Wave modeling performance in the Gulf of Mexico and Western Caribbean: Wind reanalyses assessment

被引:56
作者
Appendini, Christian M. [1 ]
Torres-Freyermuth, Alec [1 ]
Oropeza, Fernando [2 ]
Salles, Paulo [1 ]
Lopez, Jose [1 ]
Mendoza, E. Tonatiuh [1 ]
机构
[1] Univ Nacl Autonoma Mexico, Inst Ingn, Lab Ingn & Proc Costeros, Sisal 92718, Mexico
[2] Univ Nacl Autonoma Mexico, Ctr Ciencias Atmosfera, Mexico City 04360, DF, Mexico
关键词
Wave modeling; Wave hindcast; Wind reanalysis; Gulf of Mexico; ATLANTIC HURRICANE SEASON; NCEP-NCAR REANALYSIS; HINDCAST; DISSIPATION; CLIMATE; DRAG; FLOW;
D O I
10.1016/j.apor.2012.09.004
中图分类号
P75 [海洋工程];
学科分类号
0814 ; 081505 ; 0824 ; 082401 ;
摘要
This paper evaluates the wave modeling performance in the Gulf of Mexico and Western Caribbean Sea employing three different wind reanalysis data. Wind reanalysis is employed as the main forcing in wave generation/propagation numerical models. While the National Centers for Environmental Prediction (NCEP)/National Center for Atmospheric Research (NCAR) and the European Centre for Medium-Range Weather Forecasts (ECMWFs) ERA-40 reanalyses have been previously assessed in the performance for wave modeling, ECMWF's ERA-interim and in particular NCEP's North American Regional Reanalysis (NARR) are more recent reanalyses. They both provide better resolution and description of the wind fields and have not been evaluated for long-term wave modeling. Therefore, the aim of this work is the assessment of the three different wind reanalyses on the wave hindcast performance. Attention is drawn on the wind reanalysis capability for predicting both mean and extreme wave conditions during two different periods: (i) an anomalous year where cyclonic events dominate the extreme wave climate in the region (2005); and (ii) a year with the wave climate dominated by synoptic events (2006). A third generation wave model, forced by the different wind reanalysis data, is calibrated with National Data Buoy Center (NDBC) buoys observations. Wind reanalysis data allow a consistent implementation of third generation wave models in order to predict the mean wave climate (correlation coefficient similar to 0.84 for NCEP/NCAR, 0.94 for ERA-interim, 0.92 for NARR) for applied ocean studies. Numerical results revealed that both ERA-interim and NARR improve the wave modeling performance with respect to NCEP/NCAR (for extreme and non-extreme conditions), whereas the high- (spatial and temporal) resolution NARR data are more suitable for modeling extreme cyclonic events (i.e., hurricanes) in this region. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:20 / 30
页数:11
相关论文
共 49 条
  • [11] Danish Hydraulic Institute (DHI), 2011, MIKE 21 SPECTR WAV M
  • [12] The ERA-Interim reanalysis: configuration and performance of the data assimilation system
    Dee, D. P.
    Uppala, S. M.
    Simmons, A. J.
    Berrisford, P.
    Poli, P.
    Kobayashi, S.
    Andrae, U.
    Balmaseda, M. A.
    Balsamo, G.
    Bauer, P.
    Bechtold, P.
    Beljaars, A. C. M.
    van de Berg, L.
    Bidlot, J.
    Bormann, N.
    Delsol, C.
    Dragani, R.
    Fuentes, M.
    Geer, A. J.
    Haimberger, L.
    Healy, S. B.
    Hersbach, H.
    Holm, E. V.
    Isaksen, L.
    Kallberg, P.
    Koehler, M.
    Matricardi, M.
    McNally, A. P.
    Monge-Sanz, B. M.
    Morcrette, J. -J.
    Park, B. -K.
    Peubey, C.
    de Rosnay, P.
    Tavolato, C.
    Thepaut, J. -N.
    Vitart, F.
    [J]. QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2011, 137 (656) : 553 - 597
  • [13] Atlantic hurricane season of 2006
    Franklin, James L.
    Brown, Daniel P.
    [J]. MONTHLY WEATHER REVIEW, 2008, 136 (03) : 1174 - 1200
  • [14] Hasselmann K., 1974, Boundary-Layer Meteorology, V6, P107, DOI 10.1007/BF00232479
  • [15] JANSSEN PAEM, 1989, J PHYS OCEANOGR, V19, P745, DOI 10.1175/1520-0485(1989)019<0745:WISATD>2.0.CO
  • [16] 2
  • [17] Jose F, 2007, J COASTAL RES, P757
  • [18] Kalnay E, 1996, B AM METEOROL SOC, V77, P437, DOI 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO
  • [19] 2
  • [20] Komen G.J., 1994, DYNAMICS MODELLING O, DOI DOI 10.1017/CBO9780511628955