Sentences with phrase «more ocean mass»

They also found warming was twice as rapid in the Northern than the Southern hemisphere, due again to ocean dampening, since there is more ocean mass in the Southern than Northern hemisphere.

Not exact matches

Storm surge — the mass of water hurricanes push onshore from the ocean — will have a higher bed of water that will rush farther inland and destroy more property.
In a future which will increasingly be characterized by mass migration and the shifting of political borders, the Ocean Model of Civilisation can serve as a constructive paradigm for greater global security — especially its transcultural dimension — by promoting better and more dignified treatment of human beings, tolerance of diversity and respect for differences.
Using more than a dozen instruments placed around the habitat, including a first - of - its - kind underwater mass spectrometer that tracks fluctuations in key gases up and down the ocean waters, aquanauts watch readouts in real time on computer screens.
Jurgens said that is all the more reason why documenting such mass mortality events is important to better understand — and prepare for — trends happening to ocean ecosystems.
I'll add this: during some times when the oceans became more acidic because of high carbon in the atmosphere — there was a huge mass extinction event.
However, if the remaining ice shelf collapses or starts losing mass more rapidly, it could effectively unplug the glaciers next to the shelf, sending land - based ice into Southern Ocean, and contributing to sea level rise.
The planets» densities, now known much more precisely than before, suggest that some of them could have up to 5 percent of their mass in the form of water — about 250 times more than Earth's oceans.
Increased levels of atmospheric carbon dioxide could also significantly alter ocean temperatures and chemistry over the next century, which could lead to increased and more severe mass bleaching and other stressors on coral reefs.
The next step will be doing more lab experiments to determine what the critical mass for mixing is, as well as to actually head to sea and find out what happens in the open ocean.
The revised mass loss estimates will provide an important tool for researchers going forward as they estimate sea level rise as well as the potential for an even more dramatic slowdown in Atlantic ocean circulation.
The mass of cumulus clouds had increased in bulk more rapidly than any spawning storm she could remember in her eighteen years monitoring and forecasting tropical hurricanes in the Atlantic Ocean with the National Underwater and Marine Agency Hurricane Center.
Other works engage with the necessary conditions of life such as soil and, more prominently, water in an era marked by water reserve depletion, acidification of the oceans, rising sea levels, and mass extinction as well as the migration of people and species.
The non linear nature of forcing is related more to positive feedbacks and changes that are still being studied, such as cyclic changes in moisture content and regional dispersion, the methane cycles in the ocean or the potential of methane clathrate / hydrate release, and of course the race to feed more people on a planet which will inevitably add more nitrous oxide to the atmosphere and create more dead zones in the oceans, droughts, floods, fires, dogs and cats living together, mass hysteria....
Partly this has to do with changes in ocean circulation taking warmer water deeper and partly as the result of the southern hemisphere having less land mass and more ocean — where the ocean has a higher thermal inertia, meaning that it takes longer for those waters to warm.
A more saline ocean has less mass.
(More specifically, you've read it as supporting a * lag * in response, without considering that perhaps (given the physics of a high mass / high specific heat system like the oceans) what is really implied is, rather, a slow * rate * of response — but one which nevertheless «starts» immediately.)
For other areas, apparent local sea level rise will be a tad more since the oceans will increase in mass and drag the coasts down with them.
Re # 51: Because of the large thermal mass, the ocean is expected to warm more slowly than the land.
Hotter and more acidic oceans form a one - two punch that's killing off coral reefs, for example with the mass bleaching event that's currently ongoing.
For example: Sea level and temperature, ice mass, hurricanes (typhoons) wind and rain, Polar ice mass, Ice extent, CO2 Concentration, read some ocean buoys, read some tidal gauges, and much more are acceptable from the several hundred meteorological satellites..
bozzza - The differences in the Arctic are perhaps 1/4 the ocean thermal mass as global ocean averages, small overall size (the smallest ocean), being almost surrounded by land (which warms faster), more limited liquid interchanges due to bottlenecking than the Antarctic, and very importantly considerable susceptibility to positive albedo feedbacks; as less summer ice is present given current trends, solar energy absorbed by the Arctic ocean goes up very rapidly.
SLR by 2100 is more likely to come from ice mass loss from West Antarctica (WAIS) where warm ocean currents are already melting ice at glacier mouths and attacking areas of the WAIS resting on the seabed.
Notably, by studying the clouds over a limited region of the atmosphere over the eastern Pacific Ocean, as well as over nearby land masses, the team at the university's International Pacific Research Centre have declared themselves firmly in the latter camp, warning that, as temperatures continue to creep steadily upwards over the next 100 years, cloud cover will become thinner and more - sparse, thereby serving to exacerbate the problem.
The oceans are more acidic now than they have been for at least 300m years, due to carbon dioxide emissions from burning fossil fuels, and a mass extinction of key...
The impacts of ice shelf collapse and ensuing glacier acceleration are substantial, but in general, the effects of ocean melt are proving to be far more important in controlling ice sheet mass balance.
RIGHT NOW, you are expecting an air mass at an average 289K to more rapidly warm a higher thermal mass of the oceans at an average temperature of 294.2 K.
DMS is the primary source in the sulfate mass budget over the remote ocean west of 80 ° W. • The first aerosol indirect effect has been observationally quantified over the SEP, with cloud thinning of the more polluted coastal clouds mitigating the overall radiative impact.
SAL effects produce additional variations in ocean mass ranging from a few mm to more than 1 cm and can be of the same order of magnitude as the variations in dynamic bottom pressure in several ocean regions.
Because about halve the added CO2 as mass remains in the atmosphere, the total mass increases, which pushes more CO2 into the oceans and vegetation.
While many sources of stress have caused corals to bleach, «mass» coral bleaching (at scales of 100 km or more) has only occurred when anomalously warm ocean temperatures, typically coupled with high subsurface light levels, exceeded corals» physiological tolerances.
Once this La Nina faded, sea levels rebounded sharply, and that rise might have been incorrectly interpreted as some rapid acceleration in the long - term sea level rise, when in fact, mass was shifting back from land to ocean as rainfall patterns changed once more, but also much of the excess water on the land was draining back to the oceans.
The clear correlation between the net displacement of ocean water mass to land and the lower sea level during the last La Nina is a dynamical connection, showing far more than just «trend».
More than anything, this Grace data adds great credibility to the idea of filtering out these shorter - term ENSO effects in the shifts of water mass between ocean and land and back again.
For the US MIDWEST, the air masses from the Pacific first have to pass more than a thousand kilometres of mountains and thus the temperature trends in the US Midwest have unusually little noise from ocean air temperature trends.
Land mass and ocean mass surface thermal radiation are orders of magnitudes of more energy than the atmospheric thermal radiations.
They are both inconsistent with ARGO salinity data which shows that the ocean are getting more saline and therefore losing mass.
In Fig 22 you state that «air masses from the Pacific first have to pass more than a thousand kilometres of mountains and thus the temperature trends in the US Midwest have unusually little noise from ocean air temperature trends.»
Grace satellite data during the period of «the pause» is pretty convincing to many experts who believe the data pretty clearly displayed exactly where the mass was displaced to as ENSO related wind shifts caused more moisture to fall over land versus ocean.
Hot air masses from South Asia and Africa now sit over Siberia and the Russian Arctic (Pokrovsky) and in the first part of July low pressure has become more dominant in the central Arctic Ocean, which could set up northward drift along with warm air transport in the East Siberian and Laptev Seas (Maslanik).
Far more complex dynamics than one might assume — but the trend (and an accelerating one) is clear — more ice mass melting into water and flowing into the ocean.
AGW climate scientists seem to ignore that while the earth's surface may be warming, our atmosphere above 10,000 ft. above MSL is a refrigerator that can take water vapor scavenged from the vast oceans on earth (which are also a formidable heat sink), lift it to cold zones in the atmosphere by convective physical processes, chill it (removing vast amounts of heat from the atmosphere) or freeze it, (removing even more vast amounts of heat from the atmosphere) drop it on land and oceans as rain, sleet or snow, moisturizing and cooling the soil, cooling the oceans and building polar ice caps and even more importantly, increasing the albedo of the earth, with a critical negative feedback determining how much of the sun's energy is reflected back into space, changing the moment of inertia of the earth by removing water mass from equatorial latitudes and transporting this water vapor mass to the poles, reducing the earth's spin axis moment of inertia and speeding up its spin rate, etc..
- To investigate how a more realistic representation of sea ice drift affects the simulation of freshwater mass distribution in the Arctic Ocean.
I guess I could use the heat transfer rate to the ocean as a proxy and the mass of the ocean itself as a heat capacity, but I would like to know if something more formal exist in the scientific literature.
In the ocean and in the lakes, the coldest particles, or rather those whose density is the greatest, are continually tending downwards, and the motion of heat depending on this cause is much more rapid than that which takes place in solid masses in consequence of their connecting power.
when the ocean is warm and the arctic is open, it snows more and moves water mass from the oceans and adds ice mass on land and the axis does shift.
The oceans bulge out because the water is closer to the Moon than the greater mass of the Earth, and is therefore being pulled more strongly toward it.
Greenland's ice sheet has lost mass at an accelerated rate over the last decade, dumping more ice and fresh water into the ocean.
These reductions are more than just visual impressions but can dramatically alter the exchanges of mass, energy, and momentum between the atmosphere and ocean.
Feverishly hot ocean surface waters potentially reaching more than 104 degrees Fahrenheit (40 degrees Celsius) may have helped cause the greatest mass extinction in Earth's history, researchers say.
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