Data Assimilation for Phase-Resolved Ocean Wave Forecast

2021 ◽  
Author(s):  
Guangyao Wang ◽  
Yulin Pan
2016 ◽  
Vol 41 (4) ◽  
pp. 944-953 ◽  
Author(s):  
Aditya N. Deshmukh ◽  
M. C. Deo ◽  
Prasad K. Bhaskaran ◽  
T. M. Balakrishnan Nair ◽  
K. G. Sandhya

2006 ◽  
Vol 14 (1-2) ◽  
pp. 102-121 ◽  
Author(s):  
S.A. Sannasiraj ◽  
Vladan Babovic ◽  
Eng Soon Chan

2021 ◽  
pp. 77-87
Author(s):  
M. Sai Pravallika ◽  
B. Naga Varun ◽  
S. Vasavi ◽  
N. Sandeep ◽  
M. Jaya Priya ◽  
...  

1996 ◽  
Vol 118 (3) ◽  
pp. 184-189 ◽  
Author(s):  
L. H. Holthuijsen ◽  
N. Booij ◽  
L. Bertotti

To estimate uncertainties in wave forecast and hindcasts, computations have been carried out for a location in the Mediterranean Sea using three different analyses of one historic wind field. These computations involve a systematic sensitivity analysis and estimated wind field errors. This technique enables a wave modeler to estimate such uncertainties in other forecasts and hindcasts if only one wind analysis is available.


2009 ◽  
Vol 59 (3) ◽  
pp. 523-535 ◽  
Author(s):  
George Galanis ◽  
George Emmanouil ◽  
Peter C. Chu ◽  
George Kallos

Author(s):  
Guangyao Wang ◽  
Yulin Pan

Abstract The phase-resolved prediction of ocean waves is crucial for the safety of offshore operations. With the development of the remote sensing technology, it is now possible to reconstruct the phase-resolved ocean surface from radar measurements in real time. Using the reconstructed ocean surface as the initial condition, nonlinear wave models such as the high-order spectral (HOS) method can be applied to predict the evolution of the ocean waves. However, due to the error in the initial condition (associated with the radar measurements and reconstruction algorithm) and the chaotic nature of the nonlinear wave equations, the prediction by HOS can deviate quickly from the true surface evolution (in order of one minute). To solve this problem, the capability to regularly incorporate measured data into the HOS simulation through data assimilation is desirable. In this work, we develop the data assimilation capability for nonlinear wave models, through the coupling of an ensemble Kalman filter (EnKF) with HOS. The developed algorithm is validated and tested using a synthetic problem on the simulation of a propagating Stokes wave with random initial errors. We show that the EnKF-HOS method achieves much higher accuracy in the long-term simulation of nonlinear waves compared to the HOS-only method.


2020 ◽  
Author(s):  
Malek Ghantous ◽  
Lotfi Aouf ◽  
Alice Dalphinet ◽  
Cristina Toledano ◽  
Lorea García San Martín ◽  
...  

<p>One of the challenges of the Iberia-Biscay-Ireland (IBI) Monitoring Forecasting Centre in CMEMS phase 2 is the implementation of the assimilation of altimeter wave data in the wave forecast system.  In this work we explored the impact of the assimilation of altimeter wave data in the IBI domain.  We ran the Météo France version of the WAM wave model (MFWAM) in the IBI domain for 2018 and 2019, with data assimilated from the Jason 2 and 3, Saral, Cryosat 2 and Sentinel 3 altimeters.  This high-resolution (0.05 degree) configuration was forced by 0.05 degree ECMWF winds, and boundary conditions were provided by a 0.1 degree global model run.  We also included refraction from currents generated with the NEMO-IBI ocean circulation model.  We present results with and without wave–current interactions.  Validation against both buoy data and the HaiYang 2 altimeter shows that the assimilation of data leads to a marked reduction in scatter index and model bias compared to the run without data assimilation; the gains from including currents meanwhile are modest.  </p><p>The data assimilation scheme presently implemented in MFWAM uses an optimal interpolation algorithm where constant model and observational errors are assumed.  To add some sophistication, we experimented with non-constant background errors derived from a model ensemble.  Though the effect was small, the method suggests a way to improve the data assimilation performance without substantially altering the algorithm.</p>


Sign in / Sign up

Export Citation Format

Share Document