<\/p>\n
+ This convection<\/strong> generates electric currents which in turn give rise to magnetic fields.\n<\/p>\n <\/p>\n + The system lost its deep convection<\/strong> and by the afternoon of September 30, Melissa degenerated into a remnant low as thunderstorm activity decreased.\n<\/p>\n <\/p>\n + On September 21 the low crossed southern Florida and emerged into the Gulf of Mexico, and as it moved across the warm waters of the region the low began to re-acquire tropical characteristics; the low-level circulation became increasingly better defined, and convection<\/strong> redeveloped over the center.\n<\/p>\n <\/p>\n + The idea is that the star, even at luminosities below the Eddington limit, would have insufficient heat convection<\/strong> in the inner layers, resulting in a density inversion potentially leading to a massive explosion.\n<\/p>\n + Large convection<\/strong> currents in the asthenosphere transfer heat to the surface, where plumes of less dense magma break apart the plates at the spreading centers.\n<\/p>\n <\/p>\n + The NHC, however, decided the convection<\/strong> was too ephemeral to justify classification as a tropical depression and the TCFA was discontinued.\n<\/p>\n <\/p>\n + On August 14, a closed low-level circulation nearly developed to the east of Key Largo, Florida, but because of the deep convection<\/strong> remaining to the north over the mid-level center, it was weakened.\n<\/p>\n <\/p>\n + Their movement is driven by the convection<\/strong> currents in the magma.\n<\/p>\n <\/p>\n + Early on September 28, a rapid increase in convection<\/strong> and a well-organized outflow pattern allowed the low to develop into Tropical Depression Fourteen while about 115 miles west-southwest of the southernmost Cape Verde Islands.\n<\/p>\n <\/p>\n + The wind field remained well-defined as it continued westward, and deep convection<\/strong> increased two days later along the northern end of the wave axis.\n<\/p>\n <\/p>\n + Originally, the system had a disorganized circulation and thunderstorm patterns, but later turned into a tropical depression after convection<\/strong> became more organized over the center.\n<\/p>\n <\/p>\n + On August 9, an area of convection<\/strong> formed just south of Jamaica in association with a trough of low pressure.\n<\/p>\n <\/p>\n + On November 2, wind shear started affecting the storm, and all convection<\/strong> was gone by the next day, when it was located roughly 520mi off the coast of Oregon.\n<\/p>\n <\/p>\n + In early December, a low moving to the west led to the formation of a broad surface Trough trough to the east of the northern ridge to its northeast, the trough tracked slowly westward, creating scattered convection<\/strong> and some turning.\n<\/p>\n <\/p>\n + When convection<\/strong> began to decrease, the National Hurricane Center stopped sending out advisories on August 1 when Chantal began to turn into an extratropical cyclone.\n<\/p>\n <\/p>\n + A small area of convection<\/strong> 600 miles southeast of Rio de Janeiro moved into an area of low wind shear and barely 26\u00b0C warm waters on February 23, 2006.\n<\/p>\n <\/p>\n + It was initially embedded in a trough trough, but gained convection<\/strong> and developed into a tropical depression about 775miles south of Honolulu on August 19.\n<\/p>\n <\/p>\n + Shortly after exiting the Florida coastline, Wilma began to re-intensify, The remaining convection<\/strong> continued to diminish, and early on October 26 Wilma turned into an extratropical cyclone while about 230miles southeast of Halifax Regional MunicipalityHalifax, Nova Scotia.\n<\/p>\n <\/p>\n + As the system rapidly continued westward, a lot of the convection<\/strong> stayed near the center of the upper-level low, preventing development of a closed surface circulation.\n<\/p>\n <\/p>\n + Early on August 3, strong wind shear over Chris removed the deep convection<\/strong> from the low level circulation, while a building ridge ridge to its north turned the storm towards the west into an area of drier air.\n<\/p>\n <\/p>\n + The convection<\/strong> and strengthening continued and maintained itself as it moved away from Jalisco.\n<\/p>\n <\/p>\n + On August 9, it created convection<\/strong> when it was passing underneath a cold-core upper-level low.\n<\/p>\n <\/p>\n + Low amounts of wind shear and favorable outflow allowed strong deep convection<\/strong> to develop and persist near the center, and by 1800Coordinated Universal TimeUTC on September 2 the system developed into Tropical Depression Nine about 450miles southwest of Praia, Cape Verde.\n<\/p>\n <\/p>\n + A tropical wave, which had also created Tropical Depression Six, combined itself with an upper-level low pressure area to create an area of deep convection<\/strong> near Hispaniola on July 23, 2003.\n<\/p>\n <\/p>\n + The system stayed a tropical depression for 24hours before convection<\/strong> increased.\n<\/p>\n <\/p>\n + Periodically, a surge of intensely dry air known as the Saharan Air Layer is entrained behind a tropical wave, resulting in cloudless or nearly cloudless skies as convection<\/strong> is limited by the dry layer inversion.\n<\/p>\n <\/p>\n + Despite moderate wind shear, convection<\/strong> soon wrapped around the southeastern side of the low-level circulation.\n<\/p>\n <\/p>\n + After a quick burst of convection<\/strong> during the night, thunderstorm clouds inside the depression started to disappear by 3:00 am EDT.\n<\/p>\n <\/p>\n + At first, the depression moved west-northwest at about 13 mph, and most of the convection<\/strong> from the storm was separated from the center.\n<\/p>\n <\/p>\n + On August 13, while located near the northwestern Bahamas, an increase in convection<\/strong> made the upper-level low building downwards to the middle levels of the troposphere, which caused the development of an upper level anticyclone.\n<\/p>\n <\/p>\n + Holmes showed us that thermal convection<\/strong> currents were strong enough to move large land masses, which contributed to Alfred Wegener’s theory of continental drift or theory of Plate tectonics.\n<\/p>\n <\/p>\n + Continuing west because of a ridge, Eta slowly organized throughout the day as cold convection<\/strong> began to form on top of its center.\n<\/p>\n <\/p>\n + A burst of convection<\/strong> allowed Katrina to become the fifth hurricane of the 2005 season on August 25, only two hours before it made landfall around 6:30 p.m.\n<\/p>\n <\/p>\n + By six hours after development, the depression had of a somewhat exposed low-level center with deep convection<\/strong> taking up most of the northeastern semicircle.\n<\/p>\n <\/p>\n + This vigorous atmospheric convection<\/strong> also causes the general atmospheric circulation.\n<\/p>\n <\/p>\n + The next morning, it had a small amounts of convection<\/strong> near the center and well-defined bands, and the system, either a weak tropical storm or a strong tropical depression, likely reached its peak.\n<\/p>\n <\/p>\n + He proposed in 1931 that the Earth’s mantle contained convection<\/strong> cells that dissipated radioactive heat and moved the crust at the surface.\n<\/p>\n <\/p>\n + An area of persistent convection<\/strong> over the Caroline Islands was first noted in the Significant Tropical Weather Advisory on November 6.\n<\/p>\n <\/p>\n + On September 21, an area of convection<\/strong> formed in the western Caribbean Sea associated with a trough of low pressure.\n<\/p>\n <\/p>\n + On September 21, an area of convection<\/strong> developed in the western Caribbean Sea in association with a trough of low pressure.\n<\/p>\n <\/p>\n + The Grashof number represents forced convection<\/strong> in a heat transfer system.\n<\/p>\n <\/p>\n + The circulation became better organized as convection<\/strong> modestly increased over the center, and within 6hours of its formation, the system turned into a tropical depression.\n<\/p>\n <\/p>\n + As it moved quickly westward, the convection<\/strong> organized and developed into rainbands\u2013bands of showers and thunderstorms that move in a spiral direction towards the center of the storm\u2013and late on September 1 meteorologists began tracking the system using the Dvorak technique.\n<\/p>\n <\/p>\n + Because of Milwaukee’s proximity to Lake Michigan, a convection<\/strong> current forms around mid-afternoon in light wind, resulting in the so-called “lake breeze” \u2013 a smaller scale version of the more common sea breeze.\n<\/p>\n <\/p>\n + Slowly moving northwestward through Texas, Tropical Depression Erin managed to keep an area of convection<\/strong> near the center, with its widespread, but scattered rainbands dropping moderate to heavy precipitation.\n<\/p>\n <\/p>\n + However early in the morning of August 22 under highly favorable upper-level conditions, convection<\/strong> quickly increased and the system became Tropical Depression Eleven about 110miles east of Veracruz, Mexico.\n<\/p>\n <\/p>\n + As the sun sets, the convection<\/strong> current reverses and an offshore flow ensues causing a land breeze.\n<\/p>\n <\/p>\n + Some tropical or subtropical areas, such as the Philippines or south China are greatly affected by convection<\/strong> cells along a trough.\n<\/p>\n <\/p>\n + In spite of a decrease in convection<\/strong> shortly after forming, the large depression remained well organized, with a 575 mile wide wind field.\n<\/p>\n <\/p>\n + Shortly after its peak, dry air rapidly removed the convection<\/strong> and caused the eye to be gone, causing Eta to weaken back into a tropical storm at 18:00UTC.\n<\/p>\n <\/p>\n + The calculation makes use of convection<\/strong> in a viscous fluid as well as radioactivity, so it combines Perry’s idea with the effect of radioactivity, even though Perry’s contribution had been forgotten.\n<\/p>\n <\/p>\n + An area of low pressure formed on September 27 near Cape Verde in association with the wave, and convection<\/strong> slowly increased as a result of the low.\n<\/p>\n <\/p>\n + Contact convection<\/strong> starts near the terrain.\n<\/p>\n <\/p>\n + By August16, convection<\/strong> associated with Gert had mostly dissipated and whether or not the system retained a closed surface low was ambiguous.\n<\/p>\n <\/p>\n + Late on July 30, it was upgraded to a tropical depression, the third of the season, after developing deep convection<\/strong> near the center for most of the day.\n<\/p>\n <\/p>\n + But the convection<\/strong> that was associated with the depression went away and the whole structure of the storm started to get worse.\n<\/p>\n <\/p>\n + On September 7, convection<\/strong> developed over and to the west of the center for the first time in its duration.\n<\/p>\n <\/p>\n + Deep convection<\/strong> was slow to form that day since the system remained over cold waters that had upwelled in the wake of Hurricanes Gordon and Helene.\n<\/p>\n <\/p>\n + Less than a day later, when convection<\/strong> started to rapidly organize around the storm’s center, and a well-defined rain band at the northwest side of the storm, JTWC upgraded it to a typhoon.\n<\/p>\n <\/p>\n![\"In](\"https:\/\/englishteststore.net\/blog\/wp-content\/uploads\/2021\/09\/In-sentence-use-of-convection.jpg\" "\\"In")
Example sentences of “convection”:<\/h2>\n
+ Large convection<\/strong> currents in the asthenosphere transfer heat to the surface, where plumes of less dense magma break apart the plates at the spreading centers.\r\n
+ The NHC, however, decided the convection<\/strong> was too ephemeral to justify classification as a tropical depression and the TCFA was discontinued.\r\n
<\/pre>\nMore in-sentence examples of “convection”:<\/h2>\n
+ The convection<\/strong> and strengthening continued and maintained itself as it moved away from Jalisco.\r\n
+ On August 9, it created convection<\/strong> when it was passing underneath a cold-core upper-level low.\r\n
+ Low amounts of wind shear and favorable outflow allowed strong deep convection<\/strong> to develop and persist near the center, and by 1800Coordinated Universal TimeUTC on September 2 the system developed into Tropical Depression Nine about 450miles southwest of Praia, Cape Verde.\r\n
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