[8] In the north Atlantic and the northeastern Pacific oceans,
tropical waves move along the axis of the ITCZ causing an increase in thunderstorm activity, and under weak vertical wind shear, these clusters of thunderstorms can become tropical cyclones.
Not exact matches
Brian McNoldy, a meteorologist at Colorado State University who maintains a useful Web site on
tropical storms in the Atlantic Ocean, has distributed an alert about a particularly noteworthy
wave of low pressure
moving west from Africa that appears likely to become a hurricane within a week.
It can not account for the huge volume of leftover warm water that's below the surface and returned to the West Pacific and into the eastern
tropical Indian Ocean via off - equatorial slow -
moving Rossby
waves.
Extratropical cyclones have three stages of expansion: the developing stage, in which an undulating
wave develops along the front; the mature stage, in which sinking cold air sweeps equatorward west of the surface low - pressure centre and ascending warm air
moves poleward east of the cyclone; and the occluded stage, in which the warm air is entrained within and
moved above the polar air and becomes separated from the source region of the
tropical air.
A
tropical wave was along 39 west, south of 20 north,
moving west at 10 - 15 knots.
Coincidentally, after a strong East Pacific El Niño, it takes a slow
moving Rossby
wave about 6 months to return leftover warm water from the eastern to the western
tropical Pacific.