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  2. Ground-level ozone - Wikipedia

    en.wikipedia.org/wiki/Ground-level_ozone

    The IPCC believes that "measured stratospheric O3 losses over the past two decades have generated a negative forcing of the surface-troposphere system" of around 0.15 0.10 watts per square metre (W/m 2). [39] Furthermore, rising air temperatures often improve ozone-forming processes, which has a repercussion on climate, as well.

  3. Ozone layer - Wikipedia

    en.wikipedia.org/wiki/Ozone_layer

    Effective presentation of information has also proven to be important in order to educate the general population of the existence and regulation of ozone depletion and contaminants. A scientific paper was written by Sheldon Ungar in which the author explores and studies how information about the depletion of the ozone, climate change , and ...

  4. Ozone - Wikipedia

    en.wikipedia.org/wiki/Ozone

    The move proved controversial, since the Agency's own scientists and advisory board had recommended lowering the standard to 60 nmol/mol. [106] Many public health and environmental groups also supported the 60 nmol/mol standard, [113] and the World Health Organization recommends 100 μg/m 3 (51 nmol/mol).

  5. Ozone and biology - Wikipedia

    en.wikipedia.org/wiki/Ozone_and_biology

    Ozone cycle illustrated over image by NASA astronaut Scott Kelly. Ozone is a ubiquitous yet highly reactive molecule in the atmosphere. Such a highly reactive oxidizer would normally be dangerous to life but ozone's concentration at sea level is usually not high enough to be toxic.

  6. Stratosphere - Wikipedia

    en.wikipedia.org/wiki/Stratosphere

    All air entering the stratosphere must pass through the tropopause, the temperature minimum that divides the troposphere and stratosphere. The rising air is literally freeze dried; the stratosphere is a very dry place. The top of the stratosphere is called the stratopause, above which the temperature decreases with height.

  7. Gulf of Mexico - Wikipedia

    en.wikipedia.org/wiki/Gulf_of_Mexico

    The Gulf of Mexico (Spanish: Golfo de México) is an oceanic basin and a marginal sea of the Atlantic Ocean, [3] [4] mostly surrounded by the North American continent. [5] It is bounded on the northeast, north, and northwest by the Gulf Coast of the United States; on the southwest and south by the Mexican states of Tamaulipas, Veracruz, Tabasco, Campeche, Yucatán, and Quintana Roo; and on the ...

  8. How does Formula 1 move cars between races? - AOL

    www.aol.com/news/does-formula-1-move-cars...

    How does F1 move cars between races? First of all, it depends on where the race is. Formula 1 calendars are typically structured around the European races which take place in the middle months of ...

  9. Atmosphere of Earth - Wikipedia

    en.wikipedia.org/wiki/Atmosphere_of_Earth

    The atmosphere of Earth is composed of a layer of gas mixture that surrounds the Earth's planetary surface (both lands and oceans), known collectively as air, with variable quantities of suspended aerosols and particulates (which create weather features such as clouds and hazes), all retained by Earth's gravity.