How 1D-2D Models Shape Flood Hazard Management?
Flood frequency mapping in Myanmar (Source: ESA)

How 1D-2D Models Shape Flood Hazard Management?

In flood hazard management, the choice of modeling technique can significantly impact the accuracy and reliability of predictions. While pure 2D models have been widely used, the 1D-2D linked models offer distinct advantages that make them far superior for practical applications. This blog delves into the reasons why 1D-2D linked models are better suited for flood hazard assessment and management.

Understanding 1D-2D Linked Models

1D-2D linked models integrate the strengths of both 1D and 2D hydrodynamic simulations to provide a comprehensive understanding of flood events. In these models, 1D components are used to simulate flow within well-defined channels and rivers, capturing detailed flow dynamics and interactions with hydraulic structures such as bridges and culverts. Meanwhile, 2D components handle the overland flow on floodplains, offering a detailed spatial representation of flood extents, depths, and velocities. By linking these two components, 1D-2D models enable accurate simulation of both channelized and overland flows, optimizing computational efficiency and improving the overall accuracy of flood hazard assessments.

Advantages of 1D-2D Linked Models

Enhanced Computational Efficiency

Pure 2D models require significant computational resources because they must solve complex equations for every grid cell across the entire floodplain. This can be time-consuming and costly, especially for large areas. In contrast, 1D-2D linked models optimize computational efficiency by using 1D simulations in areas where flow is well-defined (like rivers) and 2D simulations only where necessary (like floodplains). This hybrid approach reduces the computational load without sacrificing accuracy.

Improved Accuracy in Channel Flow

Rivers and channels often have complex hydraulic structures such as bridges, culverts, and weirs, which are better represented in 1D models. Pure 2D models may struggle with accurately simulating these features due to their simplified representation of flow. By linking 1D and 2D models, we can utilize the detailed representation of 1D models for channels while still capturing the broader overland flow dynamics with 2D models, resulting in more accurate overall predictions.

Better Representation of Overland Flow

While 1D models excel in channel flow simulation, they fall short in representing overland flow dynamics. Pure 2D models handle overland flow better but at the cost of computational efficiency. The 1D-2D linked models strike a balance by using 2D simulations only where overland flow is significant, thus providing a more detailed and accurate representation of flood extents and depths on the floodplain.

Flexibility in Model Configuration

1D-2D linked models offer greater flexibility in model configuration. Engineers and hydrologists can selectively apply 1D or 2D components based on the specific characteristics of the study area. For example, in urban areas with complex drainage systems, a 1D approach might be used for the drainage network, while a 2D approach can be applied to simulate surface flooding. This flexibility allows for tailored modeling solutions that enhance both accuracy and efficiency.

Improved Risk Assessment and Management

Accurate flood modeling is crucial for effective flood risk assessment and management. 1D-2D linked models provide detailed insights into flood behavior, including flood wave propagation, inundation extents, and flood depths. This information is vital for designing flood mitigation measures, emergency response planning, and informing stakeholders. The hybrid approach ensures that decision-makers have reliable data to make informed choices, ultimately reducing the risk to lives and property.

Practical Applications and Case Studies

Urban Flooding in Mumbai, India

Mumbai, a densely populated coastal city, experiences severe flooding during monsoon seasons. A 1D-2D linked model was implemented to simulate the complex interactions between the urban drainage system (1D) and surface flooding (2D). The model accurately predicted flood extents and depths, enabling city planners to identify critical areas for intervention and improve flood response strategies .

River Flooding in the Mississippi Basin, USA

In the Mississippi Basin, a 1D-2D linked model was used to assess flood risks along the river and its floodplain. The 1D component simulated river flow dynamics, while the 2D component captured overland flow across the floodplain. The integrated model provided detailed flood maps, helping authorities to enhance levee designs and implement better floodplain management practices .

Coastal Flooding in Venice, Italy

Venice faces frequent flooding, exacerbated by high tides and storm surges. A 1D-2D linked model was applied to simulate the interactions between tidal flows (1D) and urban inundation (2D). This approach allowed for precise predictions of flood extents and depths, supporting the design of effective flood defenses, such as the MOSE barrier system .

Flash Flooding in Brisbane, Australia

Brisbane experiences flash flooding due to intense rainfall events. A 1D-2D linked model was used to simulate the rapid flow in creeks and channels (1D) and the subsequent overland flow across urban areas (2D). This model helped emergency services to predict flood hotspots and coordinate timely evacuations and response measures .

Agricultural Flooding in the Mekong Delta, Vietnam

The Mekong Delta, a vital agricultural region, is prone to seasonal flooding. A 1D-2D linked model was employed to understand the complex flood dynamics in the river channels (1D) and the expansive floodplains (2D). This model provided critical insights for developing flood-resistant agricultural practices and planning flood diversion schemes to protect crops .

Floodplain Management in the Thames Basin, UK

The Thames Basin is a densely populated and economically important region that frequently experiences flooding. A 1D-2D linked model was utilized to simulate river flow (1D) and floodplain inundation (2D). This model informed the development of the Thames Estuary 2100 Plan, which includes innovative flood defenses and urban planning measures to manage future flood risks .

Monsoon Flooding in Dhaka, Bangladesh

Dhaka, the capital of Bangladesh, is highly vulnerable to monsoon flooding. A 1D-2D linked model was applied to analyze the drainage network (1D) and surface water flow (2D). The model's predictions were crucial for improving the city's flood preparedness and infrastructure resilience, enabling authorities to implement targeted flood mitigation projects .


Conclusion

1D-2D linked models offer a superior alternative to pure 2D models for flood hazard management. They combine the strengths of both 1D and 2D modeling techniques, providing enhanced computational efficiency, improved accuracy, and greater flexibility. By offering detailed insights into flood behavior, these models support more effective risk assessment and management, ultimately safeguarding communities from the devastating impacts of flooding.

Embracing 1D-2D linked models in flood hazard management represents a significant step forward in our ability to predict, prepare for, and mitigate flood risks. For practitioners in the field, adopting this hybrid approach can lead to more reliable and actionable flood predictions, ensuring better protection for vulnerable areas.

Kevin Jeanes

Senior Freelance Consultant - Climate Change, Environment and Natural Resources

4 个月

Flood adaptation and mitigation these days under climate change threats needs to focus directly on historical mapping of the 'flood' - i.e. flood extent, depth and duration. Using past & recent flood maps you can assess the area & infrastructure under risk. Plus add social survey of local residents to collect validating 'past serious flood event' heights against local structures & durations of flood. Rainfall runoff models focussed on modelled river discharge are not needed, the actual flood extent in past events, and actual river stages, is empirical data which is needed to assess future risk based on past events.

Gora Chand Soren

Assistant Engineer @WBSETCL | IITKGP

4 个月

2D full RAS models are generally more efficient. However coupled models run faster as the mesh size is smaller. Anyway coupled models were easier for me . Flood hazard management should be prepared using both the models for optimum results.

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Colin McKernan, P.E., CFM

Bridge Hydraulics Lead at HDR

4 个月

In my experience, coupled 1D-2D models are not the future but rather the past. It was the approachable methodology approximately 10 years ago. We've had about 10 years now to manage flood hazard modeling with those coupled models and we struggle to find ANY models that aren't unstable and only work in the version of the model that they were developed in. That is an extremely limiting issue to communities. The list of applications and case studies is appreciated but I wonder if those clients are still satisfied with both the ease of use of the coupled models and to know if they got their best value for what was likely an expensive modeling effort.

Luis Partida

Research Scientist Numerical Surface Water Modeler/Senior Water Resources Engineer

4 个月

I slightly disagree. 1D 2D coupled models... lets say in XPSWMM can have nightmare run times. Full 2D RAS models, if set up "efficiently", will typically always perform faster than if the main river stem is a 1D reach and XS's with 2D overbanks. As far as 1D 2D coupled models being more accurate, that is entirely based on the input data and setup. If I have a 1D main river reach and a 2D overflow in the banks, the XS on the reach create tables that will interpolate between each when converging to a solution; and then have to complete a transfer over a lateral structure if it gets high enough. And what happens when water from the overbank hits the lateral structure to get into the 1D XS? It goes directly into the invert and ignores the overbanks, but of course if set up correctly this is less of a concern. All of those components require excessive experience to get it "right" and introduce "unneeded" weir calculations over laterals. In 2D there is minor interpolation based on the cell size and doesnt require structures to transfer volume. If I have a great terrain, land cover, and meteorological data set, then I prefer the optimal full 2D route. But again, EVERY scope is different.

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