Implementation and performance analysis of a high resolution coupled numerical weather and river runoff prediction model system for an Alpine catchment

被引:18
作者
Smiatek, Gerhard [1 ]
Kunstmann, Harald [1 ,2 ]
Werhahn, Johannes [1 ]
机构
[1] KIT, Inst Meteorol & Climate Res IMK IFU, D-82467 Garmisch Partenkirchen, Germany
[2] Univ Augsburg, Inst Geog, D-86135 Augsburg, Germany
关键词
Perl; POE; Hydrological model; NWP; SOAP; WEB services; MM5; WASIM-ETH; HYDROLOGICAL MODELS; PRECIPITATION; SIMULATION; FORECASTS; ENSEMBLES; RAINFALL;
D O I
10.1016/j.envsoft.2012.06.001
中图分类号
TP39 [计算机的应用];
学科分类号
081203 ; 0835 ;
摘要
This study describes the implementation of a one way coupled high resolution numerical weather and river runoff forecasting system within the Perl Object Environment (POE) framework and presents its application and performance analysis for the Alpine catchment of the Ammer River located in southern Germany. The simulation system employs the hydrological water balance model WaSiM-ETH run at 100 m x 100 m grid resolution one way coupled with the numerical weather prediction model (NWP) MM5 driven at 3.5 km grid cell resolution. The state and event driven forecasting system implements the input data download, input data provision via SOAP based WEB service and the run of the hydrology model with observed and with predicted NWP meteorology fields. It applies a lagged ensemble prediction system (EPS) taking into account combination of recent and previous NWP forecasts. The simulation system has been setup and designed for flood forecasting in the alpine environment. It is run operationally as well as in extended time slice experiments for all episodes with highest observed runoff in the period 01.10.2005-30.09.2010. The system application demonstrates the great potential of the POE based system in networking, distributed computing as well in the setup of various experiments. The river runoff simulation results show high correlation with observed runoff when driven with precipitation interpolated from station observations. The performance of the forecast shows limitations resulting from deficient timing and amount of the predicted rainfall in the complex mountainous area. Forecast skills were improved after application of a lagged ensemble prediction system. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:231 / 243
页数:13
相关论文
共 51 条
  • [1] An operational hydrological ensemble prediction system for the city of Zurich (Switzerland): skill, case studies and scenarios
    Addor, N.
    Jaun, S.
    Fundel, F.
    Zappa, M.
    [J]. HYDROLOGY AND EARTH SYSTEM SCIENCES, 2011, 15 (07) : 2327 - 2347
  • [2] An open software environment for hydrological model assessment and development
    Andrews, F. T.
    Croke, B. F. W.
    Jakeman, A. J.
    [J]. ENVIRONMENTAL MODELLING & SOFTWARE, 2011, 26 (10) : 1171 - 1185
  • [3] [Anonymous], 2011, INT GEOPHYS, DOI DOI 10.1016/B978-0-12-385022-5.00008-7
  • [4] Hydrological and meteorological aspects of floods in the Alps: an overview
    Bacchi, B
    Ranzi, R
    [J]. HYDROLOGY AND EARTH SYSTEM SCIENCES, 2003, 7 (06) : 784 - 798
  • [5] Disaggregation of rainfall for one-way coupling of atmospheric and hydrological models in regions of complex terrain
    Bindlish, R
    Barros, AP
    [J]. GLOBAL AND PLANETARY CHANGE, 2000, 25 (1-2) : 111 - 132
  • [6] Towards multi-scale integrated hydrological models using the LIQUID® framework. Overview of the concepts and first application examples
    Branger, F.
    Braud, I.
    Debionne, S.
    Viallet, P.
    Dehotin, J.
    Henine, H.
    Nedelec, Y.
    Anquetin, S.
    [J]. ENVIRONMENTAL MODELLING & SOFTWARE, 2010, 25 (12) : 1672 - 1681
  • [7] A Nonparametric Postprocessor for Bias Correction of Hydrometeorological and Hydrologic Ensemble Forecasts
    Brown, James D.
    Seo, Dong-Jun
    [J]. JOURNAL OF HYDROMETEOROLOGY, 2010, 11 (03) : 642 - 665
  • [8] Caputo R., 2003, POE PERL OBJECT ENV
  • [9] Castronova A.M., 2012, ENV MODELLING SOFTWA
  • [10] Chen F, 2001, MON WEATHER REV, V129, P569, DOI 10.1175/1520-0493(2001)129<0569:CAALSH>2.0.CO