How to use in-sentence of “convection”:
+ The low produced discontinuous amounts convection until it was absorbed by a weather frontfrontal zone late on October 5 northeast of the Leeward Islands.
+ This convection generates electric currents which in turn give rise to magnetic fields.
+ The system lost its deep convection and by the afternoon of September 30, Melissa degenerated into a remnant low as thunderstorm activity decreased.
+ 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 redeveloped over the center.
+ The idea is that the star, even at luminosities below the Eddington limit, would have insufficient heat convection in the inner layers, resulting in a density inversion potentially leading to a massive explosion.
Example sentences of “convection”:
+ Large convection currents in the asthenosphere transfer heat to the surface, where plumes of less dense magma break apart the plates at the spreading centers.
+ The NHC, however, decided the convection was too ephemeral to justify classification as a tropical depression and the TCFA was discontinued.
+ On August 14, a closed low-level circulation nearly developed to the east of Key Largo, Florida, but because of the deep convection remaining to the north over the mid-level center, it was weakened.
+ Their movement is driven by the convection currents in the magma.
+ Early on September 28, a rapid increase in convection 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.
+ The wind field remained well-defined as it continued westward, and deep convection increased two days later along the northern end of the wave axis.
+ Originally, the system had a disorganized circulation and thunderstorm patterns, but later turned into a tropical depression after convection became more organized over the center.
+ On August 9, an area of convection formed just south of Jamaica in association with a trough of low pressure.
+ On November 2, wind shear started affecting the storm, and all convection was gone by the next day, when it was located roughly 520mi off the coast of Oregon.
+ 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 and some turning.
+ When convection began to decrease, the National Hurricane Center stopped sending out advisories on August 1 when Chantal began to turn into an extratropical cyclone.
+ A small area of convection 600 miles southeast of Rio de Janeiro moved into an area of low wind shear and barely 26°C warm waters on February 23, 2006.
+ It was initially embedded in a trough trough, but gained convection and developed into a tropical depression about 775miles south of Honolulu on August 19.
+ Shortly after exiting the Florida coastline, Wilma began to re-intensify, The remaining convection continued to diminish, and early on October 26 Wilma turned into an extratropical cyclone while about 230miles southeast of Halifax Regional MunicipalityHalifax, Nova Scotia.
+ As the system rapidly continued westward, a lot of the convection stayed near the center of the upper-level low, preventing development of a closed surface circulation.
+ Early on August 3, strong wind shear over Chris removed the deep convection 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.
+ Large convection currents in the asthenosphere transfer heat to the surface, where plumes of less dense magma break apart the plates at the spreading centers.
+ The NHC, however, decided the convection was too ephemeral to justify classification as a tropical depression and the TCFA was discontinued.
More in-sentence examples of “convection”:
+ The convection and strengthening continued and maintained itself as it moved away from Jalisco.
+ On August 9, it created convection when it was passing underneath a cold-core upper-level low.
+ Low amounts of wind shear and favorable outflow allowed strong deep convection 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.
+ The convection and strengthening continued and maintained itself as it moved away from Jalisco.
+ On August 9, it created convection when it was passing underneath a cold-core upper-level low.
+ Low amounts of wind shear and favorable outflow allowed strong deep convection 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.
+ 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 near Hispaniola on July 23, 2003.
+ The system stayed a tropical depression for 24hours before convection increased.
+ 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 is limited by the dry layer inversion.
+ Despite moderate wind shear, convection soon wrapped around the southeastern side of the low-level circulation.
+ After a quick burst of convection during the night, thunderstorm clouds inside the depression started to disappear by 3:00 am EDT.
+ At first, the depression moved west-northwest at about 13 mph, and most of the convection from the storm was separated from the center.
+ On August 13, while located near the northwestern Bahamas, an increase in convection made the upper-level low building downwards to the middle levels of the troposphere, which caused the development of an upper level anticyclone.
+ Holmes showed us that thermal convection currents were strong enough to move large land masses, which contributed to Alfred Wegener’s theory of continental drift or theory of Plate tectonics.
+ Continuing west because of a ridge, Eta slowly organized throughout the day as cold convection began to form on top of its center.
+ A burst of convection 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.
+ By six hours after development, the depression had of a somewhat exposed low-level center with deep convection taking up most of the northeastern semicircle.
+ This vigorous atmospheric convection also causes the general atmospheric circulation.
+ The next morning, it had a small amounts of convection near the center and well-defined bands, and the system, either a weak tropical storm or a strong tropical depression, likely reached its peak.
+ He proposed in 1931 that the Earth’s mantle contained convection cells that dissipated radioactive heat and moved the crust at the surface.
+ An area of persistent convection over the Caroline Islands was first noted in the Significant Tropical Weather Advisory on November 6.
+ On September 21, an area of convection formed in the western Caribbean Sea associated with a trough of low pressure.
+ On September 21, an area of convection developed in the western Caribbean Sea in association with a trough of low pressure.
+ The Grashof number represents forced convection in a heat transfer system.
+ The circulation became better organized as convection modestly increased over the center, and within 6hours of its formation, the system turned into a tropical depression.
+ As it moved quickly westward, the convection organized and developed into rainbands–bands of showers and thunderstorms that move in a spiral direction towards the center of the storm–and late on September 1 meteorologists began tracking the system using the Dvorak technique.
+ Because of Milwaukee’s proximity to Lake Michigan, a convection current forms around mid-afternoon in light wind, resulting in the so-called “lake breeze” – a smaller scale version of the more common sea breeze.
+ Slowly moving northwestward through Texas, Tropical Depression Erin managed to keep an area of convection near the center, with its widespread, but scattered rainbands dropping moderate to heavy precipitation.
+ However early in the morning of August 22 under highly favorable upper-level conditions, convection quickly increased and the system became Tropical Depression Eleven about 110miles east of Veracruz, Mexico.
+ As the sun sets, the convection current reverses and an offshore flow ensues causing a land breeze.
+ Some tropical or subtropical areas, such as the Philippines or south China are greatly affected by convection cells along a trough.
+ In spite of a decrease in convection shortly after forming, the large depression remained well organized, with a 575 mile wide wind field.
+ Shortly after its peak, dry air rapidly removed the convection and caused the eye to be gone, causing Eta to weaken back into a tropical storm at 18:00UTC.
+ The calculation makes use of convection 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.
+ An area of low pressure formed on September 27 near Cape Verde in association with the wave, and convection slowly increased as a result of the low.
+ Contact convection starts near the terrain.
+ By August16, convection associated with Gert had mostly dissipated and whether or not the system retained a closed surface low was ambiguous.
+ Late on July 30, it was upgraded to a tropical depression, the third of the season, after developing deep convection near the center for most of the day.
+ But the convection that was associated with the depression went away and the whole structure of the storm started to get worse.
+ On September 7, convection developed over and to the west of the center for the first time in its duration.
+ Deep convection was slow to form that day since the system remained over cold waters that had upwelled in the wake of Hurricanes Gordon and Helene.
+ Less than a day later, when convection 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.
+ An area of convection first appeared on May4.
+ While at major hurricane status, Ivan kept very strong convection in its core with a well-defined eye.
+ The convection began to organize, and weather agencies to release the first Dvorak numbers on the system.
+ Banding and convection increased, and it became a tropical depression that night, 400 nautical miles south of Manzanillo, Mexico.
+ After becoming an extratropical cyclone, Chantal managed to keep scattered convection near its center, though its main area of convection and clouds moved to its north.
+ Atmospheric circulation, for example, is made by convection currents.
+ By early on October 17, the outer rainbands, which had previously controlled the structure of the cyclone, dissipated, while deep convection developed near and to the south of the center.
+ It is found above the convection zone.
+ The boundary between the SAL and the marine layer suppresses or “caps” any convection originating in the marine layer.