In climate research, the intensity of a storm track is often measured by the band pass filtered
eddy kinetic energy, geopotential variance or related variables.
Ocean surface cooling, in the North Atlantic as well as the Southern Ocean, increases tropospheric horizontal temperature gradients,
eddy kinetic energy and baroclinicity, which drive more powerful storms.
«
Both the eddy kinetic energy and the dry mean available potential energy have a maximum for a climate close to that of present day Earth and are smaller in much warmer and much colder climates»
This is shown by the change of zonal mean temperature and
eddy kinetic energy in our simulations with and without ice melt.
The researchers also noted a statistically significant relationship between times of low
eddy kinetic energy and extremely high temperature anomalies — for example, the sweltering Russian heat wave of 2010.
Coumou has taken the story forward, analyzing existing climate models to track the future of
eddy kinetic energy over the 21st century.
Not exact matches
«The increase in
kinetic energy of these
eddies actually only became apparent a few years after a strong SAM event.»
Eddies can grow by extracting kinetic energy from a steady - state flow pattern, if there is an elongated horizontal maximum or minimum in potential vorticity; however, the shear can tilt those eddies in such a way that the eddies give back their kinetic e
Eddies can grow by extracting
kinetic energy from a steady - state flow pattern, if there is an elongated horizontal maximum or minimum in potential vorticity; however, the shear can tilt those
eddies in such a way that the eddies give back their kinetic e
eddies in such a way that the
eddies give back their kinetic e
eddies give back their
kinetic energy.
Embedded within the mean flow is a variety of
eddy structures that not only put
kinetic energy into circulation but also carry heat and other important properties, such as nutrients for biological systems.
The
kinetic energy generated by horizontal pressure gradients dissipates in smaller - scale
eddies and ultimately converts to heat.