Sentences with phrase «stratospheric ozone recovery»

During the period of summer ozone recovery (2000 — 2050), the SAM index exhibits weakly negative, statistically insignificant trends due to stratospheric ozone recovery which offsets the positive forcing imposed by increasing GHG concentrations.
We determine its likely evolution for three intergovernmental panel on climate change (IPCC) special report on emission scenarios (SRES) for austral summer and winter, using a multi-model ensemble of IPCC fourth assessment report models which resolve stratospheric ozone recovery.
We therefore demonstrate that the future SAM will depend both upon GHG emissions and stratospheric ozone recovery.

Not exact matches

Stratospheric cooling as a result of excess CO2 does influence ozone recovery, and ozone changes in the troposphere and stratosphere to have effects on radiative balance of the planet.
We talk about the new paper «Evidence for a continuous decline in lower stratospheric ozone offsetting ozone layer recovery» as published February 6, 2018.
Increased polar stratospheric ozone losses and delayed eventual recovery owing to increasing greenhouse - gas concentration.
Chipperfield, M. P., Bekki, S., Dhomse, S., Harris, N. R. P., Hassler, B., Hossaini, R., Steinbrecht, W., Thiéblemont, R. and Weber, M.: Detecting recovery of the stratospheric ozone layer, Nature, 549, 211 — 218, doi: 10.1038 / nature23681, 2017.
Increased polar stratospheric ozone losses and delayed eventual recovery due to increasing greenhouse gas concentrations.
We talk about the new paper «Evidence for a continuous decline in lower stratospheric ozone offsetting ozone layer recovery» as published February 6, 2018.
These NOAA activities constitute a large part of the global scientific effort to understand stratospheric ozone depletion and recovery.
The scientific goal is to determine and interpret trends in global stratospheric ozone, the Antarctic ozone hole, and global atmospheric ozone depleting substances; to investigate these trends for signs of recovery of the ozone layer and evaluate implications for climate change; and to study the efficacy of newly proposed substitutes for currently used ozone - depleting substances.
This will make recovery of the stratospheric ozone layer much slower.
The trend of greater and greater depletion of global stratospheric ozone observed during the 1980s and 1990s is no longer occurring; however, it is not yet clear whether these recent changes are indicative of ozone recovery.
But not only must models of ozone loss and recovery factor in global warming — abnormally low stratospheric ozone has also a marked effect on climate change here and now.
The evolution of the forcing due to stratospheric O3 loss hinges on the rate of recovery of the ozone layer, with special regards to the spatial structure of such a recovery in the mid - to high latitudes.
Shindell, D.T., D. Rind, and P. Lonergan, 1998: Increased polar stratospheric ozone losses and delayed eventual recovery owing to increasing greenhouse - gas concentrations.
Ozone recovery in the tropical stratosphere is expected to be faster and the recovery of the polar ozone hole is expected to be slower because of the CO2 - induced cooling of the stratosphere (and increase the number of polar stratospheric cloOzone recovery in the tropical stratosphere is expected to be faster and the recovery of the polar ozone hole is expected to be slower because of the CO2 - induced cooling of the stratosphere (and increase the number of polar stratospheric cloozone hole is expected to be slower because of the CO2 - induced cooling of the stratosphere (and increase the number of polar stratospheric clouds).
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