Hydrodynamic modeling of ephemeral flow in the Iishana channel systems of the Cuvelai Basin—Northern Namibia

Medientyp: E-Artikel

Titel: Hydrodynamic modeling of ephemeral flow in the Iishana channel systems of the Cuvelai Basin—Northern Namibia

Beteiligte: Arendt, Robert [Verfasser:in]; Reinhardt‐Imjela, Christian [Verfasser:in]; Faulstich, Leona [Verfasser:in]; Schulte, Achim [Verfasser:in]; Assmann, André [Verfasser:in]; Jüpner, Robert [Verfasser:in]; Johannes, Petrina T. [Verfasser:in]; Mashauri, Damas Alfred [Verfasser:in]

Erschienen: John Wiley & Sons, Ltd.; Chichester, UK, 2023-07-13

Sprache: Englisch

DOI: https://doi.org/10.1002/rra.4187

ISSN: 1535-1459; 1535-1467

Schlagwörter: SCS‐CN ; TRMM ; flood ; FloodArea11 ; TanDEM‐X

Entstehung:

Anmerkungen: Diese Datenquelle enthält auch Bestandsnachweise, die nicht zu einem Volltext führen.

Beschreibung: Abstract The transboundary region of the Iishana system in the western Cuvelai Basin, between southern Angola and northern Namibia, is frequently affected by floods at irregular intervals. As a result, the predominantly rural, subsistence farming population has experienced crop failures, human, and economic losses. To date, very little is known about the generation of floods, flood concentration, and stormwater drainage dynamics in this region. In this study, 2D‐hydrodynamic modeling was applied to reconstruct one of the latest major flood events during the rainy season from November 2008 to March 2009 in order to study the runoff behavior and interconnectivity of the Iishana system. The model focused on the eastern part of the Iishana system, which was most affected by floods and flood damage due to the high population density in and around Oshakati, the regional capital. Two main streams were identified noteworthy because they merge and subsequently affect Oshakati. Regarding the simulated flood event water depths vary from 0.1 m to 14 m, with an average of 0.2 m, while water depths above 5 m were attributed to borrow pits. The inundation area ranged up to 1860 km 2 and the amount of water left after the rainy season on March 25th, 2009, was determined between 0.116 and 0.547 km 3 , depending on the amount of evapotranspiration considered in the model. Thus, in the Angolan part of the Iishana system, significantly larger quantities of water are available for longer periods of time during the subsequent dry season, whereas the system in Namibia stores less water, resulting in a shorter water retention period. ; Deutsche Hydrologische Gesellschaft (DHG) ; Freie Universität Berlin http://dx.doi.org/10.13039/501100007537 ; https://dx.doi.org/10.17169/refubium-35737

Zugangsstatus: Freier Zugang

Nur in Feld suchen:

Zuletzt gesuchte Begriffe: