「convection」の共起表現(1語右で並び替え)

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共起表現

「convection」の共起表現一覧(1語右で並び替え)

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By October 31 the system had acquired	convection, a warmer-than-normal core, and an eye-like
ce high and warmer temperatures aloft due to	convection, a mid-level mesohigh forms behind the leadi
under condition of zero-gravity and reduced	convection aboard the Skylab are ~10 times larger than
tsa is traced to the formation of an area of	convection about 185 km (115 miles) east of Yap in late
Typhoon Warning Center identified an area of	convection about 870 miles (1,400 km) east of Iwo Jima
outh of Wake Island on August 2. Little deep	convection accompanied the weak system despite being si
The system maintained scattered deep	convection across offshore waters and environmental con
ear and low-level helicity produced moderate	convection across central Florida in association with t
Later that day, the	convection again decreased, leaving the circulation exp
Natural	convection, aided by the wind, keeps the panels operati
A brief burst in	convection allowed Blanca to maintain 40 mph (65 km/h)
An area of	convection along the wave tracked westward to the south
rd generated minimal amounts of intermittent	convection along the southeastern portion of its circul
g features developed around the area of deep	convection, and the system was expect to develop furthe
the water heater tank, but prevent unwanted	convection and heated water to flow out of the tank.
er became separated from the area of deepest	convection, and Arthur maintained its peak intensity as
ation became displaced from the area of deep	convection, and Kay was reduced to a small low-level sw
Beatriz managed to produce modest amounts of	convection and after a burst of deep convection during
The system quickly developed deep	convection and a low-level circulation, and on Septembe
ely 14 mph (23 km/h) with no associated deep	convection and a weak low-level inverted-V curvature.
wave continued to develop moderate to strong	convection, and on August 27 a 1012 mbar (hPa; 29.88 in
eas to the sun/shade, and through radiation,	convection and conduction, heat exchange occurs.
to improve heat transfer by	convection and radiation, gases must move in the workin
Although deep	convection and banding features increased, mid-level dr
sing the center to separate from the deepest	convection, and restricting the outflow to all areas ar
ombated in four ways: radiation, conduction,	convection, and evaporation.
circulation was at the northern edge of the	convection, and Kay only reached winds of 45 mph (75 km
excess of 90 mph (145 km/h) within the deep	convection, and late on November 17 Gordon attained hur
eat dissipation (primarily by conduction and	convection and to a lesser extent by radiation).
hange in a rotary kiln may be by conduction,	convection and radiation, in descending order of effici
t southwest of Barry also helped to increase	convection and strengthen the storm.
orm while producing sporadic amounts of deep	convection, and on September 4 the banding structure im
	Convection and banding features organized around a deve
oss the tropical Atlantic Ocean with minimal	convection, and subsequent to moving through the southe
f Cuba, the system slowed down to regenerate	convection, and it re-developed into a tropical depress
caused by sun heating the ground leading to	convection and to showers and thunderstorms.
rated may be able to resist expulsion by the	convection and later yield the observed global-scale fi
an on July 29 and gained in organization and	convection, and organized into Tropical Storm Barry on
ens are ovens for high-forced volume thermal	convection applications.
number of patents, many with respect to heat	convection, are on his name.
ikely as easterly wind shear was causing the	convection around the storm to become disorganized and
The storm featured relatively deep	convection around an eye-like feature.
rm waters of the Gulf Stream, where bands of	convection around the center began to organize.
Deep	convection around the eyewall began to diminish, and Fa
The depression maintained an area of deep	convection around the center of circulation and was loc
Due to the lack of	convection around the center of the depression, it was
lation briefly became involved with the deep	convection as it accelerated northeastward, though as i
e circulation accelerated away from the deep	convection as it passed a short distance south of Acapu
Deep	convection associated with the storm diminished and the
By July 7, most of the deep	convection associated with Blanca had dissipated, and t
at NHC noted "...there is no longer any deep	convection associated with its circulation...", althoug
to the Pacific Ocean on September 10 and the	convection associated with it gradually increased.
on stellar structure involving radiation and	convection, at the same time as Ludwig Biermann but ind
study of three-dimensional spherical mantle	convection at 10(8) Rayleigh number: Effects of depth-d
known for work on air pollution, atmospheric	convection, atmospheric boundary layers, and numerical
The storm maintained a small area of deep	convection, averaging 9.2 miles (14.8 km) in diameter,
tensity for about 24 hours, during which its	convection became shifted to the north of the circulati
nued weakening took place on September 11 as	convection became fully disorganized.
On August 31,	convection became more concentrated to the south of the
espite moving through a dry environment, its	convection became organized as an anticyclone developed
Adolph deteriorated into a tropical storm as	convection became exposed from the increasingly elongat
The	convection became better organized, and with good diffl
That evening, Barry began to weaken as	convection began to decrease.
After entering the Caribbean Sea on July 26,	convection began to come together two days later.
By October 1,	convection began to develop near the center of the syst
	Convection began to intensify and consolidate later tha
On September 18, the	convection began contracting and organizing, gradually
a surface low pressure system developed, and	convection began to organize into slightly curved bands
as the circulation strengthened, despite the	convection being disorganized due to the shear.
storm was classified subtropical, due to the	convection being located east of the center.
asured under the same conditions as the heat	convection but with a (hypothetically) stagnant (or mot
deteriorated with a significant decrease in	convection; by early on May 10 much of the associated w
The wind shear calmed on September 26, and	convection came back together.
It is the sinking limb of a	convection cell.
hf is the	convection coefficient of the fin
ern Gulf of Mexico, and despite disorganized	convection conditions favored further development.
Gradual development took place as	convection consolidated around the center of circulatio
Deep	convection consolidated around the center of circulatio
rge cyclone, Fausto slowly intensified, with	convection consolidating around the center the next day
	Convection continued to organize, and the tropical wave
Deep	convection continued to build over the center due to lo
	Convection continued increasing, and it intensified to
riorated into a remnant low shortly after as	convection continued to dissipate around the storm.
	Convection continued to consolidate around the low-leve
sification began on the disturbance, and the	convection continued to organize.
ive-fire, radiant heat cooking, and hot-air,	convection cooking, and smoking by the fat and food jui
Vigorous core	convection coupled with rotation clearly admits magneti
d the mechanism of plate tectonics through a	convection current in the Earth's molten interior.
ing of a Thiele tube with red arrows showing	convection current
d bottom of the rotor produces a very strong	convection current.
nding of tectonic plate motions by exploring	convection currents in the Earth's mantle with radial m
Most heat from a domestic radiator is as	convection currents of heated air.
drawn up toward the surface of the Earth by	convection currents the mineral breaks down and release
as intended to help scientists to understand	convection currents within the Earth's mantle.
s of magma from the Earth's mantle, and that	convection currents within the mantle were continuously
nding of tectonic plate motions by exploring	convection currents in the Earth's mantle with seismolo
When drafted into the upper atmosphere by	convection currents, the hailstones acquire a rapid rot
steam boilers the circulation of water is by	convection currents, which are set up during the heatin
Later that day,	convection decreased markedly, and early on August 27 i
inent subtropical structure: bands of curved	convection deepened in the northern and eastern quadran
as the eye decreased in size and its eyewall	convection deepened.
On July 13, deep	convection developed near a mid-level circulation along
into the circulation of the storm, a band of	convection developed along a frontal boundary stretchin
An area of	convection developed along the wave axis, several hundr
approached the Pacific Ocean, a new area of	convection developed south of the original circulation
the Gulf Stream, a small but intense area of	convection developed over the center, with winds increa
An area of	convection developed on May 11, and the next day the In
A scattered area of strong	convection developed, partially in association with the
ransfer and mass transfer problems involving	convection, diffusion and surface reactions.
y, Tropical Storm Edouard began to weaken as	convection diminished from vertical shear and dry air,
However, the banding was short-lived, deep	convection diminished, and satellite microwave imagery
us outflow became weak in all directions and	convection diminished.
for about a day before the minimal amount of	convection diminished.
Because the storm was weak and the	convection disorganized when it hit Somalia, no damage
Ocean, and by late on August 22 most of the	convection dissipated from the system.
By September 6 the remaining	convection dissipated, and Edouard dissipated while bec
When Ar >> 1, natural	convection dominates and when Ar << 1, forced convectio
	Convection draws air in through the bottom orifices and
ation was exposed on the western edge of the	convection due to the storm's quick forward motion and
ation was initially located east of the main	convection, due to the presence of wind shear.
e following reference shows the liquid phase	convection during lithium niobate (LiNbO3) fiber pullin
	Convection eventually increased on September 7, as the
small low level circulation center with deep	convection flaring to the northeast of the center.
dissertation is "Transient natural and mixed	convection flows and transport adjacent to an ice surfa
used to characterize heat transfer in forced	convection flows.
em acquired enough circulation and organized	convection for it to be designated Tropical Depression
d weak; having been without significant deep	convection for 18 hours, the National Hurricane Center
organized enough with sufficiently organized	convection for the National Hurricane Center to classif
s, and the center of circulation lacked deep	convection for several days.
A small cyclone, a burst of deep	convection formed at around the same time, and was said
res-spiral rain showers of convection-as its	convection formed into a central area of deep convectio
inued forecasting difficulty, a burst of new	convection formed east of the center early on May 28, a
on April 22 the wind shear again removed the	convection from the center.
s located within a large, persistent area of	convection from the Gulf of Mexico through the central
The	convection gradually increased and became better organi
The	convection gradually consolidated over a weak low-level
	Convection gradually increased over the warm waters, th
December 7 the JTWC reported that an area of	convection had been building around a rapidly developin
yphoon Warning Center, noted that an area of	convection had persisted approximately 370 nautical mil
C) reported that an area of deep atmospheric	convection had persisted for the last 48 hours about 73
By late on April 29,	convection had begun to rebuild, though immediate restr
Micathermic heaters produce both	convection heat and radiant heat, and are usually thinn
y generation minimization, scale analysis of	convection, heatlines and masslines, transition to turb
onfigurations, including clean rooms, forced	convection, horizontal airflow, inert atmosphere, natur
the Dvorak technique, as the loss of central	convection in transitioning tropical cyclones can cause
are evacuated to eliminate distortion due to	convection in the telescope that would otherwise be cau
Subsolidus	convection in icy bodies is a slow process with ice mot
The early onset of subsolidus	convection in the Callistoan interior could have preven
The	convection in the interior parts of Callisto may be lay
at motion of the MET, which causes movement (	convection) in the liquid electrolyte, can be converted
ion, these results contribute to modeling of	convection in the Earth's mantle by providing constrain
Eruptions occur suddenly following visible	convection in the pool, but are unpredictable.
Stellar physics: Numerical simulations of	convection in stellar atmospheres, determination of ste
Gonu developed from a persistent area of	convection in the eastern Arabian Sea on June 1.
D. A. Nield and A. Bejan,	Convection in Porous Media, Second Edition, Springer-Ve
n of zones of differing degrees of buoyancy (	convection) in the Earth's mantle.
Details of the subsolidus	convection in the ice is the main source of uncertainty
Deep	convection increased in coverage, though partially remo
On August 24,	convection increased as the wave passed through the Les
On August 14,	convection increased northwest of the center and became
	Convection increased near the center despite the shear,
Early on July 15,	convection increased over the center and developed an o
	Convection increased early the next day, and a Hurrican
	Convection increased late on August 20, although it ini
Its	convection increased as it turned westward, and it was
rn Pacific Ocean on August 16, at which time	convection increased along the wave axis.
ransitioned into a tropical depression after	convection increased over the center.
the developing low was nearly stationary as	convection increased.
pical storm status early on January 28, with	convection increasing further.
lation was still dislocated from the deepest	convection, indicative of the presence of wind shear.
ard Islands and eastern Puerto Rico, and its	convection initially remained disorganized.
	Convection is the mechanism believed to be responsible
Practically, its value determines whether	convection is free or forced.
ce the low heat transfer coefficient for air	convection is adequate for a low heat flux.
The region of vigorous	convection is slightly prolate in shape, extending fart
er of circulation became separated from deep	convection, leading to the typhoon being downgraded to
ning of August 11, a sudden redevelopment in	convection led forecast models to re-intensify Kika onc
next day, the depression, devoid of any deep	convection, made landfall near Isla Altamura in northwe
n helium fusion comes to an end at the core,	convection mixes the products of the CNO cycle, resulti
eled as the system rapidly degenerated, with	convection mostly dissipating and an exposed low.
ue to its large circulation and lack of deep	convection near the center.
low pressure area to develop an area of deep	convection near Hispaniola on July 23, 2003.
For free	convection near a vertical wall, this number is
ology, were monitoring an organizing area of	convection near the southeast coast of Brazil.
The eastern system developed organized	convection near its center, and developed into Tropical
	Convection near the center of the storm waned, although
ive envelopes except for very thin shells of	convection near the surface.
subsidence and drier air; as a result, deep	convection near the center markedly decreased.
ck smoker environment which is the result of	convection of ocean water through the fractured basalts
allowness of the continental shelf restricts	convection of cooling water
When analyzing potentially mixed	convection of a liquid, the Archimedes number parametri
cal upper troposphere has been linked to the	convection of water vapor and ice.
initially moderate wind shear kept the deep	convection on the periphery of the consolidating low-le
ath, which heats the walls of the reactor by	convection or conduction.
to explain the asymmetry in supernova using	convection or mechanical instabilities in the presupern
ith buoyancy driven flow (also known as free	convection or natural convection).
Lacking deep	convection or a well defined center, the wave continued
ength of a vertical plate undergoing natural	convection, or the diameter of a sphere.
The system was associated with disorganized	convection, or thunderstorms, and moved generally south
s circulated around the incubator by natural	convection or by using a fan to keep both the CO2 level

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共起表現

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「convection」の共起表現一覧(1語右で並び替え)