ライフサイエンスコーパス: stratospheric ozone

1 o periodic enhanced UV-B due to depletion of stratospheric ozone.

2 tent greenhouse gas (GHG) that also depletes stratospheric ozone.

3 t to the regulation of both tropospheric and stratospheric ozone.

4 esterlies, largely in response to changes in stratospheric ozone.

5 e through radiative warming and depletion of stratospheric ozone.

6 for most of the anthropogenic destruction of stratospheric ozone.

7 gas that also plays a role in the cycling of stratospheric ozone.

8 se gases, tropospheric sulfate aerosols, and stratospheric ozone.

9 f increasing greenhouse gases and decreasing stratospheric ozone and is predicted to continue by the

10 y, and may be related to human influences on stratospheric ozone and/or atmospheric greenhouse gas co

11 mical reactions-specifically those producing stratospheric ozone-and providing the major source of he

12 o a significant decline from 2004 to 2007 in stratospheric ozone below an altitude of 45 km, with an

13 orocarbons (CFCs) contribute to depletion of stratospheric ozone, CFC-containing metered-dose inhaler

14 on of stratospheric chemistry show how upper stratospheric ozone changes may amplify observed, 11-yea

15 ing (i.e. chlorine and bromine) compounds in stratospheric ozone chemistry and climate forcing is poo

16 s, which individually impact global climate, stratospheric ozone concentration, or local photochemist

17 rctic, essentially complete removal of lower-stratospheric ozone currently results in an ozone hole e

18 Implicated as a stratospheric ozone-depleting compound, methyl bromide (

19 that strong synergistic interactions between stratospheric ozone depletion and greenhouse warming are

20 Due to its significant contribution to stratospheric ozone depletion and its potent greenhouse

21 to be reduced by more realistic treatment of stratospheric ozone depletion and volcanic aerosol forci

22 ities of mid-UV radiation (UVB), a result of stratospheric ozone depletion during the austral spring,

23 s syndrome to increases in UV radiation from stratospheric ozone depletion needs to be completed.

24 and reduces their potential to contribute to stratospheric ozone depletion or global warming; HFCs do

25 pics-similar to those associated with modern stratospheric ozone depletion over Antarctica-plausibly

26 and summer can be explained as a response to stratospheric ozone depletion over Antarctica.

27 000 in six major categories (climate change, stratospheric ozone depletion, agricultural intensificat

28 models forced by greenhouse gases, aerosols, stratospheric ozone depletion, and volcanic eruptions an

29 ed as contributing to the warming, including stratospheric ozone depletion, local sea-ice loss, an in

30 ride (CH3Cl), compounds that are involved in stratospheric ozone depletion, originate from both natur

31 e to the potential contributions of CH3Br to stratospheric ozone depletion, technologies for the capt

32 powerful greenhouse gas and a major cause of stratospheric ozone depletion, yet its sources and sinks

33 radiation indicate that the eruptions led to stratospheric ozone depletion.

34 ributors to the anthropogenic enhancement of stratospheric ozone depletion.

35 nt to previously unrecognized mechanisms for stratospheric ozone depletion.

36 romethane (CH3Cl) plays an important role in stratospheric ozone destruction, but many uncertainties

37 N(2)O), a greenhouse gas that contributes to stratospheric ozone destruction.

38 e gas that contributes to climate change and stratospheric ozone destruction.

39 To assess the effect of this trend on stratospheric ozone, estimates of the future stratospher

40 eloped a method for diagnosing the amount of stratospheric ozone in these UT parcels using the compac

41 on precipitation and severe depletion of the stratospheric ozone layer in the Northern Hemisphere.

42 Accordingly, the stratospheric ozone layer is expected to recover.

43 The threat N2O poses to the stratospheric ozone layer, coupled with the uncertain fu

44 source of odd-hydrogen radicals, destroy the stratospheric ozone layer, such that Earth's surface rec

45 The recognition that CFCs destroy the stratospheric ozone layer, with consequent enormous cons

46 unted for when studying the evolution of the stratospheric ozone layer.

47 known remaining anthropogenic threat to the stratospheric ozone layer.

48 2005 in the USA, because it can deplete the stratospheric ozone layer.

49 known to affect ENSO strength by modulating stratospheric ozone levels (OEI = 6 and (17)O = 3.3 per

50 ), and third and fourth quartile mean annual stratospheric ozone levels but increased with second, th

51 x, clear sky and issued ultraviolet indices, stratospheric ozone levels, and outdoor air temperature

52 , controlled substances due to their role in stratospheric ozone loss, also occur as dissolved contam

53 le the 1991 eruption of Pinatubo resulted in stratospheric ozone loss, it was due to heterogeneous ch

54 on and destruction, photooxidant cycling and stratospheric ozone loss.

55 ons of increased N(2)O abundance, leading to stratospheric ozone (O(3)) depletion, altered solar ultr

56 s the photochemical coupling between N2O and stratospheric ozone (O3), which can easily be decomposed

57 ntemporary cities to calculate the impact on stratospheric ozone of a regional nuclear war between de

58 upon the same reaction network that reduces stratospheric ozone over the Arctic.

59 , augments the greenhouse effect, diminishes stratospheric ozone, promotes smog, contaminates drinkin

60 This usage carries potential for stratospheric ozone reduction due to Br atom catalysis,

61 ll force SAM into its positive phase even if stratospheric ozone returns to normal levels, so that cl

62 ugh a photochemical reaction network linking stratospheric ozone to carbon dioxide and to oxygen.

63 at simulated changes in solar irradiance and stratospheric ozone was used to investigate the response

64 h this, models project a gradual increase in stratospheric ozone with the Antarctic ozone hole expect