Citation:
Mínguez, R., Espejo, A., Tomás, A., Méndez, F. J., & Losada, I. J. (2011). Directional Calibration of Wave Reanalysis Databases Using Instrumental Data. Journal of Atmospheric and Oceanic Technology, 28 (11), pp. 1466-1485
xmlui.dri2xhtml.METS-1.0.item-contributor-funder:
Ministerio de Ciencia e Innovación (España) Ministerio de Medio Ambiente y Medio Rural y Marino (España)
Sponsor:
The authors thank Puertos del
Estado (Spanish State Port) for providing the information
from the wave reanalysis data base. R. Mínguez
is indebted to the Spanish Ministry MICINN for the
funding provided within the Ramon y Cajal program.
This work was partly funded by projects GRACCIE
(CSD2007-00067, ProgramaConsolider-Ingenio 2010) and
AMVAR (CTM2010-15009) from the Spanish Ministry
MICINN, by Project C3E (200800050084091) from the
Spanish Ministry MAMRM, and by Project MARUCA
(E17/08) from the Spanish Ministry MF.
Project:
Gobierno de España. CTM2010-15009 Gobierno de España. CSD2007-00067 Gobierno de España. E17/08 Gobierno de España. 200800050084091 Gobierno de España. CSD2007-00067
Wave reanalysis databases (WRDBs) offer important advantages for the statistical characterization of wave climate (continuous time series, good spatial coverage, constant time span, homogeneous forcing, and more than a 40-yr-long time series) and for this reasWave reanalysis databases (WRDBs) offer important advantages for the statistical characterization of wave climate (continuous time series, good spatial coverage, constant time span, homogeneous forcing, and more than a 40-yr-long time series) and for this reason, they have become a powerful tool for the design of offshore and coastal structures. However, WRDBs are not quantitatively perfect and corrections using instrumental observations must be addressed before they are used; this process is called calibration. The calibration is especially relevant near the coast and in areas where the orography is complex, since in these places the inaccuracy of WRDB is evident because of the bad description of the wind fields (i.e., insufficient forcing resolution). The quantitative differences between numerical and instrumental data suggest that different corrections should be applied depending on the mean direction of the sea state. This paper proposes a calibration method based on a nonlinear regression problem, where the corresponding correction parameters vary smoothly along the possible wave directions by means of cubic splines. The correction of significant wave height is performed using instrumental data: (i) buoy records and/or (ii) satellite data. The performance of the method is illustrated considering data from different locations around Spain[+][-]