Evaluation of two atmospheric models for wind-wave modelling in the NW Mediterranean

被引:64
作者
Bolanos-Sanchez, R. [1 ]
Sanchez-Arcilla, A. [1 ]
Cateura, J. [1 ]
机构
[1] Catalonia Univ Technol, Lab Maritime Engn, Barcelona 08034, Spain
关键词
Mediterranean Sea; wave storms; wind modelling; wave modelling; QuikSCAT; WAM; SWAN;
D O I
10.1016/j.jmarsys.2005.09.014
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The NW Mediterranean experiences, as illustrated by the last decade, strong and rapidly varying storms with severe waves and winds. This has motivated a continuous validation of models and the efforts to improve wave and wind predictions. In this paper we use two atmospherics models, MASS (from SMC-Meteorological Office of Catalunya) and ARPEGE (from Meteo-France), to force two third generation wave models: WAM and SWAN. The evaluation and comparison has been carried out for two severe storms registered in November 2001 and March-April 2002. The ARPEGE and MASS models predicted higher 10 m wind speeds than coastal meteorological stations, a fact attributed to local land influences. Regarding the 10 m wind direction, models do not present large differences, although considerable deviations from recorded data were found during some dates. ARPEGE presents less scatter and lower errors than MASS when compared with QuikSCAT data. The 10m wind fields from both atmospheric models were used to force the two selected wave models and analyse the errors and sensitivities when predicting severe wave storms. The wave model simulations show some interesting results; during the storm, the spatial wave pattern using ARPEGE showed a higher maximum, although the values of significant wave height at the buoys were lower than the ones forced by MASS (with both WAM and SWAN). The SWAN simulations show a better agreement in predicting the growing and waning of the storm peaks. The prediction of mean period was improved when using the ARPEGE wind field. However the underestimation by SWAN due to the large energy at high frequencies was evident. Validation of spectral shape predictions showed that it still has considerable error when predicting the full frequency spectra. The storms showed bimodal spectral features which were not always reproduced by wave models and are likely to be responsible for part of the discrepancies. (c) 2006 Elsevier B.V. All rights reserved.
引用
收藏
页码:336 / 353
页数:18
相关论文
共 67 条
[1]  
ANTHES RA, 1977, MON WEATHER REV, V105, P270, DOI 10.1175/1520-0493(1977)105<0270:ACPSUA>2.0.CO
[2]  
2
[3]   Determination of high-frequency wind variability from observations and application to North Atlantic wave modeling [J].
Bauer, E ;
Weisse, R .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2000, 105 (C11) :26179-26190
[4]  
BAUER E, 1997, P 3 ERS S FLOR
[5]  
BOLANOSSANCHEZ R, 2003, P 22 INT C OFFSH MEC
[6]  
CARDONE VJ, 1995, GLOBAL ATMOS OCEAN S, V3, P107
[7]   Recent mass-movement processes on the Ebro continental slope (NW Mediterranean) [J].
Casas, D ;
Ercilla, G ;
Baraza, J ;
Alonso, B ;
Maldonado, A .
MARINE AND PETROLEUM GEOLOGY, 2003, 20 (05) :445-457
[8]   Accuracy of the modelled wind and wave fields in enclosed seas [J].
Cavaleri, L ;
Bertotti, L .
TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 2004, 56 (02) :167-175
[9]   The characteristics of wind and wave fields modelled with different resolutions [J].
Cavaleri, L ;
Bertotti, L .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2003, 129 (590) :1647-1662
[10]  
Cavaleri L, 1997, MON WEATHER REV, V125, P1964, DOI 10.1175/1520-0493(1997)125<1964:ISOTCW>2.0.CO