Tropical Cyclones and Climate Change Assessment: Part I: Detection and Attribution

Author:

Knutson Thomas1,Camargo Suzana J.2,Chan Johnny C. L.3,Emanuel Kerry4,Ho Chang-Hoi5,Kossin James6,Mohapatra Mrutyunjay7,Satoh Masaki8,Sugi Masato9,Walsh Kevin10,Wu Liguang11

Affiliation:

1. NOAA/Geophysical Fluid Dynamics Laboratory, Princeton, New Jersey

2. Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York

3. Guy Carpenter Asia-Pacific Climate Impact Centre, City University of Hong Kong, Hong Kong, China

4. Department of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts

5. School of Earth and Environmental Sciences, Seoul National University, Seoul, South Korea

6. Center for Weather and Climate, NOAA/National Centers for Environmental Information, Madison, Wisconsin

7. India Meteorological Department, New Delhi, India

8. Atmosphere and Ocean Research Institute, The University of Tokyo, Chiba, Japan

9. Meteorological Research Institute, Tsukuba, Japan

10. School of Earth Sciences, University of Melbourne, Parkville, Victoria, Australia

11. Nanjing University of Information Science and Technology, Nanjing, Jiangsu, China

Abstract

AbstractAn assessment was made of whether detectable changes in tropical cyclone (TC) activity are identifiable in observations and whether any changes can be attributed to anthropogenic climate change. Overall, historical data suggest detectable TC activity changes in some regions associated with TC track changes, while data quality and quantity issues create greater challenges for analyses based on TC intensity and frequency. A number of specific published conclusions (case studies) about possible detectable anthropogenic influence on TCs were assessed using the conventional approach of preferentially avoiding type I errors (i.e., overstating anthropogenic influence or detection). We conclude there is at least low to medium confidence that the observed poleward migration of the latitude of maximum intensity in the western North Pacific is detectable, or highly unusual compared to expected natural variability. Opinion on the author team was divided on whether any observed TC changes demonstrate discernible anthropogenic influence, or whether any other observed changes represent detectable changes. The issue was then reframed by assessing evidence for detectable anthropogenic influence while seeking to reduce the chance of type II errors (i.e., missing or understating anthropogenic influence or detection). For this purpose, we used a much weaker “balance of evidence” criterion for assessment. This leads to a number of more speculative TC detection and/or attribution statements, which we recognize have substantial potential for being false alarms (i.e., overstating anthropogenic influence or detection) but which may be useful for risk assessment. Several examples of these alternative statements, derived using this approach, are presented in the report.

Publisher

American Meteorological Society

Subject

Atmospheric Science

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