[James P. Kossin, Kerry A. Emanuel and Gabriel A. Vecchi, The poleward migration of the location of tropical
cyclone maximum intensity] Researchers looked at the global record of tropical cyclones since the 1970s.
Not exact matches
The researchers also cite previous research showing that over the past 30 years, the location where tropical
cyclones reach their
maximum intensity has shifted away from the equator and toward the poles.
According to the latest IPCC report, «tropical
cyclone frequency is likely to decrease or remain unchanged over the 21st century, while
intensity (i.e.
maximum wind speed and rainfall rates) is likely to increase.»
This leaves tropical
cyclone forecasters, who are ultimately responsible for recording TC tracks and
intensities (i.e.
maximum wind speeds), with a challenging problem.
No Category 5 was observed until 1920 or so; with poorer observations, could the
maximum intensity of
cyclones have been missed (seems like it)?
The extension of
maximum cyclone intensity scales Greg Lade proposes has long been embodied in the Modified Beaufort Scale employed by cruising sailors the world over:
Under this scenario, peak precipitation rates are likely to increase by 25 % as a result of increases in
maximum tropical
cyclone wind
intensities, which in turn cause higher storm surges.
When comparing a category 5 and a category 6 tropical
cyclone of the same duration, given the difference in their
intensity characterized by
maximum wind speed, the kinetic energy of the category 6 storm of 165 to 185 knots would be 139 % — 175 % higher than the category 5 storm of 140 knots, Lin said.
DeMaria, M., and Kaplan, J., 1994: Sea Surface Temperature and the
Maximum Intensity of Atlantic Tropical
Cyclones.
The method is a way to estimate the
maximum surface sustained wind over one minute which is the most significant data of a
cyclone intensity.
RE # 150 The most important parameter is the
maximum surface sustained wind when you are analysing the tropical
cyclones intensity with the satellite pictures.
DeMaria and Kaplan (1994) show that only 20 % of the
cyclones of the North Atlantic reach 80 % or more theirs potential
maximum intensity, case in which the
intensity reached by a
cyclone is in balance with the temperature of surface of the ocean in the absence of dynamic stresses in the atmosphere.
Recent work (Kossin et al. 2014; see GFDL Research Highlight) indicates that the latitude at which the
maximum intensity of tropical
cyclones occurs has expanded poleward globally in recent decades, although the causes for this have not been firmly established and a significant change was not seen in the Atlantic basin statistics.
This is mainly because the area of
maximum cyclone intensity has moved nearer the East Asian coastline, the researchers believe, boosting
cyclone intensity at landfall — when the centre of the storm hits the coast — over easten China, Korea and Japan.
Following the general concepts outlined by Emanuel (1987), Holland (1997) has derived an alternative thermodynamic approach to estimate
maximum potential
intensity of tropical
cyclones.