Khor Daga
Daga Deqe Sonka Shet | ||
| ||
Daten | ||
Lage | Upper Nile, Südsudan, Äthiopien Südsudan | |
Flusssystem | Nil | |
Abfluss über | Machar-Sümpfe → Khor Adar → Weißer Nil → Nil → Mittelmeer | |
Quelle | im Osten des Bundesstaates Upper Nile | |
Mündung | im ausgedehnten Sumpfgebiet der Machar-SümpfeKoordinaten: 9° 32′ 0″ N, 33° 24′ 0″ O 9° 32′ 0″ N, 33° 24′ 0″ O
| |
Einzugsgebiet | 3200 km²[1] | |
Abfluss am Pegel Daga Post[1] AEo: 1900 km² |
NNQ MNQ 1950–1954 MQ 1950–1954 Mq 1950–1954 MHQ 1950–1954 |
0 l/s 120 l/s 13,2 m³/s 6,9 l/(s km²) 42,1 m³/s |
Der Khor Daga (Daga River), äthiopisch: Deqe Sonka Shet, ist ein Fluss in Äthiopien und Südsudan.
Verlauf
Er entsteht in den Bergen der Mirab Welega Zone in Äthiopien an der Grenze zum Südsudan.[2] Er verläuft nach Westen, passiert die Stadt Daga Post im Bundesstaat Upper Nile und tritt dann ein in die Machar-Sümpfe,[3] wo sein Verlauf nicht mehr nachvollziehbar ist.[4]
Hydrometrie
Die Durchflussmenge des Daga wurde an der hydrologischen Station Daga Post bei etwa 60 % des Einzugsgebietes, über die Jahre 1950 bis 1954 gemittelt, in m³/s gemessen.[1]
<graph>{"legends":[],"scales":[{"type":"ordinal","name":"x","zero":false,"domain":{"data":"chart","field":"x"},"padding":0.2,"range":"width","nice":true},{"type":"linear","name":"y","domain":{"data":"chart","field":"y"},"zero":true,"range":"height","nice":true},{"domain":{"data":"chart","field":"series"},"type":"ordinal","name":"color","range":"category10"}],"version":2,"marks":[{"type":"rect","properties":{"hover":{"fill":{"value":"red"}},"update":{"fill":{"scale":"color","field":"series"}},"enter":{"y":{"scale":"y","field":"y"},"x":{"scale":"x","field":"x"},"y2":{"scale":"y","value":0},"width":{"scale":"x","offset":-1,"band":true},"fill":{"scale":"color","field":"series"}}},"from":{"data":"chart"}},{"type":"text","properties":{"enter":{"baseline":{"value":"middle"},"align":{"value":"left"},"text":{"field":"y"},"y":{"scale":"y","offset":-4,"field":"y"},"dy":{"scale":"x","mult":0.5,"band":true},"x":{"scale":"x","field":"x"},"angle":{"value":-90},"fontSize":{"value":11},"fill":{"value":"#54595d"}}},"from":{"data":"chart"}}],"height":200,"axes":[{"type":"x","scale":"x","properties":{"title":{"fill":{"value":"#54595d"}},"grid":{"stroke":{"value":"#54595d"}},"ticks":{"stroke":{"value":"#54595d"}},"axis":{"strokeWidth":{"value":2},"stroke":{"value":"#54595d"}},"labels":{"fill":{"value":"#54595d"}}},"grid":false},{"type":"y","scale":"y","properties":{"title":{"fill":{"value":"#54595d"}},"grid":{"stroke":{"value":"#54595d"}},"ticks":{"stroke":{"value":"#54595d"}},"axis":{"strokeWidth":{"value":2},"stroke":{"value":"#54595d"}},"labels":{"fill":{"value":"#54595d"}}},"grid":false}],"data":[{"format":{"parse":{"y":"number","x":"string"},"type":"json"},"name":"chart","values":[{"y":0.66,"series":"y","x":"Jan"},{"y":0.51,"series":"y","x":"Feb"},{"y":0.12,"series":"y","x":"März"},{"y":0.4,"series":"y","x":"April"},{"y":2.18,"series":"y","x":"Mai"},{"y":6.32,"series":"y","x":"Juni"},{"y":18,"series":"y","x":"Juli"},{"y":42.1,"series":"y","x":"Aug"},{"y":36.2,"series":"y","x":"Sept"},{"y":34.2,"series":"y","x":"Okt"},{"y":14,"series":"y","x":"Nov"},{"y":4.08,"series":"y","x":"Dez"}]}],"width":400}</graph>
Siehe auch
Einzelnachweise
- ↑ a b c Water Balance Estimates of the Machar Marshes
- ↑ Topographical map of Jonglei Archivlink.
- ↑ J. V. Sutcliffe, Y. P. Parls: The Hydrology of the Nile. Kap. The Sobat Basin and the Machar Marshes. 1999. Archivlink S. 112.
- ↑ Khor Daga bei GeoNames geonames.org. Abgerufen am 19. Juni 2022.