Convallaria odorata

air-cooled flat-four

Convalescent hospital

*Aerocar
*Aerocar 2000
*Parajet Skycar
*Terrafugia Transition

Convection rain

Convair CV-990 Coronado

Convair Model 110

Convair CV-240-21 Turboliner

Convair CV-880-22-2

Convair Model 30

Convalidation of marriage

Convective inhibition

Convair C-131 Samaritan

Convair CV-340

Convair Model 106 Skycoach

* Airspeed Ambassador
* Vickers VC.1 Viking

Experimental VTOL fighter aircraft

plane

The Convair YB-60 was an American prototype bomber aircraft for the United States Air Force, canceled on 14 August 1952.

Convair XSM-74

prop

transport flying boat

Convair X-30

Convair Model 8-24

The Convair XB-53 was a proposed jet-powered medium bomber aircraft, designed by Convair for the United States Army Air Forces. With a radical tailless, forward-swept wing design, the aircraft appeared futuristic; however, the project was canceled before either of the two prototypes were completed.

*Convair B-36

Convair CV-240

Convair FY

Conval Regional High School

Crosley

Convallamarin

Convection currents

Convair CV-340-68

Convectional Precipitation

three

Convair L-13

Convair CV-240-4

Convair Model 7

Ted Hall

Convallaria prolificans

Convair XFY

Convallarin is a crystalline glucoside extracted from the Lily of the Valley plant (Convallaria majalis)It may be obtained from the alcoholic extract of the residue from which the convallamarin has been removed with water. The alcoholic solution is treated with lead acetate, the filtrate freed from lead by hydrogen sulfide, and crystallised by concentration. An aqueous solution froths like soap and water when shaken. By long boiling with diluted acids it is split up into glucose and convallaretin.

Convair CV-240-1

Convallaria

In fluid dynamics, convective mixing is the vertical transport of a fluid and its properties. In many important ocean and atmospheric phenomena, convection is driven by density differences in the fluid, e.g. the sinking of cold, dense water in polar regions of the world's oceans; and the rising of warm, less-dense air during the formation of cumulonimbus clouds and hurricanes.

Convection cooling

Convair R3Y

Convection, Rotation and Planetary Transits

Convair XB-46

Convalescence home

Convection rolls

United States of America

Convallatoxin

The Convair Model 116 ConvAirCar was a prototype roadable aircraft that was intended to exploit the post-war aviation market. The vehicle was further developed into the Convair Model 118, but neither type achieved production status.

Convallamarin is a crystalline glycoside extracted from Convallaria majalis.

Convair Model 58-9

Convair YF-102 Delta Dagger

Convair NB-36

Convair Peacemaker

Convallatoxin is a glycoside extracted from Convallaria majalis.

Allison YT40-A-6

Convair KINGFISH

The convective overturn model of supernovae was proposed by Bethe and Wilson in 1985, and received a dramatic test with SN 1987A, and the detection of neutrinos from the explosion. The model is for type II supernovae, which take place in stars more massive than 8 solar masses.When the iron core of a super massive star becomes heavier than electron degeneracy pressure can support, the core of the star collapses, and the iron core is compressed by gravity until nuclear densities are reached when a strong rebound sends a shock wave throughout the rest of the star and tears it apart in a large supernova explosion. The remains of this core will eventually become a neutron star. The collapse produces two reactions: one breaks apart iron nuclei into 13 helium atoms and 4 neutrons, absorbing energy; and the second produces a wave of neutrinos that form a shock wave. While all models agree that there is a convective shock, there is disagreement as to how important that shock is to the supernova explosion.In the convective overturn model, the core collapses faster and faster, exceeding the speed of sound inside the star, and producing a supersonic shock wave. This shock wave explodes outward until it stalls when it reaches the neutrinosphere, where the pressure of the star collapsing inward exceeds the pressure of the neutrinos radiating outwards. This point produces heavier elements as the neutrinos are absorbed.The stalling of the shock wave represents the supernova problem, because once stalled, the shock wave should not be "reenergized". The prompt convection model states that the shock wave will increase the luminosity of the neutrinos produced by the core collapse, and this increase in energy will start the shock wave going again. The neutron fingers model has instability near the core expel another wave of energized neutrinos which reenergizes the shock wave. The entropy convection model has matter falling inward from above the shock layer down to the gain radius, which would not increase neutrino luminosity, but would allow the shock wave to continue outwards.All of these models exhibit convective overturn in that they rely on a convection mechanism to re-energize the stalled shock wave and complete the supernova explosion.There are still open issues in both the convective models and in the more general core collapse model, which include not taking into account flavor mixing and mass of neutrinos, and the inability to model large explosions. Current models indicate that the collapse may occur more slowly than thought before, which would mean the shock wave would penetrate farther into the upper layers of the star. The proto-neutron star boosts neutrino luminosities, and the additional neutrinos emitted help re-energize the shock wave. These changes remove some, but not all, of the supernova problem, and strengthen the idea of convection being an important factor in supernova explosions.

Convective Outlook

Convallaria hybrida

* List of experimental aircraft
* List of fighter aircraft

nuclear turbojets

Convair RB-36H-10-CF Peacemaker

27 kN

Convallaria fruticosa

Convair F-7 Sea Dart

Westinghouse J46-WE-2

four

In meteorology, convective instability or stability of an air mass refers to its ability to resist vertical motion. A stable atmosphere makes vertical movement difficult, and small vertical disturbances dampen out and disappear. In an unstable atmosphere, vertical air movements (such as in orographic lifting, where an air mass is displaced upwards as it is blown by wind up the rising slope of a mountain range) tend to become larger, resulting in turbulent airflow and convective activity.

Convectional lifting

Convair P-92

Allison J33-A-29

changed

Convalescence is the gradual recovery of health and strength after illness or injury. It refers to the later stage of an infectious disease or illness when the patient recovers and returns to normal, but may continue to be a source of infection even if feeling better. In this sense, "recovery" can be considered a synonymous term. This also sometimes includes patient care after a major surgery, under which they are required to visit the doctor for regular check-ups.Convalescent care facilities are sometimes recognized by the acronym CCF.

air-cooled

The Convair Model 118 ConvAirCar (also known as the Hall Flying Automobile) was a prototype flying car of which two were built. Intended for mainstream consumers, two prototypes were built and flown. The first prototype was lost after a safe, but damaging, low fuel incident. Subsequently, the second prototype was rebuilt from the damaged aircraft and flown. By that time, little enthusiasm remained for the project and the program ended shortly thereafter.

17.8 kN

Convair XP5Y

National Museum of the United States Air Force in Dayton, Ohio

Convair F-102A-80-CO Delta Dagger

A convection oven (also known as a fan-assisted oven or simply a fan oven) is an oven that has fans to circulate air around food.Convection ovens distribute heat evenly around the food, removing the blanket of cooler air that surrounds food when it is first placed in an oven and allowing food to cook more evenly in less time and at a lower temperature than in a conventional oven.

Convective outlooks

Convair

Convallaria commutata

Convair Charger

Convair CV-440-62

Convective Heat Transfer

at 29,250 ft

Convection oven

Convair Model 36

Allison T40-A-10

Convection current

jet

23.1 kN

*Bristol Brabazon
*Lockheed R6V Constitution
*Saunders-Roe Princess
*Tupolev ANT-20

Convectional storm

Convair XB-53

The Convective Boundary layer (CBL), also known as the daytime Planetary boundary layer, is the part of the atmosphere most directly affected by solar heating of the earth's surface.This layer extends from the earth surface to a capping inversion that typically locates at a height of 1–2 km by midafternoon over land. Below the capping inversion (10-60% of CBL depth, also called entrainment zone in the daytime), CBL is divided into two sub-layers: mixed layer (35-80% of CBL depth) and surface layer (5-10% of CBL depth). The mixed layer, the major part of CBL, has a nearly constant distribution of quantities such as potential temperature, wind speed, moisture and pollutant concentration because of strong buoyancy generated convective turbulent mixing. Parameterization of turbulent transport is used to simulate the vertical profiles and temporal variation of quantities of interest, because of the randomness and the unknown physics of turbulence. However, turbulence in the mixed layer is not completely random, but is often organized into identifiable structures such as thermals and plumes in the CBL. Simulation of these large eddies is quite different from simulation of smaller eddies generated by local shears in the surface layer. Non-local property of the large eddies should be accounted for in the parameterization.

Pratt & Whitney R-2800-99 "Double Wasp"

Convair NB-36H

Convair C-131F Samaritan

Convection Baking

General Dynamics Aircraft and their Predecessors

Convair YF2Y-1 Sea Dart

Convair P-81

Convalescent Home

Convective potential

In the field of fluid dynamics, a convection cell is the phenomenon that occurs when density differences exist within a body of liquid or gas. These density differences result in rising and/or falling currents, which are the key characteristics of a convection cell. When a volume of fluid is heated, it expands and becomes less dense and thus more buoyant than the surrounding fluid. The colder, denser part of the fluid descends to settle below the warmer, less-dense fluid, and this causes the warmer fluid to rise. Such movement is called convection, and the moving body of liquid is referred to as a convection cell. This particular type of convection, where a horizontal layer of fluid is heated from below, is known as Rayleigh-Bénard convection. Convection usually requires a gravitational field, but in microgravity experiments, thermal convection has been observed without gravitational effects.Fluids are generalized as materials that exhibit the property of flow; however, this behavior is not unique to liquids. Fluid properties can also be observed in gases and even in particulate solids (such as sand, gravel, and larger objects during rock slides).A convection cell is most notable in the formation of clouds with its release and transportation of energy. As air moves along the ground it absorbs heat, loses density and moves up into the atmosphere. when it is forced into the atmosphere, which has a lower air pressure, it cannot contain as much fluid as at a lower altitude, so it releases its moist air, producing rain. In this process the warm air is cooled; it gains density and falls towards the earth and the cell repeats the cycle.Convection cells can form in any fluid, including the Earth's atmosphere (where they are called Hadley cells), boiling water, soup (where the cells can be identified by the particles they transport, such as grains of rice), the ocean, or the surface of the sun. The size of convection cells is largely determined by the fluid's properties. Convection cells can even occur when the heating of a fluid is uniform.

Convective overshoot is a phenomenon of convection carrying material beyond an unstable region of the atmosphere into a stratified, stable region. Overshoot is caused by the momentum of the convecting material, which carries the material beyond the unstable region.

*Focke-Wulf Triebflügel
*Heinkel Lerche
*Lockheed XFV

Convair R4Y

Convair T-29B Flying Classroom

The Convair P6Y was an unbuilt aircraft designed by Convair in the 1950s. The design was initiated to meet a requirement of the United States Navy (USN) for an anti-submarine warfare seaplane.

From 1999 when Charles Cressy first developed, introduced and patented a drying assembly method and over the following 14 years convectant drying has been further developed and become established as an alternative to conventional refrigerant and desiccant dehumidifier drying techniques. The process is revolutionising how wet property is dried out as it minimizes stripout, secondary damage and downtime.

The Convair Kingfish reconnaissance aircraft design was the ultimate result of a series of proposals designed at Convair as a replacement for the Lockheed U-2. Kingfish competed with the Lockheed A-12 for the Project Oxcart mission, and lost to that design in 1959.

* Boulton Paul P.111
* Nord 1500 Griffon

turbojets

Convair Model 5

Convair PB4Y-2 Privateer

The Convair XC-99, AF Ser. No. 43-52436, is a prototype heavy cargo aircraft built by Convair for the United States Air Force. It was the largest piston-engined land-based transport aircraft ever built, and was developed from the Convair B-36 bomber, sharing the wings and some other structures with it. The first flight was on 24 November 1947 in San Diego, California, and after testing it was delivered to the Air Force on 26 May 1949. The Convair Model 37 was a planned civil passenger variant based on the XC-99 but was not built.

Convair Model 7-002

The convective condensation level (CCL) represents the height (or pressure) where an air parcel becomes saturated when heated from below and lifted adiabatically due to buoyancy.In the atmosphere, assuming a constant water vapor mixing ratio, the dew point temperature (the temperature where the relative humidity is 100%) decreases with increasing height because the pressure of the atmosphere decreases with height.

Convair CV-240-21

Convair Model 4

Convair C-131H Samaritan

Convair XC-99

Yenne, Bill. Convair Deltas from SeaDart to Hustler. Specialty Press: North Branch, MN, 2009. ISBN 978-1-58007-118-5.

Convair XF2Y-1 Sea Dart

Convair Kingfish

Lycoming O-435C

Convair C-131D Samaritan

Convection diffusion equation

Convective flow

Convective instability

Convair TF-102A Delta Dagger

* List of bomber aircraft
* List of military aircraft of the United States

Military transport

Convalescent

Convair CV-580

Convalesce

The Convair XFY Pogo tail-sitter was an experiment in vertical takeoff and landing. The Pogo had delta wings and three-bladed contra-rotating propellers powered by a 5,500 hp (4,100 kW) Allison YT40-A-6 turboprop engine. It was intended to be a high-performance fighter aircraft capable of operating from small warships. Landing the XFY-1 was difficult, as the pilot had to look over his shoulder while carefully working the throttle to land.

Convective inhibition (CIN or CINH) is a numerical measure in meteorology that indicates the amount of energy that will prevent an air parcel from rising from the surface to the level of free convection.CIN is the amount of energy required to overcome the negatively buoyant energy the environment exerts on an air parcel. In most cases, when CIN exists, it covers a layer from the ground to the level of free convection (LFC).

*List of military aircraft of the United States
*List of twin-boom aircraft

Convective Temperature

Convair YB-60-1-CF

Convair X-12

*North American Rockwell OV-10 Bronco
imp

Convair Sea Dart

Convair CV-440-0

Convective mixing

Convair F106 Delta Dart

Convair CV-340-62

US$4.9 million for the program

Convallariaceae

both

Convair F-106A-130-CO Delta Dart

Convective condensation level

ASW flying boat

Convective inhibition (CIN or CINH) is a numerical measure in meteorology that indicates the amount of energy that will prevent an air parcel from rising from the surface to the level of free convection.CIN is the amount of energy required to overcome the negatively buoyant energy the environment exerts on an air parcel. In most cases, when CIN exists, it covers a layer from the ground to the level of free convection (LFC). The negatively buoyant energy exerted on an air parcel is a result of the air parcel being cooler (denser) than the air which surrounds it, which causes the air parcel to accelerate downward. The layer of air dominated by CIN is warmer and more stable than the layers above or below it.The situation in which convective inhibition is measured is when layers of warmer air are above a particular region of air. The effect of having warm air above a cooler air parcel is to prevent the cooler air parcel from rising into the atmosphere. This creates a stable region of air. Convective inhibition indicates the amount of energy that will be required to force the cooler packet of air to rise. This energy comes from fronts, heating, moistening, or mesoscale convergence boundaries such as outflow and sea breeze boundaries, or orographic lift.Typically, an area with a high convection inhibition number is considered stable and has very little likelihood of developing a thunderstorm. Conceptually, it is the opposite of CAPE.CIN hinders updrafts necessary to produce convective weather, such as thunderstorms. Although, when large amounts of CIN are reduced by heating and moistening during a convective storm, the storm will be more severe than in the case when no CIN was present.CIN is strengthened by low altitude dry air advection and surface air cooling. Surface cooling causes a small capping inversion to form aloft allowing the air to become stable. Incoming weather fronts and short waves influence the strengthening or weakening of CIN.CIN is calculated by measurements recorded electronically by a Rawinsonde (weather balloon) which carries devices which measure weather parameters, such as air temperature and pressure. A single value for CIN is calculated from one balloon ascent by use of the equation below. The z-bottom and z-top limits of integration in the equation represent the bottom and top altitudes (in meters) of a single CIN layer, T v , p a r c e l {\displaystyle T_{v,parcel}} is the virtual temperature of the specific parcel and T v , e n v {\displaystyle T_{v,env}} is the virtual temperature of the environment. In many cases, the z-bottom value is the ground and the z-top value is the LFC. CIN is an energy per unit mass and the units of measurement are joules per kilogram (J/kg). CIN is expressed as a negative energy value. CIN values greater than 200 J/kg are sufficient to prevent convection in the atmosphere. CIN = ∫ z bottom z top g ( T v,parcel − T v,env T v,env ) d z {\displaystyle {\text{CIN}}=\int _{z_{\text{bottom}}}^{z_{\text{top}}}g\left({\frac {T_{\text{v,parcel}}-T_{\text{v,env}}}{T_{\text{v,env}}}}\right)dz} The CIN energy value is an important figure on a skew-T log-P diagram and is a helpful value in evaluating the severity of a convective event. On a skew-T log-P diagram, CIN is any area between the warmer environment virtual temperature profile and the cooler parcel virtual temperature profile.CIN is effectively negative buoyancy, expressed B-; the opposite of convective available potential energy (CAPE), which is expressed as B+ or simply B. As with CAPE, CIN is usually expressed in J/kg but may also be expressed as m2/s2, as the values are equivalent. In fact, CIN is sometimes referred to as negative buoyant energy (NBE).

Convair CV-240-0

Convair R3Y Tradewind

Convair XA-44

at sea level

Not flown

* Convair CV-240 family
* CC-109 Cosmopolitan

five

Convair R2Y

Convair F-92A

Convair Coronado

Convair CV5800

Convair XP6Y

16 m

In meteorology, convective instability or stability of an air mass refers to its ability to resist vertical motion. A stable atmosphere makes vertical movement difficult, and small vertical disturbances dampen out and disappear. In an unstable atmosphere, vertical air movements (such as in orographic lifting, where an air mass is displaced upwards as it is blown by wind up the rising slope of a mountain range) tend to become larger, resulting in turbulent airflow and convective activity. Instability can lead to significant turbulence, extensive vertical clouds, and severe weather such as thunderstorms.Adiabatic cooling and heating are phenomena of rising or descending air. Rising air expands and cools due to the decrease in air pressure as altitude increases. The opposite is true of descending air; as atmospheric pressure increases, the temperature of descending air increases as it is compressed. Adiabatic heating and adiabatic cooling are terms used to describe this temperature change.The adiabatic lapse rate is the rate at which a rising or falling air mass lowers or increases per distance of vertical displacement. The ambient lapse rate is the temperature change in the (non-displaced) air per vertical distance. Instability results from difference between the adiabatic lapse rate of an air mass and the ambient lapse rate in the atmosphere.If the adiabatic lapse rate is lower than the ambient lapse rate, an air mass displaced upward cools less rapidly than the air in which it is moving. Hence, such an air mass becomes warmer relative to the atmosphere. As warmer air is less dense, such an air mass would tend to continue to rise.Conversely, if the adiabatic lapse rate is higher than the ambient lapse rate, an air mass displaced upward cools more rapidly than the air in which it is moving. Hence, such an airmass becomes cooler relative to the atmosphere. As cooler air is more dense, the rise of such an airmass would tend to be resisted.When air rises, moist air cools at a lower rate than dry air. That is, for the same vertical movement, a parcel of moist air will be warmer than a parcel of dry air. This is because of the condensation of water vapor in the air parcel due to expansion cooling. As water vapor condenses, latent heat is released into the air parcel. Moist air has more water vapor than dry air, so more latent heat is released into the parcel of moist air as it rises. Dry air does not have as much water vapor, therefore dry air cools at a higher rate with vertical movement than moist air. As a result of the latent heat that is released during water vapor condensation, moist air has a relatively lower adiabatic lapse rate than dry air. This makes moist air generally less stable than dry air (see convective available potential energy). The dry adiabatic lapse rate (for unsaturated air) is 3 °C (5.4 °F) per 1,000 vertical feet. The moist adiabatic lapse rate varies from 1.1 °C to 2.8 °C (2 °F to 5 °F) per 1,000 vertical feet.The combination of moisture and temperature determine the stability of the air and the resulting weather. Cool, dry air is very stable and resists vertical movement, which leads to good and generally clear weather. The greatest instability occurs when the air is moist and warm, as it is in the tropical regions in the summer. Typically, thunderstorms appear on a daily basis in these regions due to the instability of the surrounding air.The ambient lapse rate differs in different meteorological conditions, but, on average, is 2 °C (3.5 °F) per 1,000 vertical feet.

Convallaria umbellulata

Convair CV-880

Light attack and observation aircraft

Convective overturn

Convair CV-880-22-1

Convective precipitation

*Boeing B-52 Stratofortress
*Myasishchev M-4 Molot
*Tupolev Tu-95

Convective boundary layer

Convective heat transfer, often referred to simply as convection, is the transfer of heat from one place to another by the movement of fluids. Convection is usually the dominant form of heat transfer in liquids and gases. Although often discussed as a distinct method of heat transfer, convective heat transfer involves the combined processes of unknown conduction (heat diffusion) and advection (heat transfer by bulk fluid flow).Convection can be "forced" by movement of a fluid by means other than buoyancy forces (for example, a water pump in an automobile engine). Thermal expansion of fluids may also force convection. In other cases, natural buoyancy forces alone are entirely responsible for fluid motion when the fluid is heated, and this process is called "natural convection". An example is the draft in a chimney or around any fire. In natural convection, an increase in temperature produces a reduction in density, which in turn causes fluid motion due to pressures and forces when fluids of different densities are affected by gravity (or any g-force). For example, when water is heated on a stove, hot water from the bottom of the pan rises, displacing the colder denser liquid, which falls. After heating has stopped, mixing and conduction from this natural convection eventually result in a nearly homogeneous density, and even temperature. Without the presence of gravity (or conditions that cause a g-force of any type), natural convection does not occur, and only forced-convection modes operate.The convection heat transfer mode comprises one mechanism. In addition to energy transfer due to specific molecular motion (diffusion), energy is transferred by bulk, or macroscopic, motion of the fluid. This motion is associated with the fact that, at any instant, large numbers of molecules are moving collectively or as aggregates. Such motion, in the presence of a temperature gradient, contributes to heat transfer. Because the molecules in aggregate retain their random motion, the total heat transfer is then due to the superposition of energy transport by random motion of the molecules and by the bulk motion of the fluid. It is customary to use the term convection when referring to this cumulative transport and the term advection when referring to the transport due to bulk fluid motion.

The Convair XC-99, AF Ser. No. 43-52436, is a prototype heavy cargo aircraft built by Convair for the United States Air Force. It was the largest piston-engined land-based transport aircraft ever built, and was developed from the Convair B-36 bomber, sharing the wings and some other structures with it. The first flight was on 24 November 1947 in San Diego, California, and after testing it was delivered to the Air Force on 26 May 1949.

n/a

Canceled

Convair NB-36 Crusader

Convair Tradewind

Convair F-102A Delta Dagger

Convection microwave oven

Convalidation

ft in

* Lippisch P.13a

Convair CV-990-30A-6 Coronado

— Convallaria keiskei

Convective heat transfer, often referred to simply as convection, is the transfer of heat from one place to another by the movement of fluids. Convection is usually the dominant form of heat transfer in liquids and gases.

Convection Rotation et Transits Planétaires

Convair YB-58A-10-CF Hustler

Convair CV-300

Five duty + five reserve crew

* List of military aircraft of the United States
* List of military aircraft of the United States (naval)
* List of military transport aircraft

Convection-diffusion transport equation

"Hot Flight" The quest for nuclear-powered flight.

Convecao Batista Nacional

Convallaria majalis

Convair VC-131

In the field of fluid dynamics, a convection cell is the phenomenon that occurs when density differences exist within a body of liquid or gas. These density differences result in rising and/or falling currents, which are the key characteristics of a convection cell. When a volume of fluid is heated, it expands and becomes less dense and thus more buoyant than the surrounding fluid.

Convair F-106A Delta Dart

g8J83RFggzc

38 kN

Convective acceleration

The Convair XB-46 was a single example of an experimental medium jet bomber which was developed in the mid-1940s but which never saw production or active duty. It competed with similar designs, the North American XB-45 and Martin XB-48, all of which saw little use after the successful development of the Boeing XB-47.

Convair F-102A-75-CO Delta Dagger

Convair Model 35

Convair PQM-102

Convection–diffusion transport equation

* Convair F-102 Delta Dagger
* Convair F-106 Delta Dart

Convair Model 22

Convair R4Y Samaritan

Convallaria is a genus of flowering plants, the most prevalent species of which is lily of the valley.It is usually described as the monotypic genus with the single species Convallaria majalis, but now some botanists distinguish up to 3 species of Convallaria, also including Convallaria keiskei and Convallaria montana.

Strophanthin 3alpha-1-rhamnoside ; Strophanthidin alpha-l-rhamnopyranoside; Strophanthidin a-l-rhamnopyranoside; Corglykon;20,5beta-cardenolid-19-al-3beta,5beta,14beta-triol-3beta-d-[a-1-rhamnopyranoside] ; 5Beta,20[22]-cardenolide-19-one-3beta,5alpha,14-triol-3-[6-deoxy-alpha-l-mannopyranosyl] ; 3Beta,5alpha,14-trihydroxy-19-oxo-5beta,20[22]-cardenolide-3-[6-deoxy-alpha-l-mannopyranosyl]

Convair T-32

Convair P5Y

* Saunders-Roe SR.A/1

≈500 mi

Convair F2Y Sea Dart

Conval

Convair F-106A-100-CO Delta Dart

The Convair XF-92 (originally designated XP-92) was an early American delta-wing aircraft. Originally conceived as a point-defense interceptor, the design was later used purely for experimental purposes. However, it led Convair to use the delta-wing on a number of designs, including the F-102 Delta Dagger, F-106 Delta Dart, B-58 Hustler, the US Navy's F2Y Sea Dart as well as the VTOL FY Pogo.

Convair Metropolitan

Paraguayan Air Force

Convair T-29 Flying Classroom

Convective momentum transport is an atmospheric event that involves an exchange of momentum, usually due to vertical motion (convection) associated with clouds.The essential processes responsible for cloud convective momentum transport in the tropics are:The vertical momentum advection due to subsidence of environmental air compensating cloud mass flux.The detrainment of excess momentum from clouds.The convection induced pressure gradient force.

Convair CV-440-12

Convair CV-990-30A-5

Convair CV-440 Metropolitan

Convective planetary boundary layer

— Convallaria montana

Convectional storms

Convallarin

* Project Pluto
* Project Rover
* NERVA
* WS-125

Convalescence

Convair F-106B-50-CO Delta Dart

Convair CV-240-2

Convair YB/RB-58A-10-CF Hustler

Convair F.102 Delta Dagger

Convair X-11

Convair CV-640

Convair CV-440-11

Convair NB-36H Crusader

service ceiling

*Take-off to 50 ft : Less than 500 ft
*Landing from 50 ft : Less than 500 ft

Convection Current

Convair P6Y

Convair C-99

Heavy transport

Convair C-131

Convallarin is a crystalline glucoside extracted from the Lily of the Valley plant (Convallaria majalis)It may be obtained from the alcoholic extract of the residue from which the convallamarin has been removed with water. The alcoholic solution is treated with lead acetate, the filtrate freed from lead by hydrogen sulfide, and crystallised by concentration. An aqueous solution froths like soap and water when shaken.

Convair Model 118

at 15,000 ft

none

Convair CV-540

The Convair NB-36H was a bomber that carried a nuclear reactor. It was also known as the "Crusader". It was created for the Aircraft Nuclear Propulsion program, or the ANP, to show the feasibility of a nuclear-powered bomber. Its development ended with the cancellation of the ANP program.

Convair OY

The Convair R3Y Tradewind was an American 1950s turboprop-powered flying boat designed and built by Convair.

Convective Boundary Layer

Fighters of the United States Air Force

Convective instability of the second kind

Convair Model 48 Charger

Convair X-6

Convallaria polygonatum

Prototype

Convair CORDIC II model A

ONLY AVAILABLE IF STANDING ALONE

Convair C-87

Convair OA-10

Hamilton Standard

Convair Model 8

performance header

From 1999 when Charles Cressy first developed, introduced and patented a drying assembly method and over the following 14 years convectant drying has been further developed and become established as an alternative to conventional refrigerant and desiccant dehumidifier drying techniques. The process is revolutionising how wet property is dried out as it minimizes stripout, secondary damage and downtime. In July 2013 British Standards PAS 64 "Mitigation and recovery of water damaged buildings - Code of practice" was published recognising and including descriptions of the process within the document. The PAS 64:2013 is available for purchase (www.bsigroup.com/shop)Convectant drying is described as: "the balanced manipulation and control of air exchanges, heat, and vapour pressure differential to create optimum conditions for evaporation, reduction and control of airborne moisture from the indoor environment".The word "convectant" was coined by A Habbershaw and TJ Cressy in 2003 so that the process could be recognised and established as a credible alternative to the traditional refrigerant and desiccant drying processes.The convectant drying process has been independently tested by the National Flood School in the UK (2005 and 2012) this testing confirmed the efficacy of the process which has been proven to be many times faster than traditional drying methods.Convectant drying equipment is available in portable and trailer mounted form.The method has been granted international patents. US Patent 6662467: U.S. Provisional Application No. 61/194,062, US20100011612 and for a portable hand truck method. Also, a GB Patent No 0813169.0.Both systems use heat, air exchanges and controlled manipulation of the indoor environment to reduce the drying time compared to traditional methods.

Design only

Fin-Folding Aerial Rockets

* Convair XF-92
* F-102 Delta Dagger
* F-106 Delta Dart

ft/min

* Black project

Convair XB-36 Peacemaker

*List of experimental aircraft
*List of fighter aircraft
*List of military aircraft of the United States

— Convallaria majalis or lily of the valley

Convective momentum transport

Convallaria obtusifolia

Convair YB-58-1-CF Hustler

kts

Convection column

Convair XF-92

Convair UC-880

Convair T-29

Convair XFY-1

Pratt & Whitney J57-P-3

General Electric YJ85-GE-1

Convair XP5Y-1

Convair Model 39

Convallarinum

Convalescence is the gradual recovery of health and strength after illness or injury. It refers to the later stage of an infectious disease or illness when the patient recovers and returns to normal, but may continue to be a source of infection even if feeling better. In this sense, "recovery" can be considered a synonymous term.

Convective Available Potential Energy

Convair XT-32

at 35,000 ft

Convection-diffusion equation

Convective

Convective overshoot

Steve Ginter Convair XP5Y-1 & R3Y-1/2 Tradewind

Convair CV-990

The Convair Model 48 Charger was a prototype light attack and observation aircraft of the 1960s, developed to meet a requirement for a dedicated counter-insurgency (COIN) aircraft. It was a two-seat, twin-boom aircraft powered by two turboprop engines which lost out to the North American Rockwell OV-10 Bronco of similar layout, only a single example being built.

radials

Convair CV-990-30A-6

Convair YB-60

Convalescent home

Convair XA-41

Convective derivative

Convair CV-240-12

Convective instability of the first kind

United States Military Aircraft since 1909

Convallaria stellata

Convective Available Potential Energy (CAPE)

Convair Model 37

propellers

Convair NB-36H Nuclear Test Aircraft

Convair Turboliner

Convallaria parviflora

Convair CV-340/580

Convallaria majalis range.png

Convair XB-36

Convection roaster

* Boeing B-47 Stratojet
* English Electric Canberra
* Ilyushin Il-22
* Martin XB-48
* North American B-45 Tornado

one

Convair F-7

Convair F-102

Convair PQM-102A Delta Dagger

The Convair Model 58-9 was a proposed American supersonic transport, developed by the Convair division of General Dynamics and intended to carry fifty-two passengers at over Mach 2. Derived from the B-58 Hustler bomber, it was designed in 1961 but no examples of the type were ever built.

Convallaria compressa

Map of Convallaria species distribution:

Convair Model 2

air-cooled flat-six

Convair XP-81

* List of flying boats and seaplanes
* List of military aircraft of the United States (naval)

*List of bomber aircraft
*List of military aircraft of the United States

Convair RB-36H-25-CF Peacemaker

Convection cells

Convair CV-600

Convatec

Convective rainfall

Convective outlook

Convection heater

Cancelled in 1949

Convair XP-92

Convair CV-340-32

*List of military aircraft of the United States (naval)
*List of seaplanes and amphibious aircraft

Cancelled

Convair CV-990-30A-5 Coronado

Convair F2Y

Convair F-106B-55-CO Delta Dart

m/s

Convair CORDIC II model B

The Convair X-6 was a proposed experimental aircraft project to develop and evaluate a nuclear-powered jet aircraft. The project was to use a Convair B-36 bomber as a testbed aircraft, and though one NB-36H was modified during the early stages of the project, the program was canceled before the actual X-6 and its nuclear reactor engines were completed. The X-6 was part of a larger series of programs, costing US$7 billion in all, that ran from 1946 through 1961. Because such an aircraft's range would not have been limited by liquid jet fuel, it was theorized that nuclear-powered strategic bombers would be able to stay airborne for weeks at a time.

Convalescents

The convective overturn model of supernovae was proposed by Bethe and Wilson in 1985, and received a dramatic test with SN 1987A, and the detection of neutrinos from the explosion.

Convection cell

The Convair C-131 Samaritan was an American twin-engined military transport produced from 1954 to 1956 by Convair. It was the military version of the Convair CV-240 family of airliners.

*List of military aircraft of the United States

*Beriev Be-6
*Martin P5M Marlin

Convair T-29A-CO

Pratt & Whitney R-4360-41 Wasp Major

Convectional precipitation

Convection Oven

*Flying car (aircraft)

Five

Convalescences

Convair CV-580 Airtanker

Convair CV-340-35

Convection–diffusion equation

Convective heat transfer

Convectant drying

The Convair X-6 was a proposed experimental aircraft project to develop and evaluate a nuclear-powered jet aircraft. The project was to use a Convair B-36 bomber as a testbed aircraft, and though one NB-36H was modified during the early stages of the project, the program was canceled before the actual X-6 and its nuclear reactor engines were completed. The X-6 was part of a larger series of programs, costing US$7 billion in all, that ran from 1946 through 1961.

The Convective Boundary layer (CBL), also known as the daytime Planetary boundary layer, is the part of the atmosphere most directly affected by solar heating of the earth's surface.This layer extends from the earth surface to a capping inversion that typically locates at a height of 1–2 km by midafternoon over land.

Convair CORDIC II

Convair Model 3

Convair F-106

Convair CORDIC I

Convection (meteorology)

* VTOL

Convair SM-65 Atlas

33.4 kN

Convair XFY Pogo

Convair XP5Y Tradewind

Convair T-29E

* Tu-95LAL/Tu-119

Convair CV-440

General Dynamic Aircraft and their Predecessors

Convair CV-340-31

Convair T-29D-CO

Convair XFY-1 Pogo

for program

* Convair NB-36H

The convective condensation level (CCL) represents the height (or pressure) where an air parcel becomes saturated when heated from below and lifted adiabatically due to buoyancy.In the atmosphere, assuming a constant water vapor mixing ratio, the dew point temperature (the temperature where the relative humidity is 100%) decreases with increasing height because the pressure of the atmosphere decreases with height. The CCL is determined by plotting the dew point (100%RH) verses altitude and locating the intersection with the actual measured temperature sounding. It marks where the cloud base begins when air is heated from below to the convective temperature, without mechanical lift. Once the CCL is determined, the surface temperature necessary to raise a mass of air to that height can be found by using the Dry Adiabatic Lapse Rate (DALR) to determine the potential temperature. In the early morning, this temperature is typically larger than the surface temperature, in the mid-afternoon, it may be the same.Compare this to the Lifting Condensation Level (LCL) where the air is lifted and cooled without first increasing the surface temperature. The LCL is less than or equal to the CCL depending on the temperature profile.Both condensation levels indicate the altitude (or pressure) where relative humidity reaches 100%. However, since the actual condensation level depends on the availability of condensation nuclei, clouds typically do not form until the relative humidity is somewhat above 100%.

Convecting

Reconnaissance aircraft

Wright R-3350-32

Convair CV-240 family Accidents and incidents

in rear of centre nacelle

Allison J35-A-3

radial piston engines

Convallaria angulosa

Convair XF-92A

Convalescence EP

* Lockheed A-12
* Lockheed SR-71 Blackbird
* Project Isinglass
* Tsybin RSR

Convair Model 116

Convallaria keiskei

Convair CV-880-22M-3

REQUIRED IF STANDING ALONE

Missiles, bombs, and depth charges on external hardpoints