Exemplos de uso de Thunderstorm activity em Inglês e suas traduções para o Português
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It's a scale that meteorologists use to measure thunderstorm activity.
Thunderstorm activity is expected to continue, which will trigger extensive connective showers.
But down to the south for other folks besides Bridgton… you have got some showers and thunderstorm activity on the way.
Once in the Pacific, convection, areas of thunderstorm activity, and banding features began to form.
Convection gradually became better organized, with a well-defined band in its eastern semicircle and intermittent thunderstorm activity near the center.
The control tower informed the crew of the thunderstorm activity, in addition stating that there was water on the runway.
The National Hurricane Center(NHC) remarked upon the possibility for tropical cyclone development,as the wave had already been accompanied by a broad area of shower and thunderstorm activity.
Daniel quickly became better organized,exhibiting increased thunderstorm activity and banding features.
Some organization of shower and thunderstorm activity initially took place, but dry air soon impinged upon the system and imparted weakening.
London, situated in Southern(Southwestern) Ontario, has the most lightning strikes per year in Canada,averaging 34 days of thunderstorm activity per year.
By September 17,the system produced widespread thunderstorm activity over The Bahamas and western Atlantic Ocean.
The next day, thunderstorm activity increased and organized, though another hurricane hunters flight confirmed the system did not develop into a tropical cyclone.
Upon its designation,the depression consisted of a large area of thunderstorm activity, with curved banding features and expanding outflow.
By August 11, however, the thunderstorm activity became disorganized and limited, though the next day convection reformed by the time it was located about 650 mi(1050 km) east of the Lesser Antilles.
Later on August 11, the center of Etau became partially devoid of convection,with only a narrow band of shower and thunderstorm activity persisting to the southeast of the center.
There appears to be a 15-25 day cycle in thunderstorm activity along the ITCZ, which is roughly half the wavelength of the Madden-Julian oscillation MJO.
As it approached the coast of North Carolina, the center re-developed within the deep convection underneath the mid-level circulation,although increased northerly wind shear displaced the center of Gabrielle to the north of the thunderstorm activity.
Initially containing a poorly defined circulation and intermittent thunderstorm activity, the system transitioned into a tropical depression after convection increased over the center.
Tropical Storm Erika originated from a tropical wave accompanied by disorganized shower and thunderstorm activity that moved off the west coast of Africa, near the Cape Verde Islands, on August 25.
Rainfall in the wet season is mainly due to daytime heating which leads to diurnal thunderstorm activity within a pre-existing moist airmass, so the rain mainly falls in late afternoon and early evening in savannah and monsoon regions.
At the same time, banding features became better organized.[3] Later on September 5, the overall cloud pattern improved while thunderstorm activity condensed and deepened within the increasingly well-defined circulation.
Later on September 5, the overall cloud pattern improved while thunderstorm activity condensed and deepened within the increasingly well-defined circulation.
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.
Accumulations==Narrow zones where hail accumulates on the ground in association with thunderstorm activity are known as hail streaks or hail swaths, which can be detectable by satellite after the storms pass by.
The ITCZ is formed by vertical motion largely appearing as convective activity of thunderstorms driven by solar heating, which effectively draw air in; these are the trade winds.
Ionospheric plasma excitation happens because of solar activity, thunderstorms, use of scalar plasma weapons and HAARP and lately also when the Light forces are clearing the plasma anomaly.”.