首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Projected changes of typhoon intensity in a regional climate model: Development of a machine learning bias correction scheme
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Projected changes of typhoon intensity in a regional climate model: Development of a machine learning bias correction scheme

机译:区域气候模型中台风强度的预测变化:机器学习偏差校正方案的发展

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摘要

A machine learning-based bias correction scheme was developed to adjust the simulated Western North Pacific typhoon intensity in a 25-km regional climate model (RCM). The bias correction scheme, MLERA, consists of a hybrid neural network, which takes modelled atmospheric and oceanic conditions near the storm centre as input. We use air temperature, specific humidity, and relative vorticity at 300 hPa, geopotential height at 700 hPa, wind speed at 850 hPa, sea-level pressure, 10-m wind speed, and total air-sea fluxes. Those predictors are selected using least absolute shrinkage and selection operator (Lasso) algorithm and principal component analysis (PCA). Because there is no 'ground truth' for RCM simulated storms, we train and test MLERA using ERA-Interim reanalysis and best-track data. The intensity statistics estimated from MLERA match well with those from observations. MLERA, when applied to RCM history base period, increases the likelihood of simulated typhoons (with wind speed >33 m/s) from 40.8 to 73.9% in the direct simulation. Meanwhile, the RCM itself produces no C3+ storms (wind speed >50 m/s) in both RCP4.5 and RCP8.5 scenarios, while MLERA significantly increases those storms. MLERA suggests an increasing trend of the frequency of violent typhoons from near-term (2031-2060) to long-term (2069-2098). Such an increase is consistent with our understanding that a warming climate will increase the storm intensity. The present study shows the potential of the machine learning technique for bias correcting cyclone intensity in RCMs. Furthermore, the proposed algorithm could also be applied to the next generation of high-resolution global climate models, which may have a spatial grid spacing close to today's RCMs.
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