Gilgit River
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| Gilgit River | |
|---|---|
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| Lua error in package.lua at line 80: module 'Module:InfoboxImage/data' not found. Course of the Gilgit River | |
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| Native name | Template:Native name checker |
| Location | |
| Country | Pakistan |
| Autonomous territory | Gilgit-Baltistan |
| Districts | Gupis-Yasin, Ghizer and Gilgit |
| Physical characteristics | |
| Mouth | |
• coordinates | Lua error: callParserFunction: function "#coordinates" was not found. |
• elevation | Template:Infobox river/calcunit |
| Length | Template:Infobox river/calcunit |
Basin size | Template:Infobox river/calcunit |
| • minimum | Template:Infobox river/calcunit |
| • average | Template:Infobox river/calcunit |
| • maximum | Template:Infobox river/calcunit |
| Basin features | |
| Progression | Template:RIndus |
| Tributaries | |
| • right | Hunza River |
| Waterbodies | Shandur Lake, Khukush Lake |
Script error: No such module "Check for conflicting parameters". The Gilgit River (Template:Langx) is a tributary of the Indus River, flowing through Gilgit Valley of Gilgit-Baltistan, Pakistan.[1] The upper sections of the Gilgit River are also referred to as the Gupis River and Ghizer River.
Course
Gilgit River flows through various districts including Gupis-Yasin, Ghizer and Gilgit. It originates from Shandur Lake and proceeds to join the Indus River near the towns of Juglot and Bunji. During its course, Yasin River from Yasin Valley and Karambar/Ishkoman River from Karambar Lake in Ishkoman Valley join it. Hunza River is its largest tributary, contributing over half of its mean annual volume. The confluence of Gilgit River with Indus marks the meeting point of three prominent mountain ranges: the Hindu Kush, the Himalayas, and the Karakoram.[2]
Hydrology
The catchment area of Gilgit River is Template:Cvt.[3] Before the confluence of Gilgit River with Hunza River, its mean annual discharge for the period 1981–2010 at Gilgit Gauging Station is Template:Cvt, with a minimum and maximum discharge of Template:Cvt and Template:Cvt, respectively.[3] After receiving inflow from Hunza, its mean annual discharge for the period 1981–2015 at Alam Bridge Gauging Station was Template:Cvt, with a minimum and maximum discharge of Template:Cvt and Template:Cvt, respectively.[1]
See also
References
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- ^ a b Page Module:Citation/CS1/styles.css has no content.Adnan, Muhammad; Nabi, Ghulam; Saleem Poomee, Muhammad; Ashraf, Arshad (2017-09-01). "Snowmelt runoff prediction under changing climate in the Himalayan cryosphere: A case of Gilgit River Basin". Geoscience Frontiers. 8 (5): 941–949. Bibcode:2017GeoFr...8..941A. doi:10.1016/j.gsf.2016.08.008. ISSN 1674-9871.
- ^ Page Module:Citation/CS1/styles.css has no content.Adnan, Muhammad; Liu, Shiyin; Saifullah, Muhammad; Iqbal, Mudassar; Saddique, Qaisar; Ul Hussan, Waqas; Latif, Yasir (2024-12-31). "Estimation of changes in runoff and its sources in response to future climate change in a critical zone of the Karakoram mountainous region, Pakistan in the near and far future". Geomatics, Natural Hazards and Risk. 15 (1) 2291330. Bibcode:2024GNHR...1591330A. doi:10.1080/19475705.2023.2291330. ISSN 1947-5705.
- ^ a b Page Module:Citation/CS1/styles.css has no content.Ul Hussan, Waqas; Khurram Shahzad, Muhammad; Seidel, Frank; Costa, Anna; Nestmann, Franz (2020-03-06). "Comparative Assessment of Spatial Variability and Trends of Flows and Sediments under the Impact of Climate Change in the Upper Indus Basin". Water. 12 (3): 730. Bibcode:2020Water..12..730U. doi:10.3390/w12030730. hdl:20.500.11850/409275. ISSN 2073-4441.
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