Part1
Operational Hydrology
Chapter 1
Developing the Flood Alert Map 1
This document consists of experience feedback concerning the bad weather conditions of August 11 and 12, 2008, which led to the production of orange level maps and yellow level maps and which were the subject of category-orange weather alert maps and category-yellow flood alert maps. The documentâs aim is to present a summary of the framework constituted by the various numerical tools used by forecasters from the SCHAPI-SPC network and to illustrate their usage in the form of a simple example.
1.1. Flood alert
The SCHAPI (French National Hydrometeorological and Flood Forecasting Center), along with the 22 local flood forecasting services, has published a flood alert map at least twice a day since December 2005. This map presents the hydrological risk across the 20,000 kilometers that make up the regulatory network monitored by the French government. In July 2007, MĂ©tĂ©o-France and the SCHAPI decided to produce a single ârain and floodingâ pictogram, combining MĂ©tĂ©o-Franceâs âheavy precipitationâ risk and the SCHAPI-SPC networkâs âfloodâ risk. This required work to be carried out repeatedly by MĂ©tĂ©o-France weather forecasters and the SCHAPI-SPC networkâs hydrologist forecasters.
A single portal offers access to both alert maps (http://www.meteofrance.com/vigilance/index.jsp).
Here we will describe the methods and tools made use of and employed to produce the flood alert map. We have taken as an example the relatively minor event of August 11-12, 2008, placing the emphasis more on the methodology used than on describing the event itself. The presentation is broken down into two stages, which illustrate the forecaster approach:
â the date is August 11: MĂ©tĂ©o-France forecasts heavy rain for the following day. Flood forecasters then estimate the risk for their watercourses over a timescale of 24 hours, and publish the flood alert map;
â the following day, August 12, we use on the field measurements to draw up an assessment of yesterdayâs alert.
Let us recall to begin with that the alert consists of qualifying the risk for a period to come (in this instance, 24 hours), in order to enable civil security members and the general public to take the precautions needed in order to be sheltered from risk. On the technical level, risk anticipation is based on exploiting the weather predictions in an essentially qualitative manner. As soon as there is a rainfall, it is recorded by the ground network of rain gauges and radars which feed into the hydrological models, which in turn provide forecasts of flow rates in the watercourses. Flood forecasters make use of a variety of information sources in order to develop their alert map.
| Analysis of the hydrometeorological situation from the previous day to present day | Rainfall Soil condition Floods in progress | Storm drainage systems + rain rate (ANTILOPE) Soil moisture map (SIM). Hydrograph measured + hydrological forecasts |
| Weather forecasts from the present day to the following day Hydrological forecasts (several hours) | Forecast rain rate Forecast flow-rates | Results of meteorological models: ARPEGE, ALADIN, ECMWF Hydrological models (here: ALTHAIR) |
| Hydrometeorological risk estimation for the following day | Production of the flood alert map | Rain flow charts |
The event of August 11â12 brought about contributions from the Grand Delta and RhĂŽne Amont SaĂŽne SPCs (flood forecasting services), along with the SCHAPI, for the alert maps issued on August 11 at 4 p.m. and August 12 at 10 a.m.
1.2. Developing flood alert maps for August 11â12, 2008
1.2.1. Analysis of the hydrometeorological situation
The meteorological situation on August 11â12, 2008 is characterized by a succession of several storm disturbances passing over France.
On August 11, 2008 the hydrological situation is calm, with the last significant floods on the regulatory network dating back over a month. Figure 1.1 shows that in the last 24 hours, no rain has dampened the soil on the Cévennes and RhÎne basins.
A first rain storm disturbance (named âTâ) rapidly crosses France from the West to the East on the 11th, giving accumulations that remain low, less than 10 mm for the most part.
However, MĂ©tĂ©o-France forecasts the rapid arrival of a new disturbance (named âUâ) from the West in the afternoon of the 11th, which is to cross France the following night, stopping at the Eastern end of the country on the 12th, and merging with the first disturbance.
Satellite and radar images available to forecasters (Figure 1.2) enable them to locate these different elements and monitor their development with respect to time.
1.2.2. Weather forecasts
Météo-France provides the SCHAPI-SPC network with several types of meteorological information:
(1) precipitation reports (PRs) indicating the accumulations forecast over a 24- hour period, issued by the interregional departments of Météo-France at a rate of two a day, or more if needed. The reports are issued on the scale of zones generally corresponding to river basins which are relatively large in size (Figure 1.3).
SCHAPI forecasters are sent other meteorological information, issued directly from the Météo-France numerical forecast models, ARPEGE and ALADIN (Figure 1.4);
(2) precipitation forecast maps over 24 hours by âSymposiumâ zone. These zones are smaller than the PR zones, but correspond to zones that are climatically homogeneous and not to hydrological basins (Figure 1.5);
(3) a ârisk indicator-typeâ product is also available, using what is known as the analog method. This method researches past meteorological situations closest to the forecast situation, using them to determine the probability of the rainfall thresholds being exceeded on various stations located in the CĂ©vennes and in the Alps.
1.2.2.1. Results of the numerical models
As an example of the products available to the SCHAPI, presented below are four meteorological fields taken from the Météo-France ARPEGE forecast model, which were available on the morning of August 11 and valid for August 12 at 12 p.m. UTC.
The unprocessed forecasts presented above (Figure 1.5) have not been evaluated by Météo-France. Nevertheless, they offer flood forecasters an understanding of the overall meteorological situation, highlighting the flow type (top left-hand map); the activity, position and displacement velocity of the fronts (top right-hand map); the storm potential (bottom left); the rainfall forecast by the ARPEGE model over a given time period (here: six hours). These fields can be animated for forecast timescales covering 0 to 96 hours.
The âunprocessedâ outputs of the numerical models available to the SCHAPI enable accumulations to be produced for periods of the userâs choice. Whilst these values ar...