An assessment of the wind re-analyses in the modelling of an extreme sea state in the Black Sea


AKPINAR A. , Ponce de Leon S.

DYNAMICS OF ATMOSPHERES AND OCEANS, vol.73, pp.61-75, 2016 (Journal Indexed in SCI) identifier identifier

  • Publication Type: Article / Article
  • Volume: 73
  • Publication Date: 2016
  • Doi Number: 10.1016/j.dynatmoce.2015.12.002
  • Title of Journal : DYNAMICS OF ATMOSPHERES AND OCEANS
  • Page Numbers: pp.61-75
  • Keywords: Wind waves, SWAN, Black Sea, Calibration, Satellite altimetry data, Extreme sea states, WAVE MODEL, NUMERICAL-MODELS, PERFORMANCE

Abstract

This study aims at an assessment of wind re-analyses for modelling storms in the Black Sea. A wind-wave modelling system (Simulating WAve Nearshore, SWAN) is applied to the Black Sea basin and calibrated with buoy data for three recent re-analysis wind sources, namely the European Centre for Medium-Range Weather Forecasts Reanalysis-Interim (ERA-Interim), Climate Forecast System Reanalysis (CFSR), and Modern Era Retrospective Analysis for Research and Applications (MERRA) during an extreme wave condition that occurred in the north eastern part of the Black Sea. The SWAN model simulations are carried out for default and tuning settings for deep water source terms, especially whitecapping. Performances of the best model configurations based on calibration with buoy data are discussed using data from the JASON2, TOPEX-Poseidon, ENVISAT and GFO satellites. The SWAN model calibration shows that the best configuration is obtained with Janssen and Komen formulations with whitecapping coefficient (C-ds) equal to 1.8e-5 for wave generation by wind and whitecapping dissipation using ERA-Interim. In addition, from the collocated SWAN results against the satellite records, the best configuration is determined to be the SWAN using the CFSR winds. Numerical results, thus show that the accuracy of a wave forecast will depend on the quality of the wind field and the ability of the SWAN model to simulate the waves under extreme wind conditions in fetch limited wave conditions. (C) 2015 Elsevier B.V. All rights reserved.