Dynamic Geomorphology of the Amu Darya Basin in Afghanistan: A Study of Physiography, Basin Erosion, and Channel Development

Downloads

Download the Article:

Authors

https://doi.org/10.55559/sjahss.v3i5.313

Keywords:

Amu Darya, physiography, basin denudation, sedimentation, water resource, conservation, sustainable development

Abstract

The morphological dynamics of rivers are motivated by way of a number of things, including floodplain sedimentation, channel migration, sediment transport, and hydrodynamics. A considerable information of the complicated dynamics of river structures is important to layout river initiatives which can be sustainable and environmentally conscious. Implementing thorough river control plans that include hydraulic infrastructure and ecological restoration projects is important to overcoming these boundaries. This solution will effectively manipulate competing needs for water resources whilst ensuring the preservation of the location's herbal heritage. In the cease, this study affords essential new understandings of the complex interactions between hydrological patterns, human hobby, and geological procedures within the Amu Darya Basin. The application of sustainable land control and water useful resource making plans in Afghanistan might be appreciably impacted with the aid of those findings. Afghanistan has a lot of freshwaters because the Hindu Kush Mountains receive a significant quantity of precipitation. An estimated 75 billion cubic meters of potential water resources, consisting of 57 billion cubic meters of surface water and 18 billion cubic meters of groundwater, are found in Afghanistan. The Amu Darya, Northern River Basin, Helmand River Basin, Harirud-Marghab River Basin, and Kabul River Basin make up the Indus River Basin, which provides around two-thirds of Afghanistan's freshwater resources. All of Afghanistan's rivers, with the exception of the Northern River, flow across international borders into neighboring countries. The distribution of water from the Amu Darya River was subject to limitations imposed by the USSR, which was previously known as the Union of Soviet Socialist Republics. The majority of the water is used mostly for farming. Protocol 566, formally ratified by the former USSR, allowed the transfer of water from the Amu Darya River to the four Central Asian Republics (CARs) of Tajikistan, Uzbekistan, Turkmenistan, and the Kyrgyz Republic. By investigating the bodily functions of the basin, which includes land erosion and channel development, this looks at seeks to enhance our understanding of the landscape evolution of the basin. Our intention is to improve our information of the landforms, tectonic activity history, and the consequences of climate change inside the region by utilizing geological studies and facts from faraway sensing.

Downloads

Download data is not yet available.

References

Asarin, A. E., Kravtsova, V. I., & Mikhailov, V. N. (2009). Amudarya and Syrdarya rivers and their deltas. In The handbook of environmental chemistry (pp. 101–121). https://doi.org/10.1007/698_2009_8 DOI: https://doi.org/10.1007/698_2009_8

Bates, B. E. (2008). Climate Change and Water, Technical Paper of the Intergovernmental Panel on Climate Change. DOI: https://doi.org/10.1017/CBO9780511546013

Bolch, T., Shea, J. M., Liu, S., Azam, F. M., Gao, Y., Gruber, S., Immerzeel, W. W., Kulkarni, A., Li, H., Tahir, A. A., Zhang, G., & Zhang, Y. (2019). Status and change of the cryosphere in the extended Hindu Kush Himalaya region. In Springer eBooks (pp. 209–255). https://doi.org/10.1007/978-3-319-92288-1_7 DOI: https://doi.org/10.1007/978-3-319-92288-1_7

Fairbridge, R. W. (1968). The Encyclopedia of Geomorphology. New york: Reinhold.

Froebrich, J., Olsson, O., Bauer, M., Normatov, I., & Petrov, G. (2006). Improved dam operation in the Amu Darya river basin including transboundary aspects. In CRC Press eBooks (pp. 97–103). https://doi.org/10.1201/b16818-16 DOI: https://doi.org/10.1201/b16818-16

Hagg, W., Hoelzle, M., Wagner, S., Mayr, E., & Klose, Z. (2013). Glacier and runoff changes in the Rukhk catchment, upper Amu-Darya basin until 2050. Global and Planetary Change, 110, 62–73. https://doi.org/10.1016/j.gloplacha.2013.05.005 DOI: https://doi.org/10.1016/j.gloplacha.2013.05.005

Huntington, T. G. (2006). Evidence for intensification of the global water cycle: Review and synthesis. Journal of Hydrology, 319(1–4), 83–95. https://doi.org/10.1016/j.jhydrol.2005.07.003 DOI: https://doi.org/10.1016/j.jhydrol.2005.07.003

Klötzli. (1994). Agreement concluded in 1994 between the Governments of Tajikistan and Uzbekistan on improving the ecological situationaround TADAZ.

Kostianoy, A. G., Lebedev, S. A., & Solovyov, D. M. (2013). Satellite monitoring of the Caspian Sea, Kara-Bogaz-Gol Bay, Sarykamysh and Altyn Asyr lakes, and Amu Darya River. In The handbook of environmental chemistry (pp. 197–231). https://doi.org/10.1007/698_2013_237 DOI: https://doi.org/10.1007/698_2013_237

Langat, P. K., Kumar, L., & Koech, R. (2019). Monitoring river channel dynamics using remote sensing and GIS techniques. Geomorphology, 325, 92–102. https://doi.org/10.1016/j.geomorph.2018.10.007 DOI: https://doi.org/10.1016/j.geomorph.2018.10.007

Salehie, O., Ismail, T. B., Shahid, S., Hamed, M. M., Chinnasamy, P., & Wang, X. (2022). Assessment of water resources availability in Amu Darya River Basin using GRACE data. Water, 14(4), 533. https://doi.org/10.3390/w14040533 DOI: https://doi.org/10.3390/w14040533

Schlüter, M., & Herrfahrdt-Pähle, E. (2011). Exploring Resilience and Transformability of a River Basin in the Face of Socioeconomic and Ecological Crisis: an Example from the Amudarya River Basin, Central Asia. Ecology and Society, 16(1). https://www.jstor.org/stable/26268847 DOI: https://doi.org/10.5751/ES-03910-160132

Sidle, R. C., Caiserman, A., Jarihani, B., Khojazoda, Z., Kiesel, J., Kulikov, M., & Qadamov, A. (2023). Sediment Sources, Erosion Processes, and Interactions with Climate Dynamics in the Vakhsh River Basin, Tajikistan. Water, 16(1), 122. https://doi.org/10.3390/w16010122 DOI: https://doi.org/10.3390/w16010122

Vadillo, J. A. (2013). DUNNE, T., 1978. Field studies of hillslope flow processes. In: Hillslope Hydrology. Ed. M.J. Kirkby, pp. 227-293. Cuadernos De Investigación Geográfica, 9, 105–107. https://doi.org/10.18172/cig.1099 DOI: https://doi.org/10.18172/cig.1099

Published on: 2024-05-16

Also Available On

Note: Third-party indexing sometime takes time. Please wait one week or two for indexing. Validate this article's Schema Markup on Schema.org

How to Cite

Ahmadi, J. (2024). Dynamic Geomorphology of the Amu Darya Basin in Afghanistan: A Study of Physiography, Basin Erosion, and Channel Development. Sprin Journal of Arts, Humanities and Social Sciences, 3(5), 48–52. https://doi.org/10.55559/sjahss.v3i5.313
2583-2387