Producing the Hindcast of Wind and Waves Using a High-Resolution Atmospheric Reanalysis around Korea

DC Field Value Language
dc.contributor.author 허기영 -
dc.date.accessioned 2020-07-15T21:53:16Z -
dc.date.available 2020-07-15T21:53:16Z -
dc.date.created 2020-02-11 -
dc.date.issued 2016-04-21 -
dc.identifier.uri https://sciwatch.kiost.ac.kr/handle/2020.kiost/24876 -
dc.description.abstract Sea surface wind plays a dominant role in oceanic phenomena such as oceanic waves, swells and currents that have an important effect of the climate. However, the lack of reliable historical weather observations and limited data make it difficult to effectively analyze climate variability and change over the ocean. In contrast, numerical simulation data takes advantage to analyze spatiotemporal variation of sea surface wind, but has a fundamental limit to exactly reproduce atmospheric phenomena due to initial uncertainty in the model initialization and the chaotic behavior of nonlinear system governing the atmosphere (National Research Council, 1998).To overcome the limitations, data assimilation technique has been adopted to improve the model’s initial conditions and generate the final high-resolution analysis. The reanalysis comprises the combination of state of art models and data assimilation methods with highly quality controlled observations including surface, upper-level sounding and satellite based observations. Since the release of the original National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) Reanalysis Project (NCEP-1),the NCEP/NCAR, the European Centre for Medium-Range Weather Forecasts (ECMWF), and Japan Meteorological Agency (JMA) and the Central Research Institute of Electric Power Industry (CRIEPI) produce reanalysis products covering 1979 to presenticult to effectively analyze climate variability and change over the ocean. In contrast, numerical simulation data takes advantage to analyze spatiotemporal variation of sea surface wind, but has a fundamental limit to exactly reproduce atmospheric phenomena due to initial uncertainty in the model initialization and the chaotic behavior of nonlinear system governing the atmosphere (National Research Council, 1998).To overcome the limitations, data assimilation technique has been adopted to improve the model’s initial conditions and generate the final high-resolution analysis. The reanalysis comprises the combination of state of art models and data assimilation methods with highly quality controlled observations including surface, upper-level sounding and satellite based observations. Since the release of the original National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) Reanalysis Project (NCEP-1),the NCEP/NCAR, the European Centre for Medium-Range Weather Forecasts (ECMWF), and Japan Meteorological Agency (JMA) and the Central Research Institute of Electric Power Industry (CRIEPI) produce reanalysis products covering 1979 to present -
dc.description.uri 1 -
dc.language English -
dc.publisher CKJORC -
dc.relation.isPartOf The 7th Korea-China Joint Workshop on Marine Environment Forecasting System for the Yellow Sea and East China Sea -
dc.title Producing the Hindcast of Wind and Waves Using a High-Resolution Atmospheric Reanalysis around Korea -
dc.type Conference -
dc.citation.conferencePlace KO -
dc.citation.endPage 2 -
dc.citation.startPage 1 -
dc.citation.title The 7th Korea-China Joint Workshop on Marine Environment Forecasting System for the Yellow Sea and East China Sea -
dc.contributor.alternativeName 허기영 -
dc.identifier.bibliographicCitation The 7th Korea-China Joint Workshop on Marine Environment Forecasting System for the Yellow Sea and East China Sea, pp.1 - 2 -
dc.description.journalClass 1 -
Appears in Collections:
Sea Power Enhancement Research Division > Coastal Disaster & Safety Research Department > 2. Conference Papers
Files in This Item:
There are no files associated with this item.

qrcode

Items in ScienceWatch@KIOST are protected by copyright, with all rights reserved, unless otherwise indicated.

Browse