Tropical Cyclones and Climate Suzana J. Camargo Lamont-Doherty Earth Observatory Columbia University Collaborators: Chia-Ying Lee, Adam H. Sobel, Michael K. Tippett, Allison A. Wing HURRICANE BASIC SCIENCE Self-aggregation: spontaneous organization of convection Applying ideas of self-aggregation to tropical cyclone formation Spontaneous tropical cyclogenesis in idealized numerical simulations of rotating Radiative-Convective Equilibrium What is the role of radiative-convective feedbacks in tropical cyclogenesis? Allison Wing, NSF Postdoctoral Research Fellow, Lamont-Doherty Earth Observatory TROPICAL CYCLONE GENESIS INDICES IN FUTURE CLIMATES Camargo, S.J, M.K. Tippett, A.H. Sobel, G.A. Vecchi, and M. Zhao, 2014: Testing the performance of tropical cyclone genesis in future climates using the HiRAM model. J. Climate, 27, 9171-9196. Genesis Indices • Relate key large-scale environmental variables to tropical cyclone (TC) frequency globally • Lack of quantitative genesis theory – empirical methods are useful • Reproduce seasonal and spatial variability of TC frequency using few variables • Combination of dynamical reasoning and statistical modeling to understand the probability of TC formation Tropical Cyclone Genesis Index • Robust, objective and easily reproducible procedure • Poisson Regression: objective and provides a framework for the selection of variables – Tippett, Camargo & Sobel, J. Climate (2011) • Same methodology successfully applied for – Tornadoes (Tippett, Sobel, Camargo, GRL, 2012) – Hail (Allen, Tippett, Sobel, JAMES, 2015; Nature Geoscience, 2015) – Monsoon depressions (Ditcheck, Boos, Camargo & Tippett, in prep.) TCGI – Present climate Climate Change & Genesis indices • Most model predictions: reduction in TC frequency with climate change • Genesis indices predict: increase in TC frequency with climate change “Best Index”: Saturation Deficit & PI DEVELOPMENT OF A HURRICANE RISK MODEL Chia-Ying Lee, Michael K. Tippett, Adam H. Sobel and Suzana J. Camargo Hurricane Risk Model • What’s the probability that a category 5 hurricane hit New York City or Boston or Washington DC? • How does it depend on climate? Development of a tropical cyclone “risk model” – generator of synthetic TC tracks as function of environment. Applications to climate change, variability, risk assessment, insurance. The critical component is a model for TC intensity as function of environment. We will use a statistical-dynamical model with a stochastic component. Genesis densities from observations (left), downscaling model (right) from Emanuel et al. (2008, BAMS) Approach: probabilistic multiple-linear regression model – TC intensity & environmental variables Tracks and intensity forecasts for Hurricanes Rita (2005), Earl (2010), Irene (2011) and Isaac (2012). Lee, C-Y, M.K. Tippett, S.J. Camargo, and A.H. Sobel, Monthly Weather Review, 2015 Development of a probabilistic stochastic model V0=60 kt V0=40 kt PDF [%] Forecast time Predicted intensity forecast time[hr] The performance is comparable to that of current operational models Mean absolute error (MAE) of intensity predictions from the persistence (gray-solid line), the SHIFOR (gray-dashed line), the SHIPS forecast (black-solid line), the SHIPS dependent (black-dashed line), the MLR forecast (red-solid line), and the MLR dependent (red-dashed line) models. Simulation of global intensities using all observed tracks for 31 years Upper: Storm intensity from 1981 to 2012 from observations (left) and stochastic model(right). Lower: Similar to the upper two figures, but for probabilities (%) of major storms per year per degree. • Goal: develop a global TC synthetic track generator to be used in risk assessment. • We have developed a hurricane intensity MLR model whose forecast skill is comparable to operational models (but can handle climate applications) • We have developed a stochastic model which gives a decent simulation of the global distribution of intensities. Summary • Overview of TC research at Columbia University. • A variety of methods are being used to study tropical cyclones and climate at Columbia University. • The chosen approaches are problem dependent, varying from idealized hurricane models to sophisticated statistical models, including global climate models.
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