We combine satellite data
with ocean measurements to depths of 1,800 m, and show that between January 2001 and December 2010, Earth has been steadily accumulating energy at a rate of 0.50 + / - 0.43 Wm - 2 (uncertainties at the 90 % confidence level).
Not exact matches
Saildrone's fleet of sailboats — which are outfitted
with dozens of sensors,
measurement tools, and cameras — can capture data on fish and wildlife populations, environmental health,
ocean temperatures, weather, and climate change.
Thanks to Swarm's precise
measurements along
with those from Champ — a mission that ended in 2010 after measuring Earth's gravity and magnetic fields for more than 10 years — scientists have not only been able to find the magnetic field generated by
ocean tides but, remarkably, they have used this new information to image the electrical nature of Earth's upper mantle 250 km below the
ocean floor.
In recent years, buoy - based
measurements, thought to be more accurate as buoy sensors are in direct contact
with the
ocean surface, have grown in frequency, while ship - based
measurements have become less common.
To model the projected impact of climate change on marine biodiversity, the researchers used climate - velocity trajectories, a
measurement which combines the rate and direction of movement of
ocean temperature bands over time, together
with information about thermal tolerance and habitat preference.
They compared isotope
measurements on the silica skeletons of diatoms, which store environmental signals from the
ocean's surface,
with isotope signals from radiolarians, which live in deeper water layers.
«
With its dual view
measurement capability, it will be used to derive accurate surface temperature, a key parameter at the
ocean - atmosphere boundary.
Co-author Nerilie Abram, from the Australian National University, said: «In order to better understand climate change in Antarctica, we need continued climate
measurements in the Antarctic and Southern
Ocean, and extension of these short observational records
with past climate reconstructions and climate modelling.»
The new analysis combines sea - surface temperature records
with meteorological station
measurements and tests alternative choices for
ocean records, urban warming and tropical and Arctic oscillations.
Combining the seismic data
with measurements from sediment samples previously retrieved from this region through
ocean drilling, they found that while the thickness of the incoming sediment is similar offshore of Washington and Oregon, the compaction is very different.
Their simulations did not agree
with measurements of
ocean heat made by scientists since the 1970s, particularly in the Southern Hemisphere.
Deploying new sensors that drift
with sometimes strong currents (allowing better
measurement of marine snow than sensors placed on the
ocean floor or tethered to the surface), the team sampled the flora and fauna and measured the amount of falling carbon material captured to assess the role of the
ocean as a true carbon sink.
That same year a European probe that had traveled
with Cassini plunged into the thick, foggy atmosphere of the moon Titan and — together
with the mother ship's
measurements from above — found evidence of an
ocean of ammonia and water hidden beneath a stunning landscape of dunes, mountains, and rivers.
Dr Samantha Gibbs, from
Ocean and Earth Science at the University of Southampton, who was Dr O'Dea's PhD supervisor and co-author of the study, says: «A key objective was to record calcification in fossil coccolithophores in a way that enabled direct comparison
with measurements from living specimens.
The addition of Svalbard will allow the mission to collect data on sea ice and snow in a scarcely measured section of the Arctic
Ocean and its surrounding seas, along
with measurements of a few glaciers in the Svalbard archipelago.
TIMED will launch aboard a Boeing Delta 2 rocket along
with another spacecraft, called Jason 1, which will take
measurements of circulations in the Earth's
oceans for use in climate research.
To do this, they combined
ocean wave data available from
measurements taken by
ocean buoys,
with nonlinear analysis of the underlying water wave equations.
The NASA Plankton, Aerosol, Cloud,
Ocean Ecosystem (PACE) mission, with a target launch within the next 5 years, aims to make measurements that will advance ocean and atmospheric science and facilitate interdisciplinary studies involving the interaction of the atmosphere with ocean biological sys
Ocean Ecosystem (PACE) mission,
with a target launch within the next 5 years, aims to make
measurements that will advance
ocean and atmospheric science and facilitate interdisciplinary studies involving the interaction of the atmosphere with ocean biological sys
ocean and atmospheric science and facilitate interdisciplinary studies involving the interaction of the atmosphere
with ocean biological sys
ocean biological systems.
If we can also have confidence in GRACE
measurements, which give us the
ocean mass increasing (melting and...), is it possible to find a best estimation of OHC than
with XBT, ARGO,...?
«The challenge is really first understanding what the natural variability looks like in this data - poor region, and then making
measurements long enough that we can tease out the long - term
ocean acidification trend, which is this gradual increase through time,» he said «It's really hard to see
with just one or two years of data.»
With very little land area to soak up the sun, the ARM site
measurements gathered here were expected to emulate the larger
ocean area.
With this study, Severinghaus and colleagues have shown that
measurements of noble gases in the atmosphere provide the historical record long sought by the scientific community, and can be further optimized to gain insights into modern
ocean temperature changes as well.
Comparing the concentrations of all three
ocean - derived components
with satellite
measurements of cloud droplets, the researchers developed a new mathematical equation describing how the sulfates and organic matter relate to cloud droplet concentrations.
Coastal physical oceanography, subtidal circulation,
ocean observing systems, real - time surface buoy design, towable buoy designs, autonomous vehicles, surface current
measurements with HF RADAR, Doppler technology, oceanographic applications of artificial neural networks.
«2015 is likely to be the hottest year on record
with ocean surface temperatures at the highest level since
measurements began.
Ocean coverage by floats reached 90 % by 2005 [66],
with the gaps mainly in sea ice regions, yielding the potential for an accurate energy balance assessment, provided that several systematic
measurement biases exposed in the past decade are minimized [67]--[69].
The AVM 3D function is combined
with the ROV's camera to improve
measurement of distances on the
ocean floor.
Naturally, one can do better
with measurements of subsurface
ocean temperatures and glacier volume (which affects latent heat content of the Earth), but the surface temperature does pretty well for a start.
If we can also have confidence in GRACE
measurements, which give us the
ocean mass increasing (melting and...), is it possible to find a best estimation of OHC than
with XBT, ARGO,...?
Very recent, wide ranging review of temperature
measurements in the
oceans with a detailed discussion of the accuracy of the data, planetary energy balance and the effect of the warming on sea levels.
The mainstream media by and large got the story right — puzzling anomaly tracked down, corrections in progress after a little scientific detective work, consequences minor — even though a few headline writers got a little carried away in equating a specific dip in 1945
ocean temperatures
with the more gentle 1940s - 1970s cooling that is seen in the land
measurements.
[Response: You fail to see that
ocean temperatures, satellite
measurements, glacier melting, Arctic ice retreat, changes in phenology are all consistent
with a warming planet.
But what do cloud
measurements indicate for the
ocean regions
with most cooling?
But more important than agreement
with computer models is the fact that four years
with no warming in the upper
ocean does not erase the 50 years of warming we've seen since
ocean temperature
measurements became widespread....
The very first
measurements of deep
ocean temperatures were performed
with instruments lowered from a ship down into the
ocean.
By contrast, there is quite a lot of data now telling us that CO2 is not a climate driver: We did the experiment of adding a large slug of CO2 to the air and the temperature stopped rising in 1997, the stratosphere stopped cooling in 1995 and the
oceans showed no warming down to 700m when we replaced guesswork
with accurate
measurement in 2003.
Then, when combined
with the number of
measurements and uncertainties induces by thermal eddies and
ocean mixture, it is seems unlikely to me that
measurements can tease out the true OHC.
The work in question takes
measurements from one locale, and doesn't publish conclusions, rather Doney's statements are giving his opinion about what he read, «Long - term
ocean acidification trends are clearly evident over the past several decades in open -
ocean time - series and hydrographic survey data, and the trends are consistent
with the growth rate of atmospheric carbon dioxide (Dore et al., 2009).»
In your case, the ice cores must be wrong, in my case, there is no problem
with ice core CO2 (neither
with historical CO2 levels over the
oceans), as the 0.3 K temperature increase in the period 1900 - 1950 causes an increase of about 0.9 ppmv CO2, which is within the accuracy of the ice core
measurements, the rest of the observed increase is due to human emissions.
Most interesting is that the about monthly variations correlate
with the lunar phases (peak on full moon) The Helsinki Background
measurements 1935 The first background
measurements in history; sampling data in vertical profile every 50 - 100m up to 1,5 km; 364 ppm underthe clouds and above Haldane
measurements at the Scottish coast 370 ppmCO2 in winds from the sea; 355 ppm in air from the land Wattenberg
measurements in the southern Atlantic
ocean 1925-1927 310 sampling stations along the latitudes of the southern Atlantic oceans and parts of the northern; measuring all oceanographic data and CO2 in air over the sea; high ocean outgassing crossing the warm water currents north (> ~ 360 ppm) Buchs measurements in the northern Atlantic ocean 1932 - 1936 sampling CO2 over sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly av
ocean 1925-1927 310 sampling stations along the latitudes of the southern Atlantic
oceans and parts of the northern; measuring all oceanographic data and CO2 in air over the sea; high
ocean outgassing crossing the warm water currents north (> ~ 360 ppm) Buchs measurements in the northern Atlantic ocean 1932 - 1936 sampling CO2 over sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly av
ocean outgassing crossing the warm water currents north (> ~ 360 ppm) Buchs
measurements in the northern Atlantic
ocean 1932 - 1936 sampling CO2 over sea surface in northern Atlantic Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly av
ocean 1932 - 1936 sampling CO2 over sea surface in northern Atlantic
Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly av
Ocean up to the polar circle (Greenland, Iceland, Spitsbergen, Barents Sea); measuring also high CO2 near Spitsbergen (Spitsbergen current, North Cape current) 364 ppm and CO2 over sea crossing the Atlantic from Kopenhagen to Newyork and back (Brements on a swedish island Lundegards CO2 sampling on swedish island (Kattegatt) in summer from 1920 - 1926; rising CO2 concentration (+7 ppm) in the 20s; ~ 328 ppm yearly average
Comparisons of direct
measurements with satellite data and climate models suggest that the
oceans of the southern hemisphere have been sucking up more than twice as much of the heat trapped by our excess greenhouse gases than previously calculated.
This should be obvious from the fact that we can not determine the average temperature of the
ocean from 10
measurements with any accuracy or precision.
Ambient submicron particle
measurements were made
with a high - resolution time - of - flight aerosol mass spectrometer (AMS) at the north campus of the University of California Irvine, which is located in the SoCAB approximately 5 miles inland from the Pacific
Ocean.
The satellite
measurements are made from hundreds of miles above the
ocean while those made from ships are by direct contact
with the water.
A new NASA and University of Tasmania study combined the ship's 135 - plus - year - old
measurements of
ocean temperatures
with modern observations to get a picture of how the world's
ocean has changed since the Challenger's voyage.
Researchers from the University of Tasmania, Sandy Bay, Australia; and NASA's Jet Propulsion Laboratory, Pasadena, Calif., combined the ship's
measurements of
ocean temperatures
with modern observations from the international Argo array of
ocean profiling floats.
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.
The ARGO
measurements of
ocean temperatures
with depth shows that the seasonal variation penetrates hundreds of meters deep
with a lag of only a few months or around 3 months, 1/4 of a period, to be more precise.
The biggest change occurred in
measurement methodology and scope,
with the switch from tide gauges (which measure SL at various shorelines, where humans live) to satellite altimetry (which measures the entire
ocean except polar regions and coastlines, which can not be captured by satellites).
He should keep up
with the times there has been plenty of
measurement of the deep
ocean by several different bodies.