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  2. Chlorofluorocarbon - Wikipedia

    en.wikipedia.org/wiki/Chlorofluorocarbon

    Using CFCs or SF 6 as a tracer of ocean circulation allows for the derivation of rates for ocean processes due to the time-dependent source function. The elapsed time since a subsurface water mass was last in contact with the atmosphere is the tracer-derived age. [ 71 ]

  3. Chlorotrifluoromethane - Wikipedia

    en.wikipedia.org/wiki/Chlorotrifluoromethane

    Chlorotrifluoromethane, R-13, CFC-13, or Freon 13, is a non-flammable, non-corrosive, nontoxic chlorofluorocarbon (CFC) and also a mixed halomethane. It is a man-made substance used primarily as a refrigerant. When released into the environment, CFC-13 has a high ozone depletion potential, and long atmospheric lifetime. [2]

  4. Ozone depletion - Wikipedia

    en.wikipedia.org/wiki/Ozone_depletion

    Chlorofluorocarbons (CFCs) and other halogenated ozone-depleting substances (ODS) are mainly responsible for man-made chemical ozone depletion. The total amount of effective halogens (chlorine and bromine) in the stratosphere can be calculated and are known as the equivalent effective stratospheric chlorine (EESC).

  5. Ozone depletion and climate change - Wikipedia

    en.wikipedia.org/wiki/Ozone_depletion_and...

    Only methyl chloride, which is one of the halocarbons, has a mainly natural source, [40] and it is responsible for about 20% of the chlorine in the stratosphere; the remaining 80% comes from man-made sources. [41] Chlorofluorocarbons, in contrast, are insoluble and long-lived, allowing them to reach the stratosphere.

  6. Marine primary production - Wikipedia

    en.wikipedia.org/wiki/Marine_primary_production

    Ocean chlorophyll concentration as a proxy for marine primary production. Green indicates where there are a lot of phytoplankton, while blue indicates where there are few phytoplankton. – NASA Earth Observatory 2019. [1] Marine primary production is the chemical synthesis in the ocean of organic compounds from atmospheric or dissolved carbon ...

  7. Oceanic carbon cycle - Wikipedia

    en.wikipedia.org/wiki/Oceanic_carbon_cycle

    Particulate organic carbon can be classified, based on how easily organisms can break them down for food, as labile, semilabile, or refractory. Photosynthesis by phytoplankton is the primary source for labile and semilabile molecules, and is the indirect source for most refractory molecules.

  8. Altadena winds weren't strong enough to warrant Edison ... - AOL

    www.aol.com/news/altadena-winds-were-not...

    The head of Southern California Edison said Wednesday that winds blowing in Eaton Canyon on Jan. 7 were not strong enough to merit de-energizing a powerful electrical transmission line that is now ...

  9. Trace gas - Wikipedia

    en.wikipedia.org/wiki/Trace_gas

    The global ocean is also a source of several trace gases, in particular sulfur-containing gases. In situ trace gas formation occurs through chemical reactions in the gas-phase. [ 1 ] Anthropogenic sources are caused by human related activities such as fossil fuel combustion (e.g. in transportation ), fossil fuel mining, biomass burning , and ...