Sentences with phrase «ozone in the stratosphere»

Normally, the amount of ozone in the stratosphere ranges from 30 to 100 ozone particles per billion air molecules.

When the sun is at its most intense, ozone in the stratosphere absorbs more ultraviolet energy, making areas near the equator warmer than usual.

What studies have been done in the paleo record regarding CO2 effects on ozone in the stratosphere and how it affected life?

Natural capital degradation: simplified summary of how chlorofluorocarbons (CFCs) and other chlorine - containing compounds can destroy ozone in the stratosphere faster than it is formed.

Some experts predicted that the depletion of ozone in the stratosphere due to the exhausts from the SST would produce about 10,000 additional cases of skin cancer in the world.

On Earth, temperature inversion occurs because ozone in the stratosphere absorbs much of the sun's ultraviolet radiation, preventing it from reaching the surface, protecting the biosphere, and therefore warming the stratosphere instead.

At precisely these altitudes, the amount of ozone in the stratosphere declined between three and six months after the eruption.

Unlike ozone in the stratosphere, which benefits life on Earth by blocking ultraviolet radiation from the Sun, ground - level ozone can trigger a number of health problems.

Scientists first noticed a dramatic thinning of ozone in the stratosphere about 6 miles above Antarctica in the mid 1980s.

The height of the tropopause is set by ozone in the stratosphere reacting directly with incoming solar energy so as to create a temperature inversion that blocks further upward convection.

Ozone climatology: Some chemistry / aerosol models will run with interactive stratospheric chemistry while others will prescribe ozone in the stratosphere and only run with detailed tropospheric chemistry.

'' «It all amounts to a mystery, but a troubling one because ozone protects life at the surface from incoming ultraviolet radiation, and any thinning of total ozone in the stratosphere is cause for concern.

The abnormally high quantities of atmospheric chlorine and bromine began altering the balance of ozone in the stratosphere so as to dramatically thin the ozone layer.

Ozone in the stratosphere protects earth from radiation (otherwise we would all be fried double quick) but in the troposphere it becomes a GHG, adding to the woes created by carbon dioxide, methane and nitrous oxide.

22 Ozone in the stratosphere filters out much of the harmful ultraviolet radiation from the sun View Figure 25 on page 379 of your textbook In the 1970s scientists noticed that the ozone layer over Antarctica was growing thinner OZONE DEPLETION

Here, a color - coded map showing Earth's north polar region and very low ozone in the stratosphere at an altitude of 12 miles (20 kilometers) in mid-March 2011, the peak of ozone loss.

Shorter wavelengths (UV) generate ozone in the stratosphere and penetrate the ocean.

33 OZONE DEPLETION IN THE STRATOSPHERE Less ozone in the stratosphere allows for more harmful UV radiation to reach the earth's surface.

Dr. Okano is the first to observe height profiles of ozone in the stratosphere from the ground with laser heterodyne spectroscopy.

The meeting was the first large - scale attempt to bridge the gap between scientists and policymakers on a wide range of atmospheric problems, including not just the greenhouse effect but also acid rain and the depletion of the protective layer of ozone in the stratosphere.

It is therefore very important to consider the effect of solar proton events on the temporal and spatial distribution of ozone in the stratosphere.

OMPS is a three - part instrument: a nadir mapper that maps ozone, SO2 and aerosols; a nadir profiler that measures the vertical distribution of ozone in the stratosphere; and a limb profiler that measures aerosols in the upper troposphere, stratosphere and mesosphere with high vertical resolution.

There isn't a lot of ozone in the stratosphere, but what is there performs a very important task for living creatures on the surface of the planet.

I could go through a dozen... examples: the skill associated with solar cycles, changing the ozone in the stratosphere; the skill associated with orbital changes over 6,000 years.

Ozone in the stratosphere is constantly being created and destroyed by the action of light and photochemistry.

NOAA is charged to track the amount of ozone in the stratosphere (referred to here as the «thickness» of the stratospheric ozone layer, and the atmospheric burden of ozone - depleting compounds and their alternatives.

The presence of a layer of ozone in the stratosphere is the cause of the temperature inversion that forms at the tropopause.

The stratospheric ozone tracer is defined as equal to ozone in the stratosphere, and including standard ozone removal (but not production) in the troposphere, where the tropopause is the WMO meteorological tropopause.

As an example, variations in the flow of both UV radiation and atomic particles that accompany changes in overall solar activity alter the amount of ozone in the stratosphere.

We know, for example, that the enhanced UV radiation that pours outward from the Sun at times of high solar activity increases the amount of ozone in the stratosphere.

Water vapor and ozone in the stratosphere can have a large impact on Earth's climate.

Dr. Molina won the Nobel Prize in Chemistry in 1995 for discovering that chloroflourocarbons (CFCs)-- then common in refrigerators, air conditioners, and hair spray — were destroying the protective layer of ozone in the stratosphere.

Chlorofluorocarbon (CFCs) have lowered the average concentrations of ozone in the stratosphere.