ライフサイエンスコーパス: ozone depletion

1 cate that the eruptions led to stratospheric ozone depletion.

2 c geoengineering while reducing or reversing ozone depletion.

3 ere, it would have resulted in strong global ozone depletion.

4 ng to extremely large (up to 90%) short-term ozone depletion.

5 where they release chlorine atoms that cause ozone depletion.

6 nses to GHG forcing and the other resembling ozone depletion.

7 e anthropogenic enhancement of stratospheric ozone depletion.

8 ly unrecognized mechanisms for stratospheric ozone depletion.

9 understanding the processes responsible for ozone depletion.

10 a and were modeled under conditions of 5-20% ozone depletion.

11 increases in ultraviolet B radiation due to ozone depletion.

12 use of CFCs is phased out due to concerns of ozone depletion, a variety of new chemicals and technolo

13 oil, and omega-3 capsules to global warming, ozone depletion, acidification, eutrophication, energy u

14 or categories (climate change, stratospheric ozone depletion, agricultural intensification and expans

15 ar to those in our model integrations, where ozone depletion alone is prescribed.

16 concentrations have increased as a result of ozone depletion and burning of fossil fuels.

17 We use an empirical relationship between ozone depletion and chlorine activation to estimate how

18 enated organic compounds (VOX) contribute to ozone depletion and global warming.

19 nergistic interactions between stratospheric ozone depletion and greenhouse warming are possible.

20 ct of changes in both anthropogenic factors (ozone depletion and increases in well-mixed greenhouse g

21 ts significant contribution to stratospheric ozone depletion and its potent greenhouse effect, nitrou

22 Evidence of mid-latitude ozone depletion and proof that the Antarctic ozone hole

23 the Montreal Protocol due to concerns about ozone depletion and provide an illustration of how emiss

24 st air pollutants and many gases involved in ozone depletion and the greenhouse effect.

25 by more realistic treatment of stratospheric ozone depletion and volcanic aerosol forcing.

26 Modeling studies suggest that Antarctic ozone depletion and, to a lesser degree, greenhouse gas

27 drocarbons, and sulfur compounds involved in ozone depletion and/or climate forcing, from the very vo

28 n and ecotoxicity, global warming potential, ozone depletion, and acidification.

29 earlier than the first detectable Antarctic ozone depletion, and enhanced Antarctic ozone depletion

30 al warming, fossil depletion, acidification, ozone depletion, and photochemical ozone formation and a

31 by greenhouse gases, aerosols, stratospheric ozone depletion, and volcanic eruptions and a second sui

32 These levels of halogens cause substantial ozone depletion, as well as the rapid oxidation of dimet

33 es occupy the water column during periods of ozone depletion (austral spring) and lowest in fish spec

34 y to be the response to springtime Antarctic ozone depletion, but may be due in part to increasing at

35 n extremes, to address whether or not Arctic ozone depletion can be as extreme as that observed in th

36 posed that other climate influences--such as ozone depletion--could account for the discrepancy.

37 V radiation (UVB), a result of stratospheric ozone depletion during the austral spring, on the primar

38 would strongly increase the extent of Arctic ozone depletion during the present century for cold wint

39 Ozone depletion events can change the oxidative capacity

40 bromine chemistry has been shown to initiate ozone depletion events, and it has long been hypothesize

41 Antarctic ozone depletion has been suggested to be an important dr

42 Industrial chlorofluorocarbons that cause ozone depletion have been phased out under the Montreal

43 tropical circulation changes, resulting from ozone depletion, have substantially contributed to subtr

44 Climate change and ozone depletion impacts predicted for low-income nations

45 This work surveys the depth and character of ozone depletion in the Antarctic and Arctic using availa

46 These levels of bromine cause substantial ozone depletion in the lower stratosphere, and any incre

47 t few decades is marked by rapid cooling and ozone depletion in the polar lower stratosphere of both

48 Antarctic ozone depletion is associated with enhanced chlorine fro

49 rimary cause for the dramatic and persistent ozone depletion is heating of the stratosphere by smoke,

50 In addition, there is a growing belief that ozone depletion is of only minor environmental concern b

51 ting to the warming, including stratospheric ozone depletion, local sea-ice loss, an increase in west

52 t at present predict when such severe Arctic ozone depletion may be matched or exceeded.

53 increases in UV radiation from stratospheric ozone depletion needs to be completed.

54 aturally enhanced during several days due to ozone depletion on biomass production and photosynthesis

55 eir potential to contribute to stratospheric ozone depletion or global warming; HFCs do not contain c

56 compounds that are involved in stratospheric ozone depletion, originate from both natural and anthrop

57 o those associated with modern stratospheric ozone depletion over Antarctica-plausibly link the Mount

58 be explained as a response to stratospheric ozone depletion over Antarctica.

59 provide a fingerprint for the mechanisms of ozone depletion over the last two decades.

60 Due to concerns surrounding its ozone depletion potential, there is a need for technolog

61 By comparing the ozone depletion potential-weighted anthropogenic emissio

62 ide (N2 O) is a powerful greenhouse gas with ozone depletion potential.

63 ce separation reduced the global warming and ozone depletion potentials but increased terrestrial eco

64 I2 levels are able to significantly increase ozone depletion rates, while also producing iodine monox

65 ssions of N(2)O, a potent greenhouse gas and ozone depletion substance.

66 tial contributions of CH3Br to stratospheric ozone depletion, technologies for the capture and degrad

67 sport model, we demonstrate that much larger ozone depletion than observed has been avoided by the pr

68 ons demonstrate that the widespread and deep ozone depletion that characterizes the Antarctic ozone h

69 f six indicators, related to climate change, ozone depletion, the combined effects of acidification a

70 ical expansion in the Southern Hemisphere to ozone depletion, the drivers of Northern Hemisphere expa

71 The authors estimate that with 5-20% ozone depletion, there will be 167,000-830,000 additiona

72 ctic ozone depletion, and enhanced Antarctic ozone depletion through decreasing the lower stratospher

73 ronmental impacts, including global warming, ozone depletion, toxicity, and salinization, in addition

74 house gas and a major cause of stratospheric ozone depletion, yet its sources and sinks remain poorly