Echiche nke Iris

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Echiche iris bụ echiche nke Richard Lindzen et al. chepụtara na 2001 nke tụrụ aro ka okpomọkụ dị elu n'elu oké osimiri na okpomọkụ ga-eme ka igwe ojii cirrus belata ma si otú a nwekwuo radiation radiation na-agbapụta site na ikuku nke ụwa. Nnyocha ya banyere mgbanwe ndị a hụrụ na igwe ojii na mmetụta ndị a na-emepụta na radieshon infrared wepụtara na mbara igwe n'ihi ya kwadoro echiche ahụ.[1] Nke a na-atụ aro ntanye infrared radieshon bụ echiche na-adịghị mma nke ọkụ mbụ ga-eme ka ọ dị jụụ n'elu. Echiche nke nkwenye bụ na ụbara okpomọkụ dị n'elu oké osimiri ga-eme ka ígwé ojii na-arịwanye elu na mbara igwe na-ebelata radieshon infrared na ya mere nzaghachi dị mma.

Ndị ọkà mmụta sayensị ndị ọzọ mechara nwalee echiche ahụ. Ụfọdụ kwubiri na enweghị ihe akaebe na-akwado echiche ahụ.[2] Ndị ọzọ chọtara ihe àmà na-egosi na ụbara okpomọkụ dị n'elu oké osimiri na-ebelata n'ezie ígwé ojii cirrus mana ha chọpụtara na mmetụta ahụ bụ nzaghachi dị mma kama nzaghachi na-adịghị mma nke Lindzen chepụtara.[3][4]

Nnyocha e mere n'afọ 2007 nke Roy Spencer et al. mere site na iji data satellite emelitere nwere ike ịkwado echiche iris.[5] N'afọ 2011, Lindzen bipụtara nzaghachi nye nkatọ ndị bụ isi.[6] N'afọ 2015, e bipụtara akwụkwọ nke tụgharịrị aro ọzọ na enwere ike inwe "Iris Effect".[7] Ọ tụkwara aro ihe ọ kpọrọ "usoro anụ ahụ ezi uche dị na ya maka mmetụta iris". N'afọ 2017, e bipụtara akwụkwọ nke chọpụtara na "igwe ojii anvil cirrus nke okpomọkụ na-eme ka nzaghachi ihu igwe na-adịghị mma na njikọ siri ike na arụmọrụ mmiri ozuzo".[8] Ọ bụrụ na e kwenyesiri ike mgbe ahụ nchọpụta ahụ ga-akwado ịdị adị nke "Iris Effect".

Hụkwa[dezie | dezie ebe o si]

  • Echiche nke okpomọkụ anvil
  • Mgbasawanye ụwa
  • Okpomọkụ ụwa

Edensibia[dezie | dezie ebe o si]

  1. Lindzen, R.S., M.-D. Chou, and A.Y. Hou (2001). "Does the Earth have an adaptive infrared iris?". Bull. Amer. Meteor. Soc. 82 (3): 417–432. DOI:<0417:DTEHAA>2.3.CO;2 10.1175/1520-0477(2001)082<0417:DTEHAA>2.3.CO;2. 
  2. Hartman, D.L. (2002). "No evidence for iris". Bull. Amer. Meteor. Soc. 83 (2): 249–254. DOI:<0249:NEFI>2.3.CO;2 10.1175/1520-0477(2002)083<0249:NEFI>2.3.CO;2. 
  3. Fu, Q., Baker, M., and Hartman, D. L. (2002). "Tropical cirrus and water vapor: an effective Earth infrared iris feedback?". Atmos. Chem. Phys. 2 (1): 31–37. DOI:10.5194/acp-2-31-2002. 
  4. Lin, B., B. Wielicki, L. Chambers, Y. Hu, and K.-M. Xu (2002). "The Iris Hypothesis: A Negative or Positive Cloud Feedback?". J. Clim. 15 (1): 3–7. DOI:<0003:TIHANO>2.0.CO;2 10.1175/1520-0442(2002)015<0003:TIHANO>2.0.CO;2. 
  5. Spencer, R.W., Braswell, W.D., Christy, J.R., Hnilo, J. (2007). "Cloud and radiation budget changes associated with tropical intraseasonal oscillations". Geophys. Res. Lett. 34 (15): L15707. DOI:10.1029/2007GL029698. 
  6. Lindzen R.S. (2011). "On the observational determination of climate sensitivity and its implications". Asia-Pacific J. Atmos. Sci. 47 (4): 377–390. DOI:10.1007/s13143-011-0023-x. Retrieved on 2014-01-11. 
  7. Mauritsen T. (2015). "Missing iris effect as a possible cause of muted hydrological change and high climate sensitivity in models". Nature Geoscience 8 (5): 346–351. DOI:10.1038/ngeo2414. 
  8. Choi (2017). "Revisiting the iris effect of tropical cirrus clouds with TRMM and A-Train satellite data" (in en). Journal of Geophysical Research: Atmospheres 122 (11): 2016JD025827. DOI:10.1002/2016JD025827. ISSN 2169-8996. 

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