지역기후모형을 이용한 한반도 주변해 해양기후전망

Abstract

A linear trend of sea surface temperature (SST) for the seas around Korea shows different spatial distribution (Min and Kim, 2006). Most of global climate models, however, cannot resolve well the regional features of historical and future ocean climate change for the seas around Korea due to their coarse resolution. It has motivated us to develop a regional climate model for the western North Pacific including the marginal seas. We conducted a historical simulation as a baseline and a future climate projection simulation using Regional Ocean Modeling System (ROMS) with a horizontal resolution of 1/12°. For the future climate projection, the model was forced with the time-averaged difference fields of 2081-2100 RCP4.5 run and 1981-2000 historical run simulated with CanESM2 for CMIP5 and the difference fields were superimposed on the present climate represented by National Centers for Environmental Prediction (NCEP) and Simple Ocean Data Assimilation (SODA) reanalysis data. This is known as the Pseudo Global Warming (PGW) method developed by Kimura and Kitoh (2007). On the other hand, we also conducted a future climate projection simulation using an atmospheric model, Wether Research Forecasting (WRF) with a horizontal resolution of 50 km to investigate the high resolution effects of future surface forcing for the seas around Korea. The model simulated the historical time series of SST anomaly showing similar trends tcean climate change for the seas around Korea due to their coarse resolution. It has motivated us to develop a regional climate model for the western North Pacific including the marginal seas. We conducted a historical simulation as a baseline and a future climate projection simulation using Regional Ocean Modeling System (ROMS) with a horizontal resolution of 1/12°. For the future climate projection, the model was forced with the time-averaged difference fields of 2081-2100 RCP4.5 run and 1981-2000 historical run simulated with CanESM2 for CMIP5 and the difference fields were superimposed on the present climate represented by National Centers for Environmental Prediction (NCEP) and Simple Ocean Data Assimilation (SODA) reanalysis data. This is known as the Pseudo Global Warming (PGW) method developed by Kimura and Kitoh (2007). On the other hand, we also conducted a future climate projection simulation using an atmospheric model, Wether Research Forecasting (WRF) with a horizontal resolution of 50 km to investigate the high resolution effects of future surface forcing for the seas around Korea. The model simulated the historical time series of SST anomaly showing similar trends t