The integrated measures from large - scale
ocean salinity measurements are quite good, but it is difficult to work out exactly where that freshwater has come from.
«This study is the first to show the value of using
ocean salinity measurements to forecast the intensity of tropical cyclones,» said team lead Dr. Karthik Balaguru, an oceanographer at PNNL's Marine Sciences Laboratory.
Not exact matches
Its
measurements of
ocean saltiness will also help scientists understand how changes in
salinity affect the deep currents that drive
ocean circulation.
DeVries and fellow researchers Mark Holzer of the University of New South Wales in Sydney and François Primeau of UC Irvine compiled existing oceanographic tracer data —
measurements of temperature,
salinity, CFCs (humanmade gases that dissolve into the
ocean) and carbon - 14 — and separated it into three decade - long time periods: the 1980s, the 1990s and the 2000s.
Temperature and
salinity measurements averaged between 2010 and 2014 to show
ocean alkalinity.
The patterns of
salinity change can be used to infer changes in the Earth's hydrological cycle over the
oceans (Wong et al., 1999; Curry et al., 2003) and are an important complement to atmospheric
measurements.
There's no satellite in space that's capable of directly measuring
ocean acidity, but an international team of scientists writing in the journal Environmental Science & Technology described last week how satellite
measurements of sea surface temperatures,
salinity and plankton activity could be combined and used to estimate pH.
Yet
measurements from more than 3600 automated buoys throughout the
ocean that dive down a mile and a quarter and take detailed temperature and
salinity profiles every ten days show that the deeper strata are warming faster than the near - surface strata.
The principal scientific objective is to make global SSS
measurements over the ice - free
oceans with 150 - km spatial resolution, and to achieve a
measurement error less than 0.2 (PSS - 78 [practical
salinity scale of 1978]-RRB- on a 30 - day time scale, taking into account all sensors and geophysical random errors and biases.
Salinity is indeed a key indicator of the strength of the hydrologic cycle because it tracks the differences created by varying evaporation and precipitation, runoff, and ice processes.
To conduct the research, a team of scientists led by John Fasullo of the US National Center for Atmospheric Research in Boulder, Colorado, combined data from three sources: NASA's GRACE satellites, which make detailed
measurements of Earth's gravitational field, enabling scientists to monitor changes in the mass of continents; the Argo global array of 3,000 free - drifting floats, which measure the temperature and
salinity of the upper layers of the
oceans; and satellite - based altimeters that are continuously calibrated against a network of tide gauges.
Nonetheless, the findings demonstrate that satellite - based
measurements of Arctic sea surface
salinity are reasonably accurate and successfully reflect changes due to river runoff, melting sea ice and glaciers, and
ocean circulation.
These advances include the near - global three - dimensional sampling by the Argo array of temperature and
salinity profiling floats and spaceborne measurements of sea surface salinity using the European Space Agency's Soil Moisture and Ocean Salinity (SMOS) spacecraft and NASA's Aquarius mission aboard the Argentine SAC - D spacecraft (which ceased operations in Jun
salinity profiling floats and spaceborne
measurements of sea surface
salinity using the European Space Agency's Soil Moisture and Ocean Salinity (SMOS) spacecraft and NASA's Aquarius mission aboard the Argentine SAC - D spacecraft (which ceased operations in Jun
salinity using the European Space Agency's Soil Moisture and
Ocean Salinity (SMOS) spacecraft and NASA's Aquarius mission aboard the Argentine SAC - D spacecraft (which ceased operations in Jun
Salinity (SMOS) spacecraft and NASA's Aquarius mission aboard the Argentine SAC - D spacecraft (which ceased operations in June 2015).
Despite its importance,
ocean salinity in the Arctic has been poorly monitored because of the harsh environment and obstacles posed by sea ice, which impede field
measurements.
Any field - or ship - based updates on ice conditions in the different regions such as sea ice morphology (e.g., concentration, ice type, floe size, thickness, snow cover, melt pond characteristics, topography), meteorology (surface
measurements) and oceanography (e.g., temperature,
salinity, upper
ocean temperature).
Perhaps the
measurement of the distribution of the temperatures,
salinity and velocities fields in the
oceans will allow an estimate of the heat flux coming from the surface of the
ocean relative to that coming from the
ocean depths.
-- http://onlinelibrary.wiley.com/doi/10.1002/2015GL064541/abstract High - resolution
measurements of
ocean temperature and salinity in the Arctic Ocean's Canada Basin reveal the importance of the release of solar - derived stored ocean heat on sea - ice gr
ocean temperature and
salinity in the Arctic
Ocean's Canada Basin reveal the importance of the release of solar - derived stored ocean heat on sea - ice gr
Ocean's Canada Basin reveal the importance of the release of solar - derived stored
ocean heat on sea - ice gr
ocean heat on sea - ice growth.
Other new products are the
ocean reanalyses (ECCO for instance) that tries to take the same approach with
ocean temperature and
salinity measurements.