「Convection」の共起表現(1語右で並び替え)

「Convection」の共起表現一覧(1語右で並び替え)

Convection

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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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