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Modelling the Extratropical Transition of Tropical Cyclones and Its Downstream Impact

2011
Tropical cyclones that move polewards may undergo extratropical transition (ET) and interact with the midlatitude flow. The presence of a tropical cyclone undergoing ET is often accompanied by low predictability for the Atlantic-European and Northwest-American sector, where the weather patterns can be significantly altered by an ET event.
Grams, C. M., Jones, S. C.
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Topic 2.0: Tropical cyclone formation and extratropical transition

2015
In this section, progress since ITWC-VI on research, observations and forecasting of tropical cyclone formation and extratropical transition is summarized. While tropical cyclone formation and extratropical transition are stages at opposite ends of the tropical cyclone lifecycle, significant lack of understanding remains in relation to processes ...
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A Global View of the Extratropical Tropopause Transition Layer From Atmospheric Chemistry Experiment Fourier Transform Spectrometer O3, H2O, and CO

Journal of Geophysical Research D: Atmospheres, 2009
Chris D Boone   +2 more
exaly  

On the Role of a Rossby Wave Train During the Extratropical Transition of Hurricane Helene (2006)

Quarterly Journal of the Royal Meteorological Society, 2013
Florian Pantillon   +2 more
exaly  

Large-Scale Factors in Tropical and Extratropical Cyclone Transition and Extreme Weather Events

Annals of the New York Academy of Sciences, 2008
Ian Simmonds, Alexandre Bernardes Pezza
exaly  

The Extratropical Transition of Hurricane Irene (1999): A Potential-Vorticity Perspective

Quarterly Journal of the Royal Meteorological Society, 2004
Suzanne Gray   +2 more
exaly  

Predictability associated with the downstream impact of the extratropical transition of tropical cyclones

2012
Since an extratropical transition (ET) of a decaying tropical cyclone (TC) often results in a fast-moving, rapidly developing extratropical cyclone and amplification of synoptic-scale systems far downstream, proper forecasting of ET events is critical to forecast accuracy over large ocean regions.
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