pale shorelines of an ancient lake, hinting that the climate was once much wetter in this part of western China. Today the region is arid and brown. Barkol Lake’s annual mean precipitation is 210 millimeters (8 inches), while the annual evaporation rate is 2,250 millimeters (89 inches). The desert lake receives most of its water from runoff, and the water that remains after evaporation is very salty and full of minerals. Square ponds on the edge of the lake are probably evaporation ponds used to extract those minerals from the water.
Astronauts on the International Space Station snapped this photo on the lake on November 6, 2013. The astronauts were looking over the lake from the west, so east is toward the top of the photograph. The basin is closed, which means that the small streams in the photo run into the lake, but nothing runs out. Evaporation is the only means through which water leaves Lake Barkol.
The ancient shorelines show up as concentric rings, indicating that water levels have varied many times. One study identified five climates at Barkol Lake over the past 8,000 years, ranging from warm and wet to cold and wet and finally cold and dry. The average annual temperature in the area is now just 1° Celsius (34° F), though temperatures swing from extreme highs (33.5° C or 92.3° F) to extreme lows (-43.6° C or -46.5° F).