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Journal ArticleDOI

Measured Trends in Stratospheric Ozone

TLDR
Analysis of updated ozone records, including 29 stations in the former Soviet Union, and analysis of independently calibrated satellite data records confirm many of the findings originally derived from the Dobson record concerning northern midlatitude changes in ozone.
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Soil microorganisms as controllers of atmospheric trace gases (H2, CO, CH4, OCS, N2O, and NO).

TL;DR: It is completely unclear how important microbial diversity is for the control of trace gas flux at the ecosystem level, and different microbial communities may be part of the reason for differences in trace gas metabolism, e.g., effects of nitrogen fertilizers on CH4 uptake by soil; decrease of CH4 production with decreasing temperature.
Journal ArticleDOI

Evidence for Large Upward Trends of Ultraviolet-B Radiation Linked to Ozone Depletion

TL;DR: Spectral measurements of ultraviolet-B radiation made at Toronto since 1989 indicate that the intensity of light at wavelengths near 300 nanometers has increased by 35 percent per year in winter and 7 percent peryear in summer.
Journal ArticleDOI

Complex causes of amphibian population declines

TL;DR: Climate-induced reductions in water depth at oviposition sites have caused high mortality of embryos by increasing their exposure to UV-B radiation and, consequently, their vulnerability to infection, indicating the role of large-scale climatic patterns involving the tropical Pacific.
Journal ArticleDOI

Arabidopsis Mutants Lacking Phenolic Sunscreens Exhibit Enhanced Ultraviolet-B Injury and Oxidative Damage

TL;DR: Results demonstrate that, in A. thaliana, hydroxycinnamates are more effective UV-B protectants than flavonoids, and indicate that A.Thaliana responds toUV-B as an oxidative stress, and sunscreen compounds reduce the oxidative damage caused by UV- B.
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Journal ArticleDOI

Stratospheric sink for chlorofluoromethanes: chlorine atomc-atalysed destruction of ozone

TL;DR: Chlorofluoromethanes are being added to the environment in steadily increasing amounts as discussed by the authors and these compounds are chemically inert and may remain in the atmosphere for 40 to 150 years, and concentrations can be expected to reach 10 to 30 times present levels.
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Large losses of total ozone in Antarctica reveal seasonal ClOx/NOx interaction

TL;DR: In this article, it was shown that the very low temperatures which prevail from midwinter until several weeks after the spring equinox make the Antarctic stratosphere uniquely sensitive to growth of inorganic chlorine, ClX, primarily by the effect of this growth on the NO2/NO ratio.
Journal ArticleDOI

Reduction of stratospheric ozone by nitrogen oxide catalysts from supersonic transport exhaust.

TL;DR: The projected increase in stratospheric oxides of nitrogen could reduce the ozone shield by about a factor of 2, thus permitting the harsh radiation below 300 nanometers to permeate the lower atmosphere.
Journal ArticleDOI

Total ozone trends deduced from Nimbus 7 TOMS data

TL;DR: In this article, a statistical model, including terms for seasonal variation, linear trend, quasi-biennial oscillation, solar cycle and second-order autoregressive noise has been fit to the TOMS time series of total ozone data.
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The mystery of the Antarctic Ozone “Hole”

TL;DR: In this paper, the authors reviewed observations of the total ozone column and its vertical profile over Antarctica, and the current status of the evidence supporting various theories of the behavior of ozone in the Antarctic is summarized.
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