Third Assessment on Impacts of Climate Change on Tropical Cyclones in the Typhoon Committee Region E Part I: Observed Changes, Detection and Attribution
Available online at www.sciencedirect.com ScienceDirect Tropical Cyclone Research and Review 9 (2020) 1e22 www.keaipublishing.com/tcrr Third assessment on impacts of climate change on tropical cyclones in the Typhoon Committee Region e Part I: Observed changes, detection and attribution Tsz-Cheung Lee a,*, Thomas R. Knutson b, Toshiyuki Nakaegawa c, Ming Ying d, Eun Jeong Cha e a Hong Kong Observatory, Hong Kong, China b Geophysical Fluid Dynamics Laboratory/NOAA, Princeton, NJ, USA c Meteorological Research Institute/Japan Meteorological Agency, Tsukuba, Japan d Shanghai Typhoon Institute, China Meteorological Administration, Shanghai, China e National Typhoon Center, Korea Meteorological Administration, Jeju, Republic of Korea Available online 20 March 2020 Abstract Published findings on climate change impacts on tropical cyclones (TCs) in the ESCAP/WMO Typhoon Committee Region are assessed. We focus on observed TC changes in the western North Pacific (WNP) basin, including frequency, intensity, precipitation, track pattern, and storm surge. Results from an updated survey of impacts of past TC activity on various Members of the Typhoon Committee are also reported. Existing TC datasets continue to show substantial interdecadal variations in basin-wide TC frequency and intensity in the WNP. There has been encouraging progress in improving the consensus between different datasets concerning intensity trends. A statistically significant northwest- ward shift in WNP TC tracks since the 1980s has been documented. There is low-to-medium confidence in a detectable poleward shift since the 1940s in the average latitude where TCs reach their peak intensity in the WNP. A worsening of storm inundation levels is believed to be occurring due to sea level rise-due in part to anthropogenic influence-assuming all other factors equal.
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