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  2. Ocean observations - Wikipedia

    en.wikipedia.org/wiki/Ocean_observations

    sea level JCOMM GLOSS Carbon VOS pCO2, SST, SSS IOCCP Sea ice buoys ... This is an example of quality control and monitoring of sea surface temperatures measured by ...

  3. Free Ocean CO2 Enrichment - Wikipedia

    en.wikipedia.org/wiki/Free_Ocean_CO2_Enrichment

    Free Ocean CO 2 Enrichment (FOCE) is ... the response of terrestrial plant communities to rising atmospheric CO 2 levels, ... to monitor local currents, temperature ...

  4. pCO2 - Wikipedia

    en.wikipedia.org/wiki/PCO2

    Conversely, a body of water with a pCO 2 greater than that of the atmosphere effluxes carbon dioxide. [4] [5] pCO 2 is additionally affected by water temperature and salinity. Carbon dioxide is less soluble in warmer water than cooler water, so hot water will exhibit a larger pCO 2 than cold water with the same concentration of carbon dioxide.

  5. Global Temperature-Salinity Profile Program - Wikipedia

    en.wikipedia.org/wiki/Global_Temperature...

    Making global measurements of ocean temperature and salinity (T-S) quickly and easily accessible to users is the primary goal of the GTSPP. Both real time data transmitted over the Global Telecommunications System (GTS), and delayed-mode data received by NCEI are acquired and incorporated into a continuously managed database.

  6. Martin curve - Wikipedia

    en.wikipedia.org/wiki/Martin_curve

    The Martin curve is a power law used by oceanographers to describe the export to the ocean floor of particulate organic carbon (POC). The curve is controlled with two parameters: the reference depth in the water column, and a remineralisation parameter which is a measure of the rate at which the vertical flux of POC attenuates. [1]

  7. Argo (oceanography) - Wikipedia

    en.wikipedia.org/wiki/Argo_(oceanography)

    At Ocean Station Papa in the Gulf of Alaska the temperature and salinity at the surface might be about 6°C and 32.55 parts per thousand giving a density of sea-water of 1.0256 g/cm 3. At a depth of 2000 metres (pressure of 2000 decibars) the temperature might be 2°C and the salinity 34.58 parts per thousand.

  8. Weather buoy - Wikipedia

    en.wikipedia.org/wiki/Weather_buoy

    Weather Buoy / Data Buoy / Oceanographic Buoy operated by the Marine Data Service. The first known proposal for surface weather observations at sea occurred in connection with aviation in August 1927, when Grover Loening stated that "weather stations along the ocean coupled with the development of the seaplane to have an equally long range, would result in regular ocean flights within ten years."

  9. Marine weather forecasting - Wikipedia

    en.wikipedia.org/wiki/Marine_weather_forecasting

    These stations observe ocean waves, tide levels, sea surface temperature and ocean current etc. in the Northwestern Pacific basin, as well as the Sea of Japan and the Sea of Okhotsk basin, and provide marine meteorological forecasts resulted from them, in cooperation with the Hydrographic and Oceanographic Department, Japan Coast Guard.