Combined Effect of PDO and ENSO on the Date of the First Tropical Cyclone Landfall in Continental Eastern Asia

Author(s):  
Shuang Li ◽  
Ziniu Xiao ◽  
Yuchun Zhao
2019 ◽  
Vol 34 (5) ◽  
pp. 1239-1255 ◽  
Author(s):  
Dan L. Bergman ◽  
Linus Magnusson ◽  
Johan Nilsson ◽  
Frederic Vitart

Abstract A method has been developed to forecast seasonal landfall risk using ensembles of cyclone tracks generated by ECMWF’s seasonal forecast system 4. The method has been applied to analyze and retrospectively forecast the landfall risk along the North American coast. The main result is that the method can be used to forecast landfall for some parts of the coast, but the skill is lower than for basinwide forecasts of activity. The rank correlations between forecasts issued on 1 May and observations are 0.6 for basinwide tropical cyclone number and 0.5 for landfall anywhere along the coast. When the forecast period is limited to the peak of the hurricane season, the landfall correlation increases to 0.6. Moreover, when the forecast issue date is pushed forward to 1 August, basinwide tropical cyclone and hurricane correlations increase to 0.7 and 0.8, respectively, whereas landfall correlations improve less. The quality of the forecasts is in line with that obtained by others.


2003 ◽  
Vol 16 (23) ◽  
pp. 3932-3945 ◽  
Author(s):  
Frédéric Vitart ◽  
David Anderson ◽  
Tim Stockdale

Author(s):  
Johnny C.L. Chan

As a tropical cyclone approaches land, its interaction with the characteristics of the land (surface roughness, topography, moisture availability, etc.) will lead to changes in its track as well as the rainfall and wind distributions near its landfall location. Accurate predictions of such changes are important in issuing warnings and disaster preparedness. In this chapter, the basic physical mechanisms that cause changes in the track and rainfall distributions when a tropical cyclone is about to make landfall are presented. These mechanisms are derived based on studies from both observations and idealized simulations. While the latter are relatively simple, they can isolate the fundamental and underlying physical processes that are inherent when an interaction between the land and the tropical cyclone circulation takes place. These processes are important in assessing the performance of the forecast models, and hence could help improve the model predictions and subsequently disaster preparedness.


Author(s):  
Alexandra N. Ramos‐Valle ◽  
Enrique N. Curchitser ◽  
Cindy L. Bruyère

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