Modelling the inundation and morphology of the seasonally flooded Mayas Wetlands in the Dinder National Park-Sudan

Understanding the spatiotemporal dynamics of surface water in varied, remote and inaccessible isolated floodplain lakes is difficult. Seasonal inundation patterns of these isolated lakes can be misestimated in a hydrodynamic model due to the short time of connectivity. The seasonal and annual variab...

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Main Authors: Hassaballah, K., Mohamed, Y., Omer, A., Uhlenbrook, Stefan
Format: Journal Article
Language:Inglés
Published: Springer 2020
Subjects:
Online Access:https://hdl.handle.net/10568/108935
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author Hassaballah, K.
Mohamed, Y.
Omer, A.
Uhlenbrook, Stefan
author_browse Hassaballah, K.
Mohamed, Y.
Omer, A.
Uhlenbrook, Stefan
author_facet Hassaballah, K.
Mohamed, Y.
Omer, A.
Uhlenbrook, Stefan
author_sort Hassaballah, K.
collection Repository of Agricultural Research Outputs (CGSpace)
description Understanding the spatiotemporal dynamics of surface water in varied, remote and inaccessible isolated floodplain lakes is difficult. Seasonal inundation patterns of these isolated lakes can be misestimated in a hydrodynamic model due to the short time of connectivity. The seasonal and annual variability of the Dinder River flow has great impact on what is so called Mayas wetlands, and hence, on the habitats and the ecological status of the Dinder National Park. This variability produces large morphological changes due to sediment transported within the river or from the upper catchment, which affects inflows to Mayas wetlands and floodplain inundation in general. In this paper, we investigated the morphological dimension using a quasi-3D modelling approach to support the management of the valuable Mayas wetlands ecosystems, and in particular, assessment of hydrological and morphological regime of the Dinder River as well as the Musa Maya. Six scenarios were developed and tested. The first three scenarios consider three different hydrologic conditions of average, wet and dry years under the existing system with the constructed connection canal. While the other three scenarios consider the same hydrologic conditions but under the natural system without an artificial connection canal. The modelling helps to understand the effect of human intervention (connection canal) on the Musa Maya. The comparison between the simulated scenarios concludes that the hydrodynamics and sedimentology of the Maya are driven by the two main factors: a) the hydrological variability of Dinder River; and b) deposited sediment plugs in the connection canal.
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spelling CGSpace1089352023-12-08T19:36:04Z Modelling the inundation and morphology of the seasonally flooded Mayas Wetlands in the Dinder National Park-Sudan Hassaballah, K. Mohamed, Y. Omer, A. Uhlenbrook, Stefan wetlands floodplains flooding hydrodynamics modelling hydrological factors morphology water levels sediment erosion canals rivers national parks ecosystems Understanding the spatiotemporal dynamics of surface water in varied, remote and inaccessible isolated floodplain lakes is difficult. Seasonal inundation patterns of these isolated lakes can be misestimated in a hydrodynamic model due to the short time of connectivity. The seasonal and annual variability of the Dinder River flow has great impact on what is so called Mayas wetlands, and hence, on the habitats and the ecological status of the Dinder National Park. This variability produces large morphological changes due to sediment transported within the river or from the upper catchment, which affects inflows to Mayas wetlands and floodplain inundation in general. In this paper, we investigated the morphological dimension using a quasi-3D modelling approach to support the management of the valuable Mayas wetlands ecosystems, and in particular, assessment of hydrological and morphological regime of the Dinder River as well as the Musa Maya. Six scenarios were developed and tested. The first three scenarios consider three different hydrologic conditions of average, wet and dry years under the existing system with the constructed connection canal. While the other three scenarios consider the same hydrologic conditions but under the natural system without an artificial connection canal. The modelling helps to understand the effect of human intervention (connection canal) on the Musa Maya. The comparison between the simulated scenarios concludes that the hydrodynamics and sedimentology of the Maya are driven by the two main factors: a) the hydrological variability of Dinder River; and b) deposited sediment plugs in the connection canal. 2020-09 2020-08-04T06:00:55Z 2020-08-04T06:00:55Z Journal Article https://hdl.handle.net/10568/108935 en Open Access Springer Hassaballah, K.; Mohamed, Y.; Omer, A.; Uhlenbrook, Stefan. 2020. Modelling the inundation and morphology of the seasonally flooded Mayas Wetlands in the Dinder National Park-Sudan. Environmental Processes, 7(3):723-747. [doi: 10.1007/s40710-020-00444-5]
spellingShingle wetlands
floodplains
flooding
hydrodynamics
modelling
hydrological factors
morphology
water levels
sediment
erosion
canals
rivers
national parks
ecosystems
Hassaballah, K.
Mohamed, Y.
Omer, A.
Uhlenbrook, Stefan
Modelling the inundation and morphology of the seasonally flooded Mayas Wetlands in the Dinder National Park-Sudan
title Modelling the inundation and morphology of the seasonally flooded Mayas Wetlands in the Dinder National Park-Sudan
title_full Modelling the inundation and morphology of the seasonally flooded Mayas Wetlands in the Dinder National Park-Sudan
title_fullStr Modelling the inundation and morphology of the seasonally flooded Mayas Wetlands in the Dinder National Park-Sudan
title_full_unstemmed Modelling the inundation and morphology of the seasonally flooded Mayas Wetlands in the Dinder National Park-Sudan
title_short Modelling the inundation and morphology of the seasonally flooded Mayas Wetlands in the Dinder National Park-Sudan
title_sort modelling the inundation and morphology of the seasonally flooded mayas wetlands in the dinder national park sudan
topic wetlands
floodplains
flooding
hydrodynamics
modelling
hydrological factors
morphology
water levels
sediment
erosion
canals
rivers
national parks
ecosystems
url https://hdl.handle.net/10568/108935
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