ライフサイエンスコーパス: ozone depletion

1 hieve a quantitative understanding of global ozone depletion.

2 ovide a quantitative understanding of global ozone depletion.

3 cate that the eruptions led to stratospheric ozone depletion.

4 c geoengineering while reducing or reversing ozone depletion.

5 so been speculated to have led to wide-scale ozone depletion.

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

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

8 where they release chlorine atoms that cause ozone depletion.

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

10 e anthropogenic enhancement of stratospheric ozone depletion.

11 ly unrecognized mechanisms for stratospheric ozone depletion.

12 understanding the processes responsible for ozone depletion.

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

14 increases in ultraviolet B radiation due to ozone depletion.

15 l) significantly contribute to stratospheric ozone depletion.

16 spectively, which can catalyze stratospheric ozone depletion.

17 entrations have contributed to stratospheric ozone depletion(1) and climate change(2), with the curre

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

19 with regard to human health, air pollution, ozone depletion, acidification, and land transformation.

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

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

22 ting greenhouse gas emissions and addressing ozone depletion, aligning significantly with the UN's su

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

24 otentially lowering environmental risks like ozone depletion and absorption of radiation.

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

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

27 from these banks, and associated impacts on ozone depletion and climate change.

28 eatly improves quantitative understanding of ozone depletion and climate in the global lower stratosp

29 The IOD measures the time-integrated column ozone depletion and depends only on the emission strengt

30 h provide fingerprints for the mechanisms of ozone depletion and examine the impact of nonhalogen gre

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

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

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

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

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

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

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

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

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

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

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

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

43 s of methane, nitrogen oxides, stratospheric ozone depletion, and global warming driving these trends

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

45 issions contribute 50-99% to global warming, ozone depletion, and smog impacts.

46 Chlorine oxides play crucial roles in ozone depletion, and the final oxidation steps of chlori

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

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

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

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

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

52 ratosphere, but these are only effective for ozone depletion chemistry at temperatures below about 19

53 e aerosols affect stratospheric chlorine and ozone depletion chemistry.

54 in the context of stratospheric chlorine and ozone depletion chemistry.

55 re, using a modelling framework that couples ozone depletion, climate change, damage to plants by ult

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

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

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

59 Following complete ozone depletion, elevated bromine concentrations are sus

60 Ozone depletion events can change the oxidative capacity

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

62 he stratosphere would result in catastrophic ozone depletion, extending the surface cooling caused by

63 x key ones: net energy, climate change (CC), ozone depletion, fine particulate matter formation, mari

64 une also has a lower impact in stratospheric ozone depletion, fine particulate matter formation, terr

65 tmosphere, resulting in severe stratospheric ozone depletion for several years.

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

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

68 halogen gases responsible for stratospheric ozone depletion have been regulated under the Protocol,

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

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

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

72 established that these trends were driven by ozone depletion in the Antarctic stratosphere due to emi

73 ons, including the previously reported large ozone depletion in the lower stratosphere over the tropi

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

75 roduction, compensating for up to 70% of the ozone depletion in the lower stratosphere.

76 smoke into the stratosphere, causing strong ozone depletion in the lower stratosphere.

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

78 Instead, we propose the use of an integrated ozone depletion (IOD) metric to indicate the impact of a

79 Antarctic ozone depletion is associated with enhanced chlorine fro

80 deterioration induced by massive magmatism, ozone depletion is considered a compelling ecological dr

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

82 oduction is sustained, any associated future ozone depletion is likely to be limited, despite an incr

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

84 Yet, although our main concern about ozone depletion is the subsequent increase in harmful so

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

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

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

88 plume created the ideal conditions for swift ozone depletion of 5% in the tropical stratosphere in ju

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

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

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

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

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

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

95 Reduced ozone depletion potential for VRFB and LFP can be achiev

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

97 By comparing the ozone depletion potential-weighted anthropogenic emissio

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

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

100 Ozone depletion potentials(2-4), relative measures of co

101 iable, our calculated results of time-series ozone depletion rates in global regions in the 1960s, 19

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

103 kg of carbon dioxide equivalents [CO(2)e]), ozone depletion, smog formation, acidification, eutrophi

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

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

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

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

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

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

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

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

112 en electron-induced reaction (CRE) theory of ozone depletion to obtain a quantitative understanding o

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

114 , especially in Antarctica, where effects of ozone depletion were larger.

115 f the unaccounted emissions on stratospheric ozone depletion, with implications for the Montreal Prot

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

117 er stratospheric cooling-primarily caused by ozone depletion-yields [Formula: see text] values betwee