「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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