The Current State of Operational Global (and continental) Scale Flood Forecasting

contributed by Rebecca Emerton, PhD Student at the University of Reading and ECMWF

After reading Chantal’s recent blog post discussing some of the limitations for international flood forecasting, and last week’s interview with Thomas Adams and Tom Pagano discussing their new book describing national and regional flood forecasting systems around the world, I thought it would be interesting to add to this dialogue with a brief overview of the current state of large-scale (global and continental) operational flood forecasting.

It has only really become possible to produce flood forecasts at the global scale in recent years, largely due to the integration of meteorological and hydrological modelling capabilities, improvements in data, satellite observations and land-surface hydrology modelling, and increased resources and computer power. Two of the key scientific and technological advances that have enabled the forecasting of floods at the continental and global scale include the significant increase in the skill of precipitation forecasts in recent years, and the move from deterministic to probabilistic (ensemble) numerical weather prediction (NWP).

Key factors

Three key factors highlight the need for large-scale, international flood forecasting systems:

  1. to provide information on floodiness (Stephens et al., 2016) across areas larger than a catchment, for example, to indicate where flooding during the rainy season will be worse than normal; information that is of high importance to humanitarian organisations (Braman et al., 2013)

  2. to provide forecasts in basins across the globe where there are currently no forecasts available, aiding disaster risk reduction and flood early warning efforts globally

  3. to support existing capabilities, for example, by using ensemble forecasting techniques to enable probabilistic flood forecasts, or at longer lead times for earlier warnings, as these can be computationally expensive to run.

At present, these forecasting systems are able to produce coarse-scale discharge forecasts covering entire continents or the globe. As previously discussed by Chantal, Thomas and Tom, despite recent advances, there are several grand challenges faced by international forecasting systems at present and moving forward, from data availability to resources and effective communication of forecasts.

At present, there are four operational continental scale flood forecasting systems, and two global scale. Below, I have given a very brief summary of each. These systems are continuously evolving, and are already proving to be key in supplementing national and local forecasting capabilities while supporting global-scale activities. Thanks to my co-authors at the centres running each of these systems, you can read more about each system, such as the components of the model and their operational uses, and the current state of large-scale flood forecasting (including the advances that have led to where we are now, the grand challenges facing the community, and future directions), here: Continental and Global Scale Flood Forecasting Sytems (Emerton et al., 2016). For anyone interested in reading further around national and regional forecasting systems and their histories, I also include a link to the “Flood Forecasting, A Global Perspective” book discussed in last week’s post.

The European Flood Awareness System (EFAS)

EFAS has been fully operational since 2012, with the aim of providing transnational, harmonised early warnings of flood events and hydrological information to national agencies, complementing local services. Four different meteorological forecasts are used as input to the Lisflood hydrological model, producing simulated ensemble hydrographs; however, these alone do not constitute a flood forecast – a decision-making element needs to be incorporated (Thielen et al., 2009). As such, historical meteorological data are run through Lisflood to calculate a 22-year time series of river flow, providing reference thresholds for minor or major flooding. EFAS sends warning emails to national authorities responsible for flood forecasting across Europe, and daily overviews are sent to the Emergency Response Coordination Centre (ERCC) of the European Commission.

European Hydrological Predictions for the Environment (E-HYPE)

H:\Review_Paper\Long Version\ehype_interface.pngE-HYPE is a multipurpose model based on open data, which is used for various applications such as water management, research experiments and flood forecasts. The E-HYPE Water in Europe Today (WET) tool compares the current hydrological situation with climatological data and past modelled events. E-HYPE currently uses a single deterministic NWP input, although ensemble forecasting is intended for future system developments. Alongside natural processes, HYPE also takes into account anthropogenic influences including irrigation and hydropower.

The BoM Flood Forecasting and Warning System

H:\Review_Paper\Long Version\bom_graphics.png

The BoM has been producing flood forecasts operationally for several decades, with the technology and systems used to produce these forecasts continually evolving. Recently, short-term continuous streamflow forecasting has been introduced, alongside event-based hydrological modelling and nowcasting using radar rainfall estimates. The BoM system uses various resolutions (each covering a different spatial scale) of their own deterministic NWP model as input to the Génie Rural á 4 Paramètres (GR4) hydrological models, and forecasters are also able to produce “What If” precipitation scenarios to force the hydrological models. For event-based forecasts, local models are used in support of the continental scale system.

The U.S. Hydrologic Ensemble Forecast Service (HEFS)

H:\Review_Paper\Long Version\hefs_screenshot_2(locationsinflood)_copy.png

The HEFS has been running experimentally at several regional River Forecast Centres (RFCs) across the U.S. since 2012, and is currently being rolled out operationally at all 13 RFCs. The HEFS aims to produce ensemble streamflow forecasts that seamlessly span lead times from less than 1 hour up to several  years, and that are spatially and temporally consistent, calibrated and verified. The HEFS takes four meteorological inputs; two NWP models, alongside the RFC forecasts and historical observations, and each RFC may use a different combination of 19 components within the Hydrologic Processor suite (which contains various hydrologic, hydraulic, reservoir and routing models). Also included in the HEFS are pre- and post-processing steps which allow both the uncertainties in the meteorological input and the hydrology to be taken into account.

The Global Flood Awareness System (GloFAS)

H:\Review_Paper\Long Version\glofas_interface.png

GloFAS (Alfieri et al., 2013) has been producing probabilistic flood forecasts for the global river network with up to 2 weeks lead time in a pre-operational environment since 2011, and can provide downstream countries with early warnings and information on upstream river conditions alongside global overviews of upcoming flood events in large river basins. GloFAS takes the surface and sub-surface runoff from the ECWMF ensemble prediction system as input to the Lisflood river routing model, with runoff from the ERA-Interim reanalysis archive also run through Lisflood, in order to compute return periods for the global river network. Unlike EFAS, GloFAS does not directly disseminate flood warnings, as each country has national procedures to follow, but anyone is able to access and analyse the forecasts for decision-making purposes and research.

The Global Flood Forecasting Information System (GLOFFIS)

H:\Review_Paper\Long Version\gloffis_vis.png

GLOFFIS is a research-oriented operational system based on Delft-FEWS (56), and similarly to several of the continental-scale systems, uses several meteorological inputs to drive two hydrological models; PCR-GLOBWB and W3RA. The idea behind this is to validate, verify and inter-compare real-time rainfall products as they become available. The first version of GLOFFIS went live in 2015, used internally at Deltares and by their customers. GLOFFIS is intended to be a research tool on predictability and interoperability first and foremost, but will be suitable for a wide range of applications once fully operational.

Further reading

Stephens E, Day JJ, Pappenberger F, Cloke H. Precipitation and floodiness. Geophys Res Lett 2015, 42(23): 10316–10323

Braman LS, van Aalst MK, Mason SJ, Suarez P, Ait-Chellouche Y, Tall A. Climate forecasts in disaster management: Red Cross flood operations in West Africa, 2008. Disasters 2013, 37:144–164

Thielen J, Bartholmes J, Ramos MH, de Roo A. The European Flood Alert System – part 1: concept and development. Hydrol Earth Syst Sci 2009, 13:125–140

Alfieri L, Burek P, Dutra E, Krzeminski B, Muraro D,Thielen J, Pappenberger F. GloFAS – global ensemble streamflow forecasting and flood early warning. Hydrol Earth Syst Sci 2013, 17:1161–1175

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4 Responses to The Current State of Operational Global (and continental) Scale Flood Forecasting

  1. Very interesting, this is clearly the way to go for flood forecasting!

    Note that In Canada, Environment and Climate Change Canada (ECCC) operates a 3.5-day, 1-km deterministic regional-scale hydrological prediction system for the Great Lakes and St. Lawrence River. Including the US portion of the domain, the watershed area is about as large as France and Germany combined. The system also includes a 3-D hydrodynamic model to resolve the Great Lakes themselves and a 2-D hydrodynamic model of the St. Lawrence River.

    Outputs are available through a web-mapping service, and can be viewed, for example, using GLoFAS from ECMWF or ADAGUC from KNMI. Here is a link showing two animations of streamflow forecasts and surface currents using ADAGUC:

    1) For the whole domain:

    http://meteocentre.com/plus/?srs=EPSG%3A3857&bbox=-10503249.97320635,4740689.659551858,-7700731.606742246,7009572.704572066&service=http%3A%2F%2Fcollaboration.cmc.ec.gc.ca%2Frpn-wms%2F%3FLANG%3DE,http%3A%2F%2Fcollaboration.cmc.ec.gc.ca%2Frpn-wms%2F%3FLANG%253DE&layer=WCPS-GLS.OCE-LIM_UU2W%24image%2Fpng%24true%24ARROW%241%240,WCPS-GLS.HYDROL.FORECASTS_DISC%24image%2Fpng%24true%24DISC_FULL%241%241&selected=0&baselayers=streetmap$world_line

    2) A zoom on the Detroit/Windsor region, using a different color palette (same underlying forecast):

    http://meteocentre.com/plus/?srs=EPSG%3A3857&bbox=-9480673.989073092,5058615.86510339,-8992077.037025074,5454177.711768098&service=http%3A%2F%2Fcollaboration.cmc.ec.gc.ca%2Frpn-wms%2F%3FLANG%253DE&layer=WCPS-GLS.OCE-LIM_UU2W%24image%2Fpng%24true%24ARROW%241%240,WCPS-GLS.HYDROL.FORECASTS_DISC%24image%2Fpng%24true%24DISC_WAVE%241%240&selected=0&baselayers=streetmap$world_line

    Just click the “play” button” to start the animations. Note that although the model is running operationally at ECCC, this implementation of the ADAGUC viewer is provided on a best effort basis by the Université du Québec à Montréal (UQAM), please be understanding if it does not work for you.

    ECCC is working on extending the domain to cover all of southern Canada. ECCC also provides 15-day ensemble forecasts of surface runoff for all of Canada on its web site, but internally the product is available for the whole globe, on a 0.25 degree grid.

    • Rebecca Emerton says:

      Hi Vincent, thank you for your reply and for adding this information about the system at ECCC – I was not aware of this one and it is great to hear of the developments in larger-scale ensemble forecasts for this region; I will certainly take a look at these forecasts on the ECCC web site and via the WMS!

  2. James says:

    In the US, the National Weather Service’s Office of Water Prediction (formerly OHD) just rolled “The National Water Model” in to operations on the 16th of August (a week after your post).

    A brief summary: The model is currently intended for the continental US but models sections of Canada, Mexico, and Cuba. The channel network has 2.6million reaches (NHD+v2.1), the LSM is NoahMP running at 1km, and there is a subgrid overland routing and subsurface saturated routing at 250m. There is an analysis/assimilation cycle and 3 NWP-driven forecast ranges. Short range is HRRR-based out to 15 hours, every hour. Medium range is GFS-driven, daily out to 10 days. Long range is CFS-driven, 4 members every 6 hours out to 30 days.

    Here are some links, from least to most technical

    Press release: http://www.noaa.gov/media-release/noaa-launches-america-s-first-national-water-forecast-model

    Overview of NWM: http://water.noaa.gov/about/nwm

    Technical Implementation Notice: http://www.nws.noaa.gov/om/notification/tin16-30natl_water_model.htm

  3. Rebecca Emerton says:

    Hi James, thank you for bringing this new model to my attention – a shame I missed this for the blog post, so thank you for including some information here! This is a very interesting set-up with the multiple forecast ranges at a high resolution compared to the other models discussed in the post; I certainly look forward to reading more about this model!

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