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Present Simulation and Future Typhoon Activity Projection over Western North Pacific and Taiwan/East Coast of China in 20-km HiRAM Climate Model

机译:20 km HiRAM气候模式中北太平洋西部和中国台湾/东海岸的当前模拟和未来台风活动预测

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A High Resolution Atmospheric Model (HiRAM) at 20-km resolution is adopted to simulate tropical storm (TS) activity over the western North Pacific (WNP) and Taiwan/East Coast of China (TWCN) at the present time (1979 - 2003) and future climate (2075 - 2099) under the Intergovernmental Panel on Climate Change (IPCC) fifth assessment report (AR5) representative concentration pathway (RCP) 8.5 scenarios. The results show that in contrast to TS simulation activities in most of the low-resolution climate models, TS activities except intensity over the WNP and TWCN region are well simulated by HiRAM at 20-km resolution. The linkage between large-scale environments and TS genesis simulated by HiRAM are dramatically superior to those in low-resolution fifth Coupled Model Intercomparison Project (CMIP5) models. During 2075 - 2099, both TS genesis numbers and TS frequency over the WNP and TWCN are projected to decrease consistent with the IPCC AR5 report. However, the rate of decrease (49%) is much greater than that projected in IPCC AR5. The decrease in TC genesis numbers under global warming is primarily attributed to the reduction in mid-level relative humidity and large-scale ascending motion, despite the warmer sea surface temperature (SST) providing more favorable conditions for TS formation. TS intensity and the maximum precipitation rate are projected to increase under global warming. At the end of the 21st century, the mean precipitation rate within 200 km of TS storm center over the TWCN region is projected to increase by 54%.
机译:目前(1979年至2003年)采用了分辨率为20公里的高分辨率大气模型(HiRAM)来模拟北太平洋西部(WNP)和中国台湾/中国东海岸(TWCN)上的热带风暴(TS)活动。政府间气候变化专门委员会(IPCC)第五次评估报告(AR5)代表性浓度途径(RCP)8.5情景下的未来气候变化(2075-2099)。结果表明,与大多数低分辨率气候模式中的TS模拟活动相反,HiRAM在20 km分辨率下很好地模拟了WNP和TWCN区域上除强度以外的TS活动。 HiRAM模拟的大规模环境与TS生成之间的关联性明显优于低分辨率第五耦合模型比较项目(CMIP5)模型中的链接。在2075年至2099年期间,预计WNP和TWCN上的TS发生数和TS频率都会减少,与IPCC AR5报告一致。但是,下降速度(49%)远大于IPCC AR5的预测速度。尽管变暖的海面温度(SST)为TS的形成提供了更有利的条件,但在全球变暖下TC发生数的减少主要归因于中层相对湿度和大规模上升运动的减少。随着全球变暖,TS强度和最大降水率预计会增加。到21世纪末,预计TWCN地区TS风暴中心200公里以内的平均降水量将增加54%。

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