globalchange  > 气候变化事实与影响
DOI: doi:10.1038/nclimate2742
论文题名:
Usefulness and limitations of global flood risk models
作者: Philip J. Ward
刊名: Nature Climate Change
ISSN: 1758-816X
EISSN: 1758-6936
出版年: 2015-07-24
卷: Volume:5, 页码:Pages:712;715 (2015)
语种: 英语
英文关键词: Hydrology ; Environmental sciences ; Water resources ; Projection and prediction
英文摘要:

Global flood risk models were developed to identify risk hotspots in a world with increasing flood occurrence. Here we assess the ability and limitations of the current models and suggest what is needed moving forward.

Global flood risk models (GFRMs) are now a reality1, 2, 3, 4, 5, 6, 7. More and more, these 'quick and not so dirty' methods8 are being put to use by an increasing range of practitioners and decision-makers. The adoption of the Sendai Framework for Disaster Risk Reduction9 and the Warsaw International Mechanism for Loss and Damage Associated with Climate Change Impacts10 have made these efforts even more essential.

However, GFRMs have their limits compared with local-scale models11, and there is often a mismatch between their actual ability and the envisaged use by practitioners. Modellers and users need to critically assess this discrepancy. We provide perspectives drawing from practical applications of global river flood risk models (Table 1), demonstrating the accomplishments in these examples, as well as limitations and gaps between user 'wish lists' and model capabilities. We present a research agenda to address these issues and reduce the gaps.

Table 1: Links to models, tools, and programmes discussed in the text.

The global assessment reports (GAR)4 of the United Nations Office for Disaster Risk Reduction provide a high-level platform for distributing global natural hazard risk data, including floods, which has proved instrumental in advocating for disaster risk management (DRM) internationally. Risk is framed as a 'contingent liability'; if a country allows future risks to accumulate, it effectively undermines its own potential for future socioeconomic development. This has paved the way for a more quantitative approach in the Sendai framework compared with the previous Hyogo Framework for Action, setting quantitative risk-reduction targets that are now being developed into measurable indicators.

GFRMs have been applied by the World Bank and the Global Facility for Disaster Reduction and Recovery to inform national-level DRM. Following Nigeria's devastating floods in 2012, a post-disaster needs assessment recommended strengthening flood resilience. In response, the World Bank Africa Disaster Risk Management team began developing a National Flood Risk Management Implementation Plan. At the time, little local or national information was available to assess flood risk. Within weeks, the GLOFRIS model5, 6 (Global Flood Risk with IMAGE Scenarios) was used to provide flood risk maps per state. These were used in dialogues to engage stakeholders and identify risk hotspots requiring further localized research. Building on this success, a first-cut state-level flood risk assessment was commissioned for World Bank's Europe and Central Asia region, including climate and socioeconomic projections. These rapid assessments in data-scarce countries have been useful in internal World Bank Group discussions and will be used in the near future to inform discussions with governments in the region.

With advances in numerical algorithms12, new global datasets13, and high-performance computing, it is now possible to develop global flood hazard models at 100 m resolution that solve hydrodynamic equations. An example is the SSBN-flow model14, which has been used for national flood hazard mapping in Belize as part of the World Bank Caribbean Risk Information Programme. The Government of Belize will use the nationally consistent, indicative flood hazard maps to support decision-making in spatial and infrastructure planning, particularly for housing and roads, from national to enumeration area scales. This approach has considerably enhanced the quality of flood information, which was previously unavailable. Implementation challenges included model validation against limited local data in Belize, and managing user expectations on model capabilities. Example data from the SSBN-flow model for Africa can be found in Fig. 1.

Figure 1: Example hazard data from a global flood model, overlaid on impervious surface area (ISA) data27 as an indicator of exposure.
Example hazard data from a global flood model, overlaid on impervious surface area (ISA) data as an indicator of exposure.

The hazard data shown here are from the SSBN global flood model14, and show 1-in-100-year maximum flood depth for: a, all of Africa; b, River Niger at Onitsha, Nigeria; and c, Blue Nile at Omdurman, Sudan.

Of course, GFRMs are no panacea. A question regularly posed by users is what the exact risk is for a particular community, street, or asset. Such questions highlight the apparent mismatch between the resolution and accuracy of GFRMs and the detail of information required for local-level decisions. The accuracy of flood hazard maps is dependent on the quality of the elevation data (digital elevation models; DEMs) used. Although a near-global DEM of 30 m resolution is now available18, 19, flood hazard map accuracy at such scales remains limited due to a number of factors, including: accuracy of boundary conditions used to force inundation models (for example, meteorological data)5; limitations in knowledge of river geomorphology (for example, river profiles and roughness); and the accuracy of DEMs themselves20. To estimate risk at such detailed scales, local data on exposure (how many people, buildings, and other elements are located in harm's way) and vulnerability (how susceptible are those exposed elements to flooding) are also required. Obtaining detailed information on exposure and vulnerability at the global scale remains an open challenge.

While GFRMs are used to assess the effectiveness of DRM strategies at the large scale, the granularity of the input data means that they cannot be used to design individual DRM measures. For example, while we can assess damages avoided by protecting a country against a 100-year flood, we cannot use GFRMs to design the actual measures needed to achieve this. In the example of dykes, questions regarding location, height, material, and so forth, cannot be answered using GFRMs. These limitations must be clearly communicated to users at all stages of engagement, to avoid mismatches in expectations down the line. A key challenge is the lack of data on flood management strategies already in place. Flood management has already played a strong role in reducing vulnerability to flooding21; ignoring this leads to gross overestimates of risk5.

In addition, emergency responders require flood risk information in terms of the potential impacts of a flood event, which is currently not contained in global flood forecasting and monitoring systems. At present, most of these systems only provide physical flood thresholds, based on statistical analyses of predicted riverflow, since detailed global flood hazard modelling in near real-time remains a daunting task.

A priority for increasing GFRM accuracy is an improved representation of fundamental physical and socioeconomic processes leading to flood impacts. For hazard modelling, we need better elevation data20. While the recently released 30 m DEM19 has improved horizontal resolution substantially, it did not improve the vertical accuracy required to improve global inundation models. An exciting commercial initiative towards such an improvement is WorldDEM, which is to feature a large increase in vertical accuracy. Efforts have been undertaken to yield river-width data at the global scale13, but more data are needed on other key geomorphological aspects, not to mention the presence of anthropogenic features in hydraulic systems, such as dykes and levees.

But without profoundly improved representations of exposure and vulnerability, gains from improved hazard modelling will not filter through to improved risk estimates. At present, GFRMs use simple aggregated land-use data to represent exposure, such as 'urban area' per cell, and vulnerability is commonly represented by a handful of depth-damage functions. These assumptions ignore huge spatial heterogeneities in exposure and vulnerability22. An exciting initiative that could revolutionize GFRMs is OpenStreetMap (OSM), a global crowdsourced database of buildings and infrastructure. OSM is being used to support local DRM worldwide23. A challenge for the global risk modelling community is to find smart ways to harness this wealth of object-based exposure data for GFRMs.

In many of the world's most 'risky' places, such as rapidly urbanizing deltas, flood hazards are the result of the interaction of river discharge and coastal sea levels. We therefore need to move towards an integration of river and coastal flood risk modelling to accurately assess risk in these places. The improvements described above would help with this, but it would also require developing dynamical global tide and storm surge models, and linking these with river flood models. Further gains in granularity, accuracy, and model speed could be made by nesting local flood models within global models. Such nesting has a long tradition in global climate modelling24, and could offer GFRMs the advantage of gaining more detail in areas where it is required.

Urgent efforts are required to develop databases showing current flood management worldwide. A database of flood protection standards per country is expected shortly, providing a valuable first step. Moving forward, the community requires information on which specific measures are taken and where, in terms of not only structural measures, but also non-structural measures such as flood zoning, building codes, and insurance. We could learn from crowdsourcing successes in other fields, such as OSM, by using such platforms to develop crowdsourced databases on the location and height of protection measures such as dykes and levees. Such a database could play an important role in monitoring DRM and climate change adaptation efforts.

Global-scale flood forecasting and monitoring systems need to go beyond the provision of solely information on exceedance above physical flood thresholds. Emergency responders require information on forecasted flood impacts, and should be able to link their action thresholds to global-scale flood forecasting and monitoring systems. Connecting the offline global flood risk information from GFRMs to global flood forecasting and monitoring systems is a key to further increasing the usability of both of these model families.

The effectiveness of risk information in supporting DRM is largely contingent on how the information is communicated and its timely availability. When a disaster occurs, information is required immediately — there is no time for lengthy periods to commission new studies, carry out new simulations, analyse and present results, and so forth. A range of tools has recently been developed to communicate risk in a clear and effective way. One example is InaSAFE, an open-source tool for impact assessment, now used extensively to support decision-making at national and sub-national levels in Indonesia and elsewhere. Successes like InaSAFE and the Aqueduct Global Flood Analyzer emphasize the demand for translating complex flood risk data into interactive and actionable information. While a first push in this direction is being made, further developments are required.

Not only should information be actionable, its (deep) uncertainties should be estimated and transparently communicated. At present, there is clear frustration regarding the lack of guidance from modellers on the reliability and uncertainty contained in model results. A better representation of uncertainty may lead to better decision-making25. Techniques to communicate and visualize uncertainty in relation to decision-making already exist, such as adaptation pathways25, but such novel techniques still need to be made fit for use with GFRM outputs.

Addressing this research agenda is a daunting task for any single organization. It requires interdisciplinary research, close collaboration with user communities, and grounding in a wider context of DRM and climate change adaptation. Launched in 2014, the Global Flood Partnership provides a platform for organizations involved in global flood risk, early warning, and observation to collectively identify and address challenges26. As a bottom-up, voluntary partnership, it allows direct knowledge transfer from centres of excellence in global flood risk modelling to users, including hydrological and emergency management authorities, humanitarian response organizations, international development banks, and the private sector. Harnessing the knowledge and drive of this network should help us push towards a new generation of actionable GFRMs for contributing to real-world DRM and climate change adaptation.

  1. Dilley, M. et al. Natural Disaster Hotspots. A Global Risk Analysis (The World Bank, 2005).
  2. Hallegatte, S., Green, C., Nicholls, R. J. & Corfee-Morlot, J. Nature Clim. Change 3, 802806 (2013).
  3. Hirabayashi, Y. et al. Nature Clim. Change 3, 816821 (2013).
  4. UNISDR Global Assessment Report on Disaster Risk Reduction. Making Development Sustainable: The Future of Disaster Risk Management (United Nations International Strategy for Disaster Reduction Secretariat, 2015).
  5. Ward, P. J. et al. Environ. Res. Lett. 8, 044019 (2013).
  6. Winsemius, H. C., Van Beek, R., Jongman, B., Ward, P. J. & Bouwman, A. Hydrol. Earth Syst. Sci. 17, 18711892 (2013).
  7. Ward, P. J. et al. Proc. Natl Acad. Sci. USA 111, 1565915664 (2014).
  8. Understanding Risk: Producing Actionable Information (World Bank, 2015).
  9. Sendai Framework for Disaster Risk Reduction 2015–2030 A/CONF.224/L.2 (United Nations, 2015).
  10. Decision2/CP.19 Warsaw International Mechanism for Loss and Damage Associated with Climate Change Impacts (UNFCCC, 2013).
  11. Jonkman, S. N. Nature Clim. Change 3, 1004 (2013).
  12. Bates, P. D., Horritt, M. S. & Fewtrell, T. J. J. Hydro. 387, 3345 (2010).
  13. Yamazaki, D. et al. Water Resour. Res. 50, 34673480 (2014).
  14. Bates, P. D., Smith, A., Sampson, C., Alfielri, L. & Neal, J. C. in Am. Geophys. Union Fall Meet. Abstract H33M-03 (AGU, 2014)
  15. Mechler, R. et al. Nature Clim. Change 4, 235237 (2014). URL:
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/4644
Appears in Collections:气候变化事实与影响
科学计划与规划
气候变化与战略

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Philip J. Ward. Usefulness and limitations of global flood risk models[J]. Nature Climate Change,2015-07-24,Volume:5:Pages:712;715 (2015).
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