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Aeronomy

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29: 515:. Atmospheric tides dominate the dynamics of the mesosphere and lower thermosphere, serving as an important mechanism for transporting energy from the upper atmosphere into the lower atmosphere. Terrestrial aeronomers study atmospheric tides because an understanding of them is essential to an understanding of the atmosphere as a whole and of benefit in improving the understanding of meteorology. Modeling and observations of atmospheric tides allow researchers to monitor and predict changes in the Earth's atmosphere. 392: 358: 349: 975: 340: 524: 442:. Although terrestrial aeronomy and meteorology once were completely separate fields of scientific study, cooperation between terrestrial aeronomers and meteorologists has grown as discoveries made since the early 1990s have demonstrated that the upper and lower atmospheres have an impact on one another's 631:
uses the findings of terrestrial and planetary aeronomy — traditionally separate scientific fields — to compare the characteristics and behaviors of the atmospheres of other planets with one another and with the upper atmosphere of Earth. It seeks to identify and describe the ways in which differing
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studies the regions of the atmospheres of other planets that correspond to the Earth's mesosphere, thermosphere, exosphere, and ionosphere. In some cases, a planet's entire atmosphere may consist only of what on Earth constitutes the upper atmosphere, or only a portion of it. Planetary aeronomers use
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An alternative definition divides the atmosphere into three rather than two parts, with the "upper atmosphere" limited to the exosphere and thermosphere, the mesosphere and stratosphere making up the "middle atmosphere," and the "lower atmosphere" consisting only of the troposphere. Use of this
541:"Upper-atmospheric lightning" or "upper-atmospheric discharge" are terms aeronomers sometimes use to refer to a family of electrical-breakdown phenomena in the Earth's upper atmosphere that occur well above the altitudes of the 264:, study the motions and chemical composition and properties of the Earth's upper atmosphere and regions of the atmospheres of other planets that correspond to it, as well as the interaction between upper atmospheres and the 797: 657:
definition does not change the focus of aeronomy, which is all of the Earth's atmosphere above the stratopause, or of meteorology, which is all of the Earth's atmosphere below the stratopause.
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observed in the lower atmosphere. Currently, the preferred term for an electrical-discharge phenomenon induced in the upper atmosphere by tropospheric lightning is "
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adopted it. "Aeronomy" later also began to refer to the study of the corresponding regions of the atmospheres of other planets.
856: 957: 881: 763: 736: 592:, or land on other planets to gain knowledge of the atmospheres of those planets through the use of instruments such as 221: 192: 914: 552:" (TLE). There are various types of TLEs including red sprites, sprite halos, blue jets, and ELVES (an acronym for " 374: 373:(center) are among the tools aeronomers use to gather data on the Earth's upper atmosphere. At right, a model of the 511:
Atmospheric tides are global-scale periodic oscillations of the Earth′s atmosphere, analogous in many ways to ocean
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has allowed planetary aeronomers to expand their field to include the atmospheres of those planets as well.
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Royal Belgian Institute for Space Aeronomy "Aeronomy, atmosphere science, what is it?" Accessed 21 May 2021
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Nagy, Andrew F.; Balogh, André; Thomas E. Cravens; Mendillo, Michael; Mueller-Woodarg, Ingo (2008).
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Aeronomy of the Middle Atmosphere : Chemistry and Physics of the Stratosphere and Mesosphere
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on various planets affect the creation, evolution, diversity, and disappearance of atmospheres.
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Nagy, Andrew F., "History of Planetary Aeronomy," cosmos.esa.int Accessed 23 March 2021
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and corresponding regions of the atmospheres of other planets. It is a branch of both
953: 877: 759: 732: 609: 553: 829:, Geophysical Monograph Series Volume 130, 2002, unpaginated Accessed 23 March 2021" 302:
entitled "Some Thoughts on Nomenclature." The term became official in 1954 when the
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Volland, H., "Atmospheric Tidal and Planetary Waves", Kluwer Publ., Dordrecht, 1988
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processes in the Earth's upper atmosphere. Terrestrial aeronomers use ground-based
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Representation of upper-atmospheric lightning and electrical-discharge phenomena
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Earle R. Williams (November 2001) "Sprites, elves, and glow discharge tubes,"
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Science of the upper region of the Earth's or other planetary atmospheres
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to describe the study of the Earth's upper atmosphere in 1946 in a
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Planetary Aeronomy: Atmosphere Environments in Planetary Systems
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focuses on the Earth's upper atmosphere, which extends from the
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An animation of atmospheric tide data gathered by the
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environment. In atmospheric regions aeronomers study,
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Atmospheres in the Solar System: Comparative Aeronomy
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The Thermosphere - the Earth's Outermost Atmosphere
473:, and ELVES. They also investigate the causes of 314:Aeronomy can be divided into three main branches: 852: 850: 778:Sydney Chapman, "Some Thoughts on Nomenclature," 992: 260:. Scientists specializing in aeronomy, known as 847: 518: 304:International Union of Geodesy and Geophysics 222: 913:(11) : 41-47. Available on-line at: 497:to gather data from the upper atmosphere. 229: 215: 782:157, (1946): 405. Available on-line at: 890: 724: 522: 390: 867: 623: 329: 993: 430:. Terrestrial aeronomy contrasts with 567: 500: 414:and is defined as consisting of the 872:. Physics of the Upper Atmosphere. 13: 410:to the atmosphere's boundary with 193:Glossary of tropical cyclone terms 14: 1037: 967: 952:, Berlin: Springer-Verlag, 2004, 426:and their ionized component, the 375:Aeronomy of Ice in the Mesosphere 973: 356: 347: 338: 27: 940: 929: 899: 244:is the scientific study of the 861: 791: 772: 745: 718: 650: 616:, the discovery since 1995 of 135:Climate variability and change 1: 711: 457:Terrestrial aeronomers study 986:The NOAA Aeronomy Laboratory 399:satellite in September 2005. 7: 664: 533:Upper-atmospheric lightning 519:Upper-atmospheric lightning 463:upper-atmospheric lightning 309: 10: 1042: 758:. Springer. pp. 1–2. 530: 504: 279: 203:Glossary of climate change 731:. Springer. pp. xi. 576:ground-based telescopes, 276:are important phenomena. 198:Glossary of tornado terms 868:Chapman, Sydney (1960). 643: 550:transient luminous event 383:polar mesospheric clouds 608:and techniques such as 465:discharges such as red 188:Glossary of meteorology 960:Accessed 23 March 2021 725:Brasseur, Guy (1984). 528: 400: 385:in Earth's atmosphere. 1001:Atmospheric chemistry 671:Atmospheric chemistry 598:optical spectrometers 562:Electromagnetic Pulse 560:perturbations due to 526: 394: 270:chemical dissociation 254:atmospheric chemistry 56:Atmospheric chemistry 1026:Atmospheric sciences 1011:Electrical phenomena 982:at Wikimedia Commons 755:Comparative Aeronomy 629:Comparative aeronomy 624:Comparative aeronomy 404:Terrestrial aeronomy 330:Terrestrial aeronomy 324:comparative aeronomy 316:terrestrial aeronomy 294:letter to the editor 288:introduced the term 44:Atmospheric dynamics 21:Atmospheric sciences 1006:Atmospheric physics 676:Atmospheric physics 537:Sprites (lightning) 258:atmospheric physics 39:Atmospheric physics 23: 573:Planetary aeronomy 568:Planetary aeronomy 558:Very-Low-Frequency 529: 401: 379:noctilucent clouds 320:planetary aeronomy 284:The mathematician 19: 978:Media related to 958:978-3-662-09362-7 883:978-0-12-582050-9 765:978-0-387-87824-9 738:978-94-009-6403-7 610:radio occultation 554:Emission of Light 501:Atmospheric tides 459:atmospheric tides 239: 238: 1033: 977: 961: 944: 938: 933: 927: 903: 897: 894: 888: 887: 865: 859: 854: 845: 844: 842: 840: 831:. Archived from 821: 800: 795: 789: 776: 770: 769: 749: 743: 742: 722: 658: 654: 606:plasma detectors 578:space telescopes 507:Atmospheric tide 495:sounding rockets 469:, sprite halos, 371:sounding rockets 360: 351: 342: 246:upper atmosphere 231: 224: 217: 98:Tropical cyclone 31: 24: 18: 1041: 1040: 1036: 1035: 1034: 1032: 1031: 1030: 991: 990: 970: 965: 964: 945: 941: 934: 930: 904: 900: 895: 891: 884: 866: 862: 855: 848: 838: 836: 823: 822: 803: 796: 792: 777: 773: 766: 750: 746: 739: 723: 719: 714: 667: 662: 661: 655: 651: 646: 634:magnetic fields 626: 594:interferometers 570: 539: 531:Main articles: 521: 509: 503: 389: 388: 387: 386: 363: 362: 361: 353: 352: 344: 343: 332: 312: 282: 235: 17: 12: 11: 5: 1039: 1029: 1028: 1023: 1018: 1013: 1008: 1003: 989: 988: 983: 969: 968:External links 966: 963: 962: 939: 928: 922:2012-05-27 at 898: 889: 882: 874:Academic Press 860: 846: 835:on 22 May 2013 801: 790: 771: 764: 744: 737: 716: 715: 713: 710: 709: 708: 703: 698: 693: 688: 683: 678: 673: 666: 663: 660: 659: 648: 647: 645: 642: 638:thermodynamics 625: 622: 569: 566: 520: 517: 505:Main article: 502: 499: 365: 364: 355: 354: 346: 345: 337: 336: 335: 334: 333: 331: 328: 311: 308: 286:Sydney Chapman 281: 278: 237: 236: 234: 233: 226: 219: 211: 208: 207: 206: 205: 200: 195: 190: 182: 181: 175: 174: 173: 172: 164: 163: 157: 156: 155: 154: 153: 152: 147: 140:Climate change 137: 132: 131: 130: 117: 116: 110: 109: 108: 107: 106: 105: 95: 94: 93: 88: 75: 74: 68: 67: 66: 65: 64: 63: 53: 52: 51: 41: 33: 32: 15: 9: 6: 4: 3: 2: 1038: 1027: 1024: 1022: 1021:Space physics 1019: 1017: 1014: 1012: 1009: 1007: 1004: 1002: 999: 998: 996: 987: 984: 981: 976: 972: 971: 959: 955: 951: 950: 943: 937: 932: 925: 924:archive.today 921: 918: 917: 916:Physics Today 912: 908: 907:Physics Today 902: 893: 885: 879: 876:. p. 4. 875: 871: 864: 858: 853: 851: 834: 830: 828: 820: 818: 816: 814: 812: 810: 808: 806: 799: 794: 787: 786: 781: 775: 767: 761: 757: 754: 748: 740: 734: 730: 727: 721: 717: 707: 704: 702: 701:Space physics 699: 697: 694: 692: 689: 687: 684: 682: 679: 677: 674: 672: 669: 668: 653: 649: 641: 639: 635: 630: 621: 619: 615: 611: 607: 603: 602:magnetometers 599: 595: 591: 587: 583: 579: 574: 565: 563: 559: 555: 551: 547: 544: 538: 534: 525: 516: 514: 508: 498: 496: 492: 488: 484: 480: 476: 472: 468: 464: 460: 455: 453: 449: 445: 441: 437: 433: 429: 425: 421: 417: 413: 409: 405: 398: 393: 384: 380: 376: 372: 368: 359: 350: 341: 327: 325: 321: 317: 307: 305: 301: 300: 295: 291: 287: 277: 275: 271: 267: 263: 259: 255: 251: 247: 243: 232: 227: 225: 220: 218: 213: 212: 210: 209: 204: 201: 199: 196: 194: 191: 189: 186: 185: 184: 183: 180: 177: 176: 171: 168: 167: 166: 165: 162: 159: 158: 151: 148: 146: 143: 142: 141: 138: 136: 133: 129: 126: 125: 124: 121: 120: 119: 118: 115: 112: 111: 104: 101: 100: 99: 96: 92: 89: 87: 84: 83: 82: 79: 78: 77: 76: 73: 70: 69: 62: 59: 58: 57: 54: 50: 47: 46: 45: 42: 40: 37: 36: 35: 34: 30: 26: 25: 22: 948: 942: 931: 915: 910: 906: 901: 892: 869: 863: 837:. 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Index

Atmospheric sciences

Atmospheric physics
Atmospheric dynamics
category
Atmospheric chemistry
category
Meteorology
Weather
category
portal
Tropical cyclone
category
Climatology
Climate
category
Climate variability and change
Climate change
category
portal
Aeronomy
Aeronomy
Glossary of meteorology
Glossary of tropical cyclone terms
Glossary of tornado terms
Glossary of climate change
v
t
e
upper atmosphere

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