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Convection cell

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86: 189: 254: 25: 175:, when it radiates heat. At some point, the fluid becomes denser than the fluid beneath it, which is still rising. Since it cannot descend through the rising fluid, it moves to one side. At some distance, its downward force overcomes the rising force beneath it, and the fluid begins to descend. As it descends, it warms again through surface contact or conductivity and the cycle repeats. 78: 121:, 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 266:
Movie of the solar photosphere observed with the Swedish 1-m Solar Telescope (SST) on La Palma, Spain. The movie shows solar granulation which is a result of convective motions of bubbles of hot gas that rise from the solar interior. When these bubbles reach the surface, the gas cools and flows down
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All thunderstorms, regardless of type, go through three stages: a 'developing stage', a 'mature stage', and a 'dissipating stage'. The average thunderstorm has a 24 km (15 mi) diameter. Depending on the conditions present in the atmosphere, these three stages take an average of 30 minutes
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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
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again in the darker lanes between the bright cells. In these so-called intergranular lanes, we can also see small bright points and more extended bright elongated structures. These are regions with strong magnetic fields.
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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.
258: 140:; 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 85: 171:
A rising body of fluid typically loses heat when it encounters a cold surface when it exchanges heat with colder liquid through direct exchange, or in the example of the
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to form, which support lightning and thunder. Generally, thunderstorms require three conditions to form: moisture, an unstable air mass, and a lifting force (heat).
133:. Convection usually requires a gravitational field, but in microgravity experiments, thermal convection has been observed without gravitational effects. 163:. 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. 159:), 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 499: 222:
of vaporisation, which allows the rising packet of air to cool less than its surrounding air, continuing the cloud's ascension. If enough
210:. Clouds form as relatively warmer air carrying moisture rises within cooler air. As the moist air rises, it cools, causing some of the 495: 290:
averaging about 1,000 kilometres in diameter. The plasma cools as it rises and descends in the narrow spaces between the granules.
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Altocumulus cloud as seen from the Space Shuttle. Altocumulus clouds are formed by convective activity.
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Heating caused by the compression of descending air is responsible for such winter phenomena as the
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after fermenting 10 days with cinnamon floating on top. Convection is caused by yeast releasing CO2.
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Warm air has a lower density than cool air, so warm air rises within cooler air, similar to
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Civil engineers' pocket book: a reference-book for engineers, contractors
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Nonboussinesq Thermal Convection in Microgravity under Nonuniform Heating
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is present in the atmosphere, this process will continue long enough for
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Storm world: hurricanes, politics, and the battle over global warming
496:"A Severe Weather Primer: Questions and Answers about Thunderstorms" 446:. New York: Black Dog & Leventhal Publisher. pp. 210–211. 493: 136:
Fluids are generalized as materials that exhibit the property of
106: 218:. When the moisture condenses, it releases energy known as the 77: 110: 197: 117:. These density differences result in rising and/or falling 90: 286:, which are rising columns of superheated (5,800 Â°C) 160: 114: 470:
Severe Thunderstorms and Tornadoes in the United States
383:"Fog And Stratus – Meteorological Physical Background" 151:
Convection cells can form in any fluid, including the
125:, and the moving body of liquid is referred to as a 404: 320: 246:(as it is known in western North America) or the 178: 541: 494:National Severe Storms Laboratory (2006-10-15). 441: 385:. Zentralanstalt fĂĽr Meteorologie und Geodynamik 354:. Chinese International Press. pp. 112–13. 500:National Oceanic and Atmospheric Administration 402: 435: 16:Cyclic flow of convection currents in a fluid 466: 347: 460: 65:Learn how and when to remove this message 252: 187: 84: 76: 487: 280:is composed of convection cells called 542: 237: 411:. Houghton Mifflin Harcourt. p.  307:Yu. A.Gaponenko and V. E. Zakhvataev, 18: 380: 327:. D. Van Nostrand Company. p.  109:differences exist within a body of 105:is the phenomenon that occurs when 13: 14: 561: 521: 271: 473:. DIANE Publishing. p. 16. 192:Stages of a thunderstorm's life. 183: 23: 214:in the rising packet of air to 467:Peter Folger (10 April 2011). 396: 374: 341: 314: 300: 179:Within the Earth's troposphere 1: 293: 528:Mountainnature.com — Chinook 7: 10: 566: 351:Ancient Chinese Inventions 321:Albert Irvin Frye (1913). 195: 166: 131:Rayleigh–BĂ©nard convection 442:Michael H. Mogil (2007). 403:Chris C. Mooney (2007). 37:may need to be rewritten 155:(where they are called 268: 193: 94: 82: 265: 191: 88: 80: 348:Yikne Deng (2005). 238:Adiabatic processes 228:cumulonimbus clouds 119:convection currents 89:6-gallon bucket of 533:2014-02-14 at the 269: 194: 173:Earth's atmosphere 153:Earth's atmosphere 95: 83: 480:978-1-4379-8754-6 453:978-1-57912-743-5 422:978-0-15-101287-9 361:978-7-5085-0837-5 263: 75: 74: 67: 47:lead layout guide 557: 515: 514: 512: 511: 502:. Archived from 491: 485: 484: 464: 458: 457: 439: 433: 432: 430: 429: 410: 400: 394: 393: 391: 390: 378: 372: 371: 369: 368: 345: 339: 338: 336: 335: 318: 312: 304: 264: 208:hot air balloons 70: 63: 59: 56: 50: 43:improve the lead 27: 26: 19: 565: 564: 560: 559: 558: 556: 555: 554: 540: 539: 535:Wayback Machine 524: 519: 518: 509: 507: 492: 488: 481: 465: 461: 454: 444:Extreme Weather 440: 436: 427: 425: 423: 401: 397: 388: 386: 379: 375: 366: 364: 362: 346: 342: 333: 331: 319: 315: 305: 301: 296: 274: 253: 250:(in the Alps). 240: 234:to go through. 204: 186: 181: 169: 127:convection cell 103:convection cell 71: 60: 54: 51: 40: 28: 24: 17: 12: 11: 5: 563: 553: 552: 538: 537: 523: 522:External links 520: 517: 516: 486: 479: 459: 452: 434: 421: 395: 373: 360: 340: 313: 298: 297: 295: 292: 273: 272:Within the Sun 270: 239: 236: 185: 182: 180: 177: 168: 165: 99:fluid dynamics 73: 72: 32:The article's 31: 29: 22: 15: 9: 6: 4: 3: 2: 562: 551: 548: 547: 545: 536: 532: 529: 526: 525: 506:on 2009-08-25 505: 501: 497: 490: 482: 476: 472: 471: 463: 455: 449: 445: 438: 424: 418: 414: 409: 408: 399: 384: 377: 363: 357: 353: 352: 344: 330: 326: 325: 317: 311: 310: 303: 299: 291: 289: 285: 284: 279: 251: 249: 245: 235: 231: 229: 225: 221: 217: 213: 209: 203: 199: 190: 184:Thunderstorms 176: 174: 164: 162: 158: 154: 149: 145: 143: 139: 134: 132: 128: 124: 120: 116: 112: 108: 104: 100: 92: 87: 79: 69: 66: 58: 48: 45:and read the 44: 38: 35: 30: 21: 20: 508:. Retrieved 504:the original 489: 469: 462: 443: 437: 426:. Retrieved 406: 398: 387:. Retrieved 381:FMI (2007). 376: 365:. Retrieved 350: 343: 332:. Retrieved 323: 316: 308: 302: 281: 275: 241: 232: 205: 202:Thunderstorm 170: 157:Hadley cells 150: 146: 135: 126: 102: 96: 61: 55:October 2023 52: 41:Please help 36: 34:lead section 278:photosphere 224:instability 220:latent heat 212:water vapor 142:rock slides 550:Convection 510:2009-09-01 428:2009-08-31 389:2009-02-07 367:2009-06-18 334:2009-08-31 294:References 276:The Sun's 196:See also: 123:convection 91:honey wine 544:Category 531:Archived 283:granules 216:condense 244:chinook 167:Process 107:density 477:  450:  419:  358:  288:plasma 111:liquid 198:Cloud 475:ISBN 448:ISBN 417:ISBN 356:ISBN 248:Föhn 200:and 138:flow 101:, a 329:462 161:Sun 144:). 115:gas 113:or 97:In 546:: 498:. 415:. 413:20 513:. 483:. 456:. 431:. 392:. 370:. 337:. 68:) 62:( 57:) 53:( 49:. 39:.

Index

lead section
improve the lead
lead layout guide
Learn how and when to remove this message


honey wine
fluid dynamics
density
liquid
gas
convection currents
convection
Rayleigh–Bénard convection
flow
rock slides
Earth's atmosphere
Hadley cells
Sun
Earth's atmosphere

Cloud
Thunderstorm
hot air balloons
water vapor
condense
latent heat
instability
cumulonimbus clouds
chinook

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