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Article

Comparing Combined 1D/2D and 2D Hydraulic Simulations Using High-Resolution Topographic Data: Examples from Sri Lanka—Lower Kelani River Basin

by
Jayanga T. Samarasinghe
1,
Vindhya Basnayaka
2,
Miyuru B. Gunathilake
3,
Hazi M. Azamathulla
4 and
Upaka Rathnayake
2,*
1
Department of Earth Environmental and Resource Sciences, University of Texas, El Paso, TX 79968, USA
2
Department of Civil Engineering, Faculty of Engineering, Sri Lanka Institute of Information Technology, Colombo 10115, Sri Lanka
3
Environment and Natural Resources, Norwegian Institute of Bioeconomy and Research, 1433 Ås, Norway
4
Department of Civil and Environmental Engineering, Faculty of Engineering, University of West Indies, St. Augustine 32080, Trinidad and Tobago
*
Author to whom correspondence should be addressed.
Hydrology 2022, 9(2), 39; https://doi.org/10.3390/hydrology9020039
Submission received: 18 January 2022 / Revised: 15 February 2022 / Accepted: 16 February 2022 / Published: 17 February 2022
(This article belongs to the Special Issue Climate Change Effects on Hydrology and Water Resources)

Abstract

The application of numerical models to understand the behavioural pattern of a flood is widely found in the literature. However, the selection of an appropriate hydraulic model is highly essential to conduct reliable predictions. Predicting flood discharges and inundation extents are the two most important outcomes of flood simulations to stakeholders. Precise topographical data and channel geometries along a suitable hydraulic model are required to accurately predict floods. One-dimensional (1D) hydraulic models are now replaced by two-dimensional (2D) or combined 1D/2D models for higher performances. The Hydraulic Engineering Centre’s River Analysis System (HEC-RAS) has been widely used in all three forms for predicting flood characteristics. However, comparison studies among the 1D, 2D to 1D/2D models are limited in the literature to identify the better/best approach. Therefore, this research was carried out to identify the better approach using an example case study of the Kelani River basin in Sri Lanka. Two flood events (in 2016 and 2018) were separately simulated and tested for their accuracy using observed inundations and satellite-based inundations. It was found that the combined 1D/2D HEC-RAS hydraulic model outperforms other models for the prediction of flows and inundation for both flood events. Therefore, the combined model can be concluded as the better hydraulic model to predict flood characteristics of the Kelani River basin in Sri Lanka. With more flood studies, the conclusions can be more generalized.
Keywords: 1D/2D model; 2D model; HEC-RAS; hydraulic simulations; Kelani River basin 1D/2D model; 2D model; HEC-RAS; hydraulic simulations; Kelani River basin

Share and Cite

MDPI and ACS Style

Samarasinghe, J.T.; Basnayaka, V.; Gunathilake, M.B.; Azamathulla, H.M.; Rathnayake, U. Comparing Combined 1D/2D and 2D Hydraulic Simulations Using High-Resolution Topographic Data: Examples from Sri Lanka—Lower Kelani River Basin. Hydrology 2022, 9, 39. https://doi.org/10.3390/hydrology9020039

AMA Style

Samarasinghe JT, Basnayaka V, Gunathilake MB, Azamathulla HM, Rathnayake U. Comparing Combined 1D/2D and 2D Hydraulic Simulations Using High-Resolution Topographic Data: Examples from Sri Lanka—Lower Kelani River Basin. Hydrology. 2022; 9(2):39. https://doi.org/10.3390/hydrology9020039

Chicago/Turabian Style

Samarasinghe, Jayanga T., Vindhya Basnayaka, Miyuru B. Gunathilake, Hazi M. Azamathulla, and Upaka Rathnayake. 2022. "Comparing Combined 1D/2D and 2D Hydraulic Simulations Using High-Resolution Topographic Data: Examples from Sri Lanka—Lower Kelani River Basin" Hydrology 9, no. 2: 39. https://doi.org/10.3390/hydrology9020039

APA Style

Samarasinghe, J. T., Basnayaka, V., Gunathilake, M. B., Azamathulla, H. M., & Rathnayake, U. (2022). Comparing Combined 1D/2D and 2D Hydraulic Simulations Using High-Resolution Topographic Data: Examples from Sri Lanka—Lower Kelani River Basin. Hydrology, 9(2), 39. https://doi.org/10.3390/hydrology9020039

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