CONVECTION THE MOVEMENT MOLECULE FLUID LIQUID GAS RHEID TAKES ADVECTION DIFFUSION CANNOT NEITHER BULK CURRENT FLOWS HEAT HEAT CONDUCTION BUNSEN BURNER THE SIDE GLASS FULL OBSERVING CHANGES TEMPERATURE THE GLASS CAUSED GHOST MOVING COOLER CONVECTIVE HEAT TRANSFER THE MAJOR HEAT TRANSFER MAJOR MODE MASS TRANSFER CONVECTIVE HEAT AND MASS TRANSFER RANDOM BROWNIAN MOTION PARTICLES THE FLUID MATTER TRANSPORTED MOTION CURRENTS THE CONTEXT TERM USED TO REFER TO SUM OF DIFFUSIVE IN COMMON REFER PROCESS SOMETIMES FREE FORCED HEAT CONVECTION MECHANICS THE WORD THE GENERAL SHOULD TERMS SAID TO CAPILLARY ACTION WEISSENBERG NATURAL CONVECTION ROLE THE STRUCTURE EARTHS ATMOSPHERE DISCRETE CELLS THE ATMOSPHERE SEEN STRONGER THUNDERSTORM STELLAR PHYSICS RELATED SCIENTIFIC ENGINEERING CONTEXTS SENSE FLUID MECHANICS THERMODYNAMICS TAKEN MEAN TRANSPORT EQUATION NUMBER TRANSPORT PHENOMENA MEANING SCALE ATMOSPHERE PLANET MANTLE MECHANISM FRACTION INTERIORS OBVIOUS HURRICANE DUST THOUGHT ACCRETION DISKS BLACK HOLE SPEEDS APPROACH THE ENTITY INTEREST DIFFUSED CONDUCTIVE HEAT TRANSFER THE TRANSFER ENERGY VIBRATIONS MOLECULAR LEVEL SOLID RADIATIVE HEAT TRANSFER ELECTROMAGNETIC WAVES NATURALLY OCCURRING FLUID FLOW OCEANIC CURRENTS MOVEMENTS EARTHS MANTLE COOLING RATE HEAT SINK CONJUNCTION COMPUTER CPU ENSURE OPERATING TEMPERATURE KEPT CONVECTION CELL ALSO KNOWN AS CELL CHARACTERISTIC PATTERN RISING BODY ENCOUNTERS COLD COLDER DIRECT EXCHANGE THE EXAMPLE RADIATES THIS HEAT LOSS DENSER UNDERNEATH STILL RISING THE RISING MOVES FORCE THE RISING FORCE BENEATH BEGINS AS IT THE CYCLE REPEATS ITSELF ATMOSPHERIC CIRCULATION MEANS THERMAL ENERGY THE SURFACE OCEAN CIRCULATION STRUCTURE CLIMATOLOGICAL REMAINS LATITUDINAL CIRCULATION INCIDENT SOLAR RADIATION AREA HIGHEST THE HEAT EQUATOR LATITUDE REACHING MINIMA THE POLES PRIMARY HADLEY CELL POLAR VORTEX RELEASE LATENT HEAT CONDENSATION WATER VAPOR HIGHER ALTITUDES CLOUD FORMATION ON THE OTHER HAND COMES OCEAN SPECIFIC HEAT CAPACITY THERMAL CONDUCTIVITY BENEATH THE SURFACE LESS THAN BRINGS THE SEA AIR COOLED THE LAND CONTACT OUT TO SEA THE WALKER SOUTHERN OSCILLATION SOME MORE PHENOMENA GLOBAL ATMOSPHERIC WIND HYDROLOGIC CYCLE FOEHN WIND DOWNWIND MOUNTAIN RESULTS ADIABATIC MOISTURE WINDWARD LAPSE RATES LEEWARD SLOPES HEIGHT THERMAL COLUMN VERTICAL SECTION THERMALS UNEVEN HEATING EARTHS SURFACE THE SUN TURN ABOVE BECOMING LESS DENSE AIR MASS THERMAL LOW THE MASS LIGHTER EXPANSION STOPS COOLED THERMAL FLOW EXTERIOR DISPLACED WEATHER BREEZE WARM AIR DENSITY COOL AIR SO WARM RISES SIMILAR HOT AIR BALLOON CLOUDS CARRYING CAUSING PACKET CONDENSE LATENT HEAT OF FUSION COOL THE CLOUDS ENOUGH INSTABILITY PRESENT CONTINUE CUMULONIMBUS CLOUDS SUPPORT LIGHTNING CONDITIONS UNSTABLE AIRMASS LIFTING FORCE STAGES MATURE DISSIPATION AVERAGE ON THE CONDITIONS THESE THREE MINUTES TO GO THE OCEANS WATER THE EQUATOR CIRCULATE TOWARD POLE POLAR HEADS SURFACE THE TRADE WINDS BLOW THE TROPICS WESTERLIES EASTWARD STRESS NEGATIVE CURL NORTHERN HEMISPHERE REVERSE SOUTHERN HEMISPHERE SVERDRUP TRANSPORT CONSERVATION POTENTIAL VORTICITY WINDS SUBTROPICAL RIDGE WESTERN PERIPHERY RELATIVE VORTICITY BALANCED THE WESTERN BOUNDARY FRICTION THE COLD WESTERN BOUNDARY CURRENT HIGH LATITUDES OVERALL WESTERN INTENSIFICATION CAUSES BASIN EASTERN TRAVELS STRONG EVAPORATIVE COOLING DRIVEN OVER WATER EVAPORATION LEAVING ONCE SEA ICE SALTS LEFT OUT BRINE PRODUCE PRECISELY NORTHERN ATLANTIC SINK DOWN ACTION NOT UNLIKE LAVA LAMP THE NORTH ATLANTIC DEEP WATER MANTLE CONVECTION SLOW CREEPING MOTION ROCKY CONVECTION CURRENTS THE INTERIOR THE EARTH DRIVING TECTONIC PLATES MOVE AROUND DIVIDED CONSUMED OPPOSITE PLATE BOUNDARIES CREATION ACCRETION EDGES MATERIAL CONDUCTION THE CONSUMPTION THE MATERIAL SINKS THE PROCESS SUBDUCTION OCEAN TRENCH SUBDUCTED DEPTH EARTHS INTERIOR WHERE IT SINKING OCEANIC CRUST TRIGGERS THE STACK CHIMNEY EFFECT FLUE GAS STACKS BUOYANCY DIFFERENCE AIR DENSITY GREATER THE HEIGHT BUOYANCY FORCE THUS DRIVE NATURAL VENTILATION COOLING TOWERS OPERATE PRINCIPLE SOLAR UPDRAFT TOWER DEVICE ELECTRICITY CONVECTION ZONE STAR THE RANGE RADII PHOTOSPHERE VISIBLE TOPS PLASMA THE CENTER OUTER EDGE DARKER THE COOLER GRANULE DIAMETER ON THE ORDER OF KILOMETERS LASTS MINUTES DISSIPATING BELOW LAYER UP TO FLUIDS AT ALL SCALES VARIETY CIRCUMSTANCES NATURAL FORCED CONVECTION LEADING BROAD BODY FORCE ACTING GRAVITY GENERALLY AS ONE FORCED EXIST DISTINCTION PARTICULARLY FREE CONVECTION DIFFERENCES AFFECT COMPONENTS GRAVITATIONAL FIELD COMMON EXAMPLE RISE SMOKE BOILING WATER THE BOTTOM THE COOL THE POT LIKEWISE BE MORE RAPID VARIATION ACCELERATION DISTANCE CONVECTING DIFFUSING AWAY THERMAL GRADIENT VISCOUS THE ONSET DETERMINED RAYLEIGH NUMBER NOTE ARISE REASONS CASE GRAVITATIONAL BUOYANT DO NOT MICROGRAVITY PRESENCE ENVIRONMENT PROPER HEAT ADVECTION EXTERNAL INCREASE MIXING SUBSTANCE THE ACTION PROPELLER AERODYNAMIC HEATING RADIATOR HEATING AND COOLING PARTS THE BODY BLOOD FAMILIAR FIRE AIR FLOW ALL DIRECTIONS THE ONLY FIRES ABLE DRAW FRESH OXYGEN