Sentences with phrase «of turbulent ocean»

Visualized these stock markets may take the shape of a turbulent ocean with waves made of human hope, greed, and fear.

But there may be a way to cut drag force by almost 30 %, according to computer simulations of turbulent ocean - water flows reported in the 19 May issue of Science by mechanical engineer Yiqing Du of the Massachusetts Institute of Technology and applied mathematician George Karniadakis of Brown University.

Visualized, these stock markets may take the shape of a turbulent ocean with waves made of human hopes, dreams, greed and fear.

Not exact matches

Scientists don't fully understand what's driving Jupiter's strongest auroras, but data gathered by the orbiting Juno spacecraft hint that the electrons generating Jupiter's polar glows may be accelerated by turbulent waves in the planet's magnetic field — a process somewhat akin to surfers being driven shoreward ahead of breaking ocean waves, the researchers report today in Nature.

OFF the northernmost tip of Scotland, where the turbulent waters of the Atlantic Ocean meet those of the North Sea, sits a chain of 70 mostly uninhabited islands collectively known as Orkney.

A new study has found that turbulent mixing in the deep waters of the Southern Ocean, which has a profound effect on global ocean circulation and climate, varies with the strength of surface eddies — the ocean equivalent of storms in the atmosphere — and possibly also wind spOcean, which has a profound effect on global ocean circulation and climate, varies with the strength of surface eddies — the ocean equivalent of storms in the atmosphere — and possibly also wind spocean circulation and climate, varies with the strength of surface eddies — the ocean equivalent of storms in the atmosphere — and possibly also wind spocean equivalent of storms in the atmosphere — and possibly also wind speeds.

Another analogy is that emotions can be like turbulent waves thrashing about on the surface of the ocean.

Key West, Fla., sits at the southern most point of the continental U.S., right where America dips its big toe into the waters of both the turbulent Atlantic Ocean and the balmy Gulf of Mexico simultaneously.

Instead of the tranquil Caribbean Sea, the beaches face the Atlantic Ocean, which means that waters can be more turbulent, especially in the winter months.

Whether the installation represents the turbulent journey associated with cancer diagnosis or the infinite life of plastic garbage in our oceans, the installation's place suspended in the air serves as a symbolic reminder that pollution and cancer are issues hanging over all of our heads.

An arrangement of piano keys on the museum floor creates a visual experience that references turbulent ocean waves, splintered boards of a wrecked ship and slaves who lost their lives during the trans - Atlantic journey.

Attempting to bring the project full circle, Dodd presents the culmination of the turbulent journey through time and space set inside the grumbly, rumbling Catfish studio, its» belly burping and bumping along the ocean floor through heat and sleet, though coup to calm, through leaks, bursts, filibusters and b - flat notes, a kidneys» need, a tickle in the throat... and the final upheaval of the roaring storm whose ochre radius swung down and pointed with pin prick precision straight to Catfish and with the last clap of thunder deafly pronounced: «THE FOSS GOES ON!

My recent paintings and sculptures focus on the African - American experience of navigating public spaces while remaining buoyant within them... Working beyond the physical image of the body, objects of buoyancy, and navigation become metaphors for selfhood, resilience, and the sanity required in the turbulent oceans of contemporary America.»

For most of the catalog, the work depicts a chaotic and turbulent ocean swell accompanied with Pettibon's poetic text, but occasionally an image from the shore will appear to break the movement of riders crossing waves.

Jeremy Jackson, a lead author of the report, wrote a compelling piece on the findings for the Ocean Portal blog of the National Museum of Natural History that includes this vital line, which is in sync with my assertion that we can chart a «good» path in this turbulent Anthropocene era:

If Victor wasn't so stupid & trollish I would suggest Rob Painting's «How Increasing Carbon Dioxide Heats The Ocean» over on SkS and, by way of preparation, the added quote from IPCC AR5 WG1 3.4.1 «The net air — sea heat flux is the sum of two turbulent (latent and sensible) and two radiative (shortwave and longwave) components.»

Updated, 6:30 p.m. Earth's climate is shaped by the interplay of two complicated and turbulent systems — the atmosphere and oceans.

We need to be cognizant of everything from local - scale stable boundary layer micrometeorolgy and ocean unstable boundary layer turbulent processes to global oceanic and atmospheric circulation patterns such as the Arctic Oscillation and the Gulf Stream's seasonal evolution.

«The turbulent mixing in thin ocean surface boundary layers (OSBL), which occupy the upper 100 m or so of the ocean, control the exchange of heat and trace gases between the atmosphere and ocean.»

Ocean heat flux is a turbulent and complex system [7] which utilizes atmospheric measurement techniques such as eddy covariance to measure the rate of heat transfer expressed in the unit of joules or watts per second.

One the main key surface parameters involved in the exchange of energy between the atmosphere and oceans are: wind stress, surface turbulent latent and sensible heat fluxes.

These effects produced / induced in the Atmosphere can readily produce fluctuations in measure of «System Temperature» over a few Decades and even Centuries, whilst slower alterations to Turbulent Process in the liquid of the Ocean trend to produce fluctuation in measures of «System Temperature» over multiple Centuries.

Local changes to the atmospheric circulation are affected by turbulent fluxes of sensible and latent heat from the ocean to the atmosphere.

Energy may be stored, transported in various forms, and converted among the different types, giving rise to a rich variety of weather or turbulent phenomena in the atmosphere and ocean.

They are calculated as daily turbulent air - sea fluxes over global oceans with a spatial resolution of 0.25 ° in longitude and latitude.

ENSO is a product of changing turbulent flow rates between the ocean and the atmosphere.

Please refer to textbooks like the book of S.A. Thorpe The turbulent ocean, Cambridge University Press, 2005, 439 pages, for an explanation that the idea of a stratified ocean limited to a 50 m top layer is foreign to reality.

The air - sea interface «is typically the most turbulent part of the ocean,» Clayson said.

Brooks I. M., M. Tjernström, P. O. G. Persson, M. D. Shupe, R. A. Atkinson, G. Canut, C. E. Birch, T. Mauritsen, J. Sedlar and B. J. Brooks (September 2017): The Turbulent Structure of the Arctic Summer Boundary Layer During The Arctic Summer Cloud - Ocean Study.

But this is to do with turbulent motions of the ocean being transferred to the surface.

The ocean surface is a free surface thus the absence of turbulence at the ocean surface is due to a totally different mechanism to the absence of turbulence in the viscous sublayer of a turbulent boundary layer.

The atmosphere and the ocean are two interacting turbulent media with turbulent processes going on inside them, and there are all sorts and shapes of physical boundary (of the ocean in particular) that «contain'the eddies in a way that may or may not allow prediction of average conditions over areas less than the size of the earth.

IMO the process whose changes are most likely to be responsible for apparent changes to deep ocean heat content are changes to the nature of turbulent vertical mixing in specific areas of the world, especially the West Pacific / South China Sea, and perhaps the Caribbean and Gulf of Mexico.

People telling you they believe in G.H.G. Theory are ALL TRYING to TELL you a HIGHLY TURBULENT, WELL MIXED F.R.I.G.I.D, -15 degree OCEAN of GAS,

Chou, 2006: Decorrelation scales of high resolution turbulent fluxes at the ocean - surface and a method to fill - in gaps in satellite data products.

This breaking is often spectacular, with turbulent structures observed hundreds of meters above the seafloor, and driving turbulence dissipations and mixing up to 10,000 times open - ocean levels.