الغلاف الأوسط

(تم التحويل من Mesosphere)
هذا المقال هو عن طبقة في الغلاف الجوي. إذا كنت تريد الاستخدامات الأخرى، انظر الغلاف الأوسط (توضيح).
Earth's atmosphere as it appears from space, as bands of different colours at the horizon. From the bottom, afterglow illuminates the troposphere in orange with silhouettes of clouds, and the stratosphere in white and blue. Next the mesosphere (pink area) extends to just below the edge of space at one hundred kilometers and the pink line of airglow of the lower thermosphere (dark), which hosts green and red aurorae over several hundred kilometers.
مخطط يبين الطبقات الخمس الرئيسية الغلاف الجوي للأرض: exosphere, thermosphere, mesosphere, stratosphere, and troposphere. From Earths surface to the top of the stratosphere (50 كم) is just under 1% of Earth's radius.

الغلاف الأوسط ( Mesosphere ؛ /ˈmɛsəˌsfɪər,_ˈmɛzʔ,_ˈmiːsəʔ,_ʔzəʔ/;[1] من يونانية قديمة μέσος (mésos)، وتعني "middle", و -sphere)، هو الطبقة الثالثة من طبقات الغلاف الجوي، بين الطبقة الجوية العليا (الإستراتوسفير) والغلاف الحراري، وهي أعلى طبقة من الغلاف الجوي. وتبدأ حدود الغلاف الأوسط على ارتفاع 45 كم من سطح الأرض، وتمتد إلى مسافة 100 كيلو متر. In the mesosphere, temperature decreases as altitude increases. This characteristic is used to define limits: it begins at the top of the stratosphere (sometimes called the stratopause), and ends at the mesopause, which is the coldest part of Earth's atmosphere, with temperatures below −143 °C (−225 °F; 130 K). The exact upper and lower boundaries of the mesosphere vary with latitude and with season (higher in winter and at the tropics, lower in summer and at the poles), but the lower boundary is usually located at altitudes from 47 to 51 km (29 to 32 mi; 154,000 to 167,000 ft) above sea level, and the upper boundary (the mesopause) is usually from 85 to 100 km (53 to 62 mi; 279,000 to 328,000 ft).[2][3][4][5]

The stratosphere and mesosphere are sometimes collectively referred to as the "middle atmosphere",[6] which spans altitudes approximately between 12 and 80 km (7.5 and 49.7 mi) above Earth's surface. The mesopause, at an altitude of 80–90 km (50–56 mi), separates the mesosphere from the thermosphere—the second-outermost layer of Earth's atmosphere. On Earth, the mesopause nearly co-incides with the turbopause, below which different chemical species are well-mixed due to turbulent eddies. Above this level the atmosphere becomes non-uniform because the scale heights of different chemical species differ according to their molecular masses.

The term near space is also sometimes used to refer to altitudes within the mesosphere. This term does not have a technical definition, but typically refers to the region roughly between the Armstrong limit (about 62,000 ft or 19 km, above which humans require a pressure suit in order to survive) and the Kármán line (where astrodynamics must take over from aerodynamics in order to achieve flight); or, by another definition, to the space between the highest altitude commercial airliners fly at (about 40,000 ft (12.2 km)) and the lowest perigee of satellites being able to orbit the Earth (about 45 mi (73 km)). Some sources distinguish between the terms "near space" and "upper atmosphere", so that only the layers closest to the Kármán line are described as "near space".

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درجات الحرارة

وتقل درجة حرارة الجو في الغلاف الأوسط مع زيادة الارتفاع. وعند قاعدة الغلاف الأوسط يكون متوسط درجة الحرارة -2°م. وتصل أقل درجة حرارة للغلاف الجوي للأرض، عند قمة الغلاف الأوسط، وتسمى حد الغلاف الأوسط. وقد تنخفض درجة الحرارة لتصل إلى – 109°م، فوق القطبين الشمالي والجنوبي. وتوجد أقل درجات حرارة في منطـقة حد الغلاف الأوسط فـوق القطب في فصل الصيف.

ويعتقد العلماء أنّ الهواء في الغلاف الأوسط، قد يختلط، كما يحدث في الطبقة السفلى من الغلاف الجوي، والمعروفة باسم التروبوسفير. وتنخفض درجة الحرارة في كلا الطبقتين، مع ازدياد الارتفاع. وتهب الرياح القوية في الغلاف الأوسط. وإحدى الدلالات على حركة الهواء المتغيرة، في الغلاف الأوسط، تأتي نتيجة مشاهدة الآثار المتعرجة للشُّهب التي تمر من خلاله. وقد شوهدت غيوم رقيقة في الأقاليم القطبية للغلاف الأوسط أثناء فصل الصيف.


السمات الديناميكية

Afterglow of the troposphere (orange), the stratosphere (blue) and the mesosphere (dark) at which atmospheric entry begins, leaving smoke trails, such as in this case of a spacecraft reentry.

The main most important features in this region are strong zonal (East-West) winds, atmospheric tides, internal atmospheric gravity waves (commonly called "gravity waves"), and planetary waves. Most of these tides and waves start in the troposphere and lower stratosphere, and propagate to the mesosphere. In the mesosphere, gravity-wave amplitudes can become so large that the waves become unstable and dissipate. This dissipation deposits momentum into the mesosphere and largely drives global circulation.

Noctilucent clouds are located in the mesosphere. The upper mesosphere is also the region of the ionosphere known as the D layer, which is only present during the day when some ionization occurs with nitric oxide being ionized by Lyman series-alpha hydrogen radiation. The ionization is so weak that when night falls, and the source of ionization is removed, the free electron and ion form back into a neutral molecule.

A 5 km (3.1 mi; 16,000 ft) deep sodium layer is located between 80–105 km (50–65 mi; 262,000–344,000 ft). Made of unbound, non-ionized atoms of sodium, the sodium layer radiates weakly to contribute to the airglow. The sodium has an average concentration of 400,000 atoms per cubic centimetre. This band is regularly replenished by sodium sublimating from incoming meteors. Astronomers have begun utilizing this sodium band to create "guide stars" as part of the adaptive optical correction process used to produce ultra-sharp ground-based observations.[7] Other metal layers, e.g. iron and potassium, exist in the upper mesosphere/lower thermosphere region as well.

Beginning in October 2018,[8] a distinct type of aurora has been identified, originating in the mesosphere. Often referred to as 'dunes' due to their resemblance to sandy ripples on a beach, the green undulating lights extend toward the equator. They have been identified as originating about 96 km (60 mi; 315,000 ft) above the surface. Since auroras are caused by ultra-high-speed solar particles interacting with atmospheric molecules, the green color of these dunes has tentatively been explained by the interaction of those solar particles with oxygen molecules. The dunes therefore occur where mesospheric oxygen is more concentrated.[9]

Millions of meteors enter the Earth's atmosphere, averaging 40,000 tons per year.[10] The ablated material, called meteoric smoke, is thought to serve as condensation nuclei for noctilucent clouds.

الاستكشاف

The mesosphere lies above altitude records for aircraft,[11] while only the lowest few kilometers are accessible to balloons, for which the altitude record is 53.0 kilometres (32.9 mi).[12] Meanwhile, the mesosphere is below the minimum altitude for orbital spacecraft due to high atmospheric drag.[13][14][15] It has only been accessed through the use of sounding rockets, which are only capable of taking mesospheric measurements for a few minutes per mission.[16] As a result, it is the least-understood part of the atmosphere, resulting in the humorous moniker ignorosphere.[17][18] The presence of red sprites and blue jets (electrical discharges or lightning within the lower mesosphere), noctilucent clouds, and density shears within this poorly understood layer are of current scientific interest.

On February 1, 2003, مكوك فضاء كلومبيا broke up on reentry at about 62 km (39 mi) altitude, in the lower mesosphere, killing all seven crew members.

النيازك

تدخل ملايين النيازك الغلاف الجوي، بمتوسط 40 طن في اليوم.[19] ويذوب أو يتبخر معظمهم في الغلاف الأوسط نتيجة الاصطدام مع جسيمات الغاز المحتواة فيه. وينتج عن ذلك تركز أعلى من الحديد والمواد الحرارية الأخرى في تلك النيازك التي تصل الأرض.

ظواهر في الغلاف الأوسط والفضاء القريب

An astronaut onboard the International Space Station observes lightning at the horizon extending into the mesosphere as red sprite just below the line of airglow.
Noctilucent clouds (not to be mistaken with the slightly higher up airglow), at the upper edge of the mesosphere.

انظر أيضاً

المصادر

  1. ^ قالب:Cite Dictionary.com
  2. ^ "Middle atmosphere". www.antarctica.gov.au. Retrieved 17 June 2018.
  3. ^ Venkat Ratnam, M.; Patra, A. K.; Krishna Murthy, B. V. (25 March 2010). "Tropical mesopause: Is it always close to 100 km?". Journal of Geophysical Research. 115 (D6): D06106. Bibcode:2010JGRD..115.6106V. doi:10.1029/2009jd012531. ISSN 0148-0227.
  4. ^ "The Mesosphere - overview". scied.ucar.edu. UCAR Center for Science Education. Retrieved 17 June 2018.
  5. ^ von Zahn, U.; Höffner, J.; Eska, V.; Alpers, M. (1 November 1996). "The mesopause altitude: Only two distinctive levels worldwide?". Geophysical Research Letters. 23 (22): 3231–34. Bibcode:1996GeoRL..23.3231V. doi:10.1029/96gl03041. ISSN 0094-8276.
  6. ^ "Middle Atmosphere Meteorology". atmos.washington.edu. University of Washington. Retrieved 19 December 2018.
  7. ^ "Martin Enderlein et al., ESO's Very Large Telescope sees four times first light, Laser Focus World, July 2016, pp. 22-24".
  8. ^ The "dunes" were first spotted by photographers in Finland and Sweden.
  9. ^ "Wu, Katherine J. A New Type of Aurora Ripples Across the Sky in Horizontal Green "Dunes". Smithsonian Magazine (29 January 2020)".
  10. ^ Leinert C.; Gruen E. (1990). "Interplanetary Dust". Physics and Chemistry in Space (R. Schwenn and E. Marsch eds.). Springer-Verlag. pp. 204-275
  11. ^ "Powered Aeroplanes World Records". Fédération Aéronautique Internationale. Archived from the original on 11 September 2016. Retrieved 31 August 2016.
  12. ^ "Research on Balloon to Float over 50 km Altitude". Institute of Space and Astronautical Science, JAXA. Retrieved 29 September 2011.
  13. ^ "IADC Space Debris Mitigation Guidelines" (PDF). Inter-Agency Space Debris Coordination Committee. 15 October 2002. Archived from the original (PDF) on 3 December 2013. Retrieved 31 August 2016.
  14. ^ "NASA Safety Standard 1740.14, Guidelines and Assessment Procedures for Limiting Orbital Debris" (PDF). Office of Safety and Mission Assurance. 1 August 1995. Archived from the original (PDF) on 15 February 2013.
  15. ^ "100 km Altitude Boundary for Astronautics". Fédération Aéronautique Internationale.
  16. ^ "NASA Sounding Rocket Program Overview". NASA Sounding Rocket Program. NASA. 24 July 2006. Retrieved 10 October 2006.
  17. ^ "Reusable Rockets Set to Explore the 'Ignorosphere'". Discover Magazine. 1 September 2016. Retrieved 2 April 2018.
  18. ^ "Upper atmosphere may hold clues in Columbia mystery". 6 February 2003.
  19. ^ Leinert C.; Gruen E. (1990). "Interplanetary Dust". Physics and Chemistry in Space (R. Schwenn and E. Marsch eds.). Springer-Verlag. pp. 204--275

وصلات خارجية

قالب:Earth's atmosphere

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