4.7 Article

Future Thermodynamic Impacts of Global Warming on Landfalling Typhoons and Their Induced Storm Surges to the Pearl River Delta Region as Inferred from High-Resolution Regional Models

期刊

JOURNAL OF CLIMATE
卷 35, 期 15, 页码 4905-4926

出版社

AMER METEOROLOGICAL SOC
DOI: 10.1175/JCLI-D-21-0436.1

关键词

Storm surges; Climate change; Greenhouse gases; Hurricanes; typhoons; Numerical analysis; modeling

资金

  1. National Key Research and Development Program of China [2019YFC1510400]
  2. Hong Kong Research Grant Council's General Research Fund [14306115]
  3. Chinese University of Hong Kong [A.02.20.00401]
  4. Guangdong Major Project of Basic and Applied Basic Research [2020B0301030004]
  5. Pearl River S&T Nova Program of Guangzhou [201906010054]
  6. Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies [2020B1212060025]
  7. National Natural Science Foundation of China [42105161]
  8. Shenzhen Research Institute

向作者/读者索取更多资源

This study investigates the possible thermodynamic effects of global warming on landfalling typhoons and storm surges in South China, using the WRF and SLOSH models. The findings suggest that under a warmer climate, typhoon intensity, storm structure, precipitation, and storm surge may all change and have implications for South China and the Pearl River Delta region.
Possible thermodynamic effects of global warming on the landfalling typhoons that affect South China and their associated storm surges over Pearl River Delta region are investigated, using the Weather Research and Forecasting (WRF) Model and the Sea, Lake, and Overland Surges from Hurricanes (SLOSH) model based on the pseudo-global warming (PGW) technique. Twenty intense historical TCs that brought extreme storm surges to Hong Kong since the 1960s are selected and replicated by the 3-km WRF Model, with the outputs to drive the SLOSH model in storm surge simulation. The tracks, intensities, storm structure, and induced storm surges are well simulated. The PGW technique is then used to build a warmer background climate for the 20 selected TCs in the period of 2075-99 under the RCP8.5 scenario. To obtain a better adjusted warming environment, a pre-PGW adjustment method is developed. Comparing the same TCs in PGW experiments and historical runs, the TC lifetime peak (landfall) intensity can be intensified by about 9% +/- 8% (12% +/- 13%), with a similar to 3% increase of TC peak intensity per degree of SST warming being inferred. The TCs are projected to be more compact, with the radius of maximum wind (RMW) reduced by similar to 7% +/- 10%. TC precipitation is also expected to increase, with the extreme precipitation within the eyewall strengthened by 22% +/- 12%. All the above characters have passed the Student's t test at 0.05 significance level. Finally, the projected induced storm surges near the Hong Kong waters are not significantly tested, although a weak storm surge height increase tendency is revealed.

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