2010
DOI: 10.1080/1755876x.2010.11020112
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Forecasting the Aegean Sea hydrodynamics within the POSEIDON-II operational system

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Cited by 26 publications
(26 citation statements)
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“…The heat and freshwater fluxes, at the air-sea interface, are calculated using hourly fields of wind velocity (10 m), relative humidity (2 m), air temperature (2 m), precipitation, net incoming short wave radiation and incoming long wave radiation, using properly tuned bulk formulae set (Korres and Lascaratos, 2003). The circulation model implemented in this study has been validated through various applications with finer (e.g., Kourafalou et al, 2006;Korres et al, 2010) or coarser horizontal resolution (Korres et al, 2007;Tsiaras et al, 2014). The same model is currently operational with a slightly higher resolution (1/30 • ) as part of the POSEIDON forecasting system (www.poseidon.hcmr.…”
Section: Circulation Modelmentioning
confidence: 99%
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“…The heat and freshwater fluxes, at the air-sea interface, are calculated using hourly fields of wind velocity (10 m), relative humidity (2 m), air temperature (2 m), precipitation, net incoming short wave radiation and incoming long wave radiation, using properly tuned bulk formulae set (Korres and Lascaratos, 2003). The circulation model implemented in this study has been validated through various applications with finer (e.g., Kourafalou et al, 2006;Korres et al, 2010) or coarser horizontal resolution (Korres et al, 2007;Tsiaras et al, 2014). The same model is currently operational with a slightly higher resolution (1/30 • ) as part of the POSEIDON forecasting system (www.poseidon.hcmr.…”
Section: Circulation Modelmentioning
confidence: 99%
“…odu.edu/POMWEB/) with numerous applications both for ocean and regional modeling studies. POM has been implemented in the Mediterranean Sea at basin/sub-basin scale (Zavatarelli and Mellor, 1995;Horton et al, 1997;Korres and Lascaratos, 2003, among others) and also on regional studies, including the Aegean Sea (Korres et al, 2010;Androulidakis et al, 2012;among others). It is a primitive equation, sigma coordinate and free surface elevation model that employes a 2.5 turbulence closure scheme (Mellor and Yamada, 1982) for vertical mixing.…”
Section: Circulation Modelmentioning
confidence: 99%
“…o ) regional atmospheric model (Papadopoulos and Katsafados, 2009) issuing forecasts for 5 days ahead. The assimilation system for the Mediterranean Sea hydrodynamic model is very similar to the one presented in the work of Korres et al (2010). It is based on the singular evolutive extended Kalman (SEEK) filter with covariance localization and partial evolution of the correction directions.…”
Section: Appendix A: Data Set Descriptionmentioning
confidence: 99%
“…The error covariance matrix is approximated with 60 EOF modes (correction directions), where the first 18 (the most dominant ones) are evolved with the model dynamics while the rest are kept invariant in time. The localization technique adopted for the Mediterranean Sea forecasting system is explained in Korres et al (2010). The method localizes the covariance matrix by neglecting observations beyond a cut-off radius which is selected upon sensitivity studies to be equal to 200 km.…”
Section: Appendix A: Data Set Descriptionmentioning
confidence: 99%
“…The assimilation scheme is based on the Singular Evolutive Extended Kalman (SEEK) filter which is an error subspace extended Kalman filter that operates with low-rank error covariance matrices as a way to reduce the prohibitive computational burden of the extended Kalman filter (Pham et al, 1998). The filter is additionally implemented with covariance localization and partial evolution of the correction directions (Korres et al, 2010).…”
Section: The Hydrodynamic Modelmentioning
confidence: 99%