Using globally available soil moisture indicators for flood modelling in Mediterranean catchments

Floods are one of the most dangerous natural hazards in Mediterranean regions. Flood forecasting tools and early warning systems can be very beneficial to reducing flood risk. Event-based rainfall–runoff models are frequently employed for operational flood forecasting purposes because of their simplicity and the reduced number of parameters involved with respect to continuous models. However, the advantages related to the reduced parameterization oppose to the need of a correct initialization of the model, especially in areas characterized by strong climate seasonality. In this case, the use of continuous models could be desirable but it is very problematic in poorly gauged areas where continuous rainfall and temperature data are not available. This paper introduces a Simplified Continuous Rainfall–Runoff model (SCRRM), which uses globally available soil moisture retrievals to identify the initial wetness condition of the catchment, and, only event rainfall data to simulate discharge hydrographs. The model calibration involves only three parameters. For soil moisture, besides in situ data, satellite products from the Advanced SCATterometer (ASCAT) and the Advanced Microwave Scanning Radiometer for Earth observation (AMSR-E) sensors were employed. Additionally, the ERA-Land reanalysis soil moisture product of the European Centre for Medium-Range Weather Forecasting (ECMWF) was used. SCRRM was tested in the small catchment of the Rafina River, 109 km 2 , located in the eastern Attica region, Greece. Specifically, sixteen recorded rainfall–runoff events were simulated by considering the different indicators for the estimation of the initial soil moisture conditions from in situ, satellite and reanalysis data. By comparing the performance of the different soil moisture products, we conclude that: (i) all global indicators allow for a fairly good reproduction of the selected flood events, providing much better results than those obtained from setting constant initial conditions; (ii) the use of all the indicators yields similar results when compared with a standard continuous simulation approach that, however, is more data demanding; (iii) SCRRM is robust since it shows good performances in validation for a significant flood event that occurred on February 2013 (after calibrating the model for small to medium flood events). Due to the wide diffusion of globally available soil moisture retrievals and the limited number of parameters used, the proposed modelling approach is very suitable for runoff prediction in poorly gauged areas.

[1]  V. Singh,et al.  Assimilation of Observed Soil Moisture Data in Storm Rainfall-Runoff Modeling , 2009 .

[2]  Florian Pappenberger,et al.  ERA-Interim/Land: a global land water resources dataset , 2013 .

[3]  A. Robock,et al.  The International Soil Moisture Network: a data hosting facility for global in situ soil moisture measurements , 2011 .

[4]  Luca Brocca,et al.  Estimation of antecedent wetness conditions for flood modelling in northern Morocco , 2012 .

[5]  Christophe Bouvier,et al.  Flood modelling with a distributed event-based parsimonious rainfall-runoff model: case of the karstic Lez river catchment , 2012 .

[6]  Marco Borga,et al.  The influence of soil moisture on threshold runoff generation processes in an alpine headwater catchment , 2010 .

[7]  Vazken Andréassian,et al.  How crucial is it to account for the antecedent moisture conditions in flood forecasting? Comparison of event-based and continuous approaches on 178 catchments , 2009 .

[8]  P. Ayral,et al.  Impact of rainfall spatial distribution on rainfall-runoff modelling efficiency and initial soil moisture conditions estimation , 2011 .

[9]  J. Eitzinger,et al.  The ASCAT Soil Moisture Product: A Review of its Specifications, Validation Results, and Emerging Applications , 2013 .

[10]  Keith Beven,et al.  A manifesto for the equifinality thesis , 2006 .

[11]  Richard de Jeu,et al.  Improving Curve Number Based Storm Runoff Estimates Using Soil Moisture Proxies , 2009, IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing.

[12]  W. Wagner,et al.  A new method for rainfall estimation through soil moisture observations , 2013 .

[13]  Luca Brocca,et al.  Distributed rainfall‐runoff modelling for flood frequency estimation and flood forecasting , 2011 .

[14]  Klaus Scipal,et al.  Validation of ERS scatterometer‐derived soil moisture data in the central part of the Duero Basin, Spain , 2005 .

[15]  Luca Brocca,et al.  On the potential of MetOp ASCAT‐derived soil wetness indices as a new aperture for hydrological monitoring and prediction: a field evaluation over Luxembourg , 2012 .

[16]  Sandrine Anquetin,et al.  The benefit of high-resolution operational weather forecasts for flash flood warning , 2008 .

[17]  Nam-won Kim,et al.  Temporally weighted average curve number method for daily runoff simulation , 2008 .

[18]  Luca Brocca,et al.  On the estimation of antecedent wetness conditions in rainfall–runoff modelling , 2008 .

[19]  W. Wagner,et al.  Soil moisture estimation through ASCAT and AMSR-E sensors: An intercomparison and validation study across Europe , 2011 .

[20]  W. Wagner,et al.  Initial soil moisture retrievals from the METOP‐A Advanced Scatterometer (ASCAT) , 2007 .

[21]  Patrick Willems,et al.  Increasing river flood preparedness by real-time warning based on wetness state conditions , 2013 .

[22]  E. Todini,et al.  2 APPLICATION OF THE TOPKAPI MODEL WITHIN THE DMIP 2 PROJECT , 2009 .

[23]  José I. Barredo,et al.  Major flood disasters in Europe: 1950–2005 , 2007 .

[24]  Yves Tramblay,et al.  Assessment of initial soil moisture conditions for event-based rainfall–runoff modelling , 2010 .

[25]  Vijay P. Singh,et al.  Assessment of flooding in urbanized ungauged basins: a case study in the Upper Tiber area, Italy , 2005 .

[26]  Erwin Zehe,et al.  Predicting event response in a nested catchment with generalized linear models and a distributed watershed model , 2012 .

[27]  J. Thepaut,et al.  The ERA‐Interim reanalysis: configuration and performance of the data assimilation system , 2011 .

[28]  C. T. Wang,et al.  A representation of an instantaneous unit hydrograph from geomorphology , 1980 .

[29]  W. Wagner,et al.  A Method for Estimating Soil Moisture from ERS Scatterometer and Soil Data , 1999 .

[30]  Y. Kerr,et al.  Evaluation of remotely sensed and modelled soil moisture products using global ground-based in situ observations , 2012 .

[31]  Yann Kerr,et al.  The SMOS Mission: New Tool for Monitoring Key Elements ofthe Global Water Cycle , 2010, Proceedings of the IEEE.

[32]  V. Jacobshagen Geologie von Griechenland , 1986 .

[33]  Vijay P. Singh,et al.  Lag prediction in ungauged basins: an investigation through actual data of the upper Tiber River valley , 2002 .

[34]  L. Isaksen,et al.  A simplified Extended Kalman Filter for the global operational soil moisture analysis at ECMWF , 2013 .

[35]  Luca Brocca,et al.  Design soil moisture estimation by comparing continuous and storm‐based rainfall‐runoff modeling , 2011 .

[36]  C. Makropoulos,et al.  THE IMPACT OF FOREST FIRES ON THE VULNERABILITY OF PERI-URBAN CATCHMENTS TO FLOOD EVENTS (THE CASE OF THE EASTERN ATTICA REGION) , 2012 .

[37]  Luca Brocca,et al.  What perspective in remote sensing of soil moisture for hydrological applications by coarse-resolution sensors , 2011, Remote Sensing.

[38]  Marco Mancini,et al.  Parsimonious modeling of vegetation dynamics for ecohydrologic studies of water‐limited ecosystems , 2005 .

[39]  Ezio Todini,et al.  History and perspectives of hydrological catchment modelling , 2011 .

[40]  W. Wagner,et al.  Improving runoff prediction through the assimilation of the ASCAT soil moisture product , 2010 .

[41]  Federico Garavaglia,et al.  The SCHADEX method: A semi-continuous rainfall–runoff simulation for extreme flood estimation , 2013 .

[42]  G. Aronica,et al.  A Regional Methodology for Deriving Flood Frequency Curves (FFC) in Partially Gauged Catchments with Uncertain Knowledge of Soil Moisture Conditions , 2004 .

[43]  Luca Brocca,et al.  Antecedent Wetness Conditions based on ERS scatterometer data in support to rainfall-runoff modeling , 2009 .

[44]  Jeffrey P. Walker,et al.  A methodology for surface soil moisture and vegetation optical depth retrieval using the microwave polarization difference index , 2001, IEEE Trans. Geosci. Remote. Sens..

[45]  D. Viviroli,et al.  Continuous simulation for flood estimation in ungauged mesoscale catchments of Switzerland - Part II: Parameter regionalisation and flood estimation results , 2009 .

[46]  R. Jeu,et al.  Multisensor historical climatology of satellite‐derived global land surface moisture , 2008 .