Not exact matches
Now that you, O sage, have yourself crossed the
ocean of the
world of becoming, please rescue also the other living beings who have
sunk so deep into suffering!
The Southern
Ocean sink strength is, at present, determined by the winds in that part of the
world.
At various points in Earth's history, dust fell into the
ocean and fed algae, which gobbled up carbon dioxide and
sank to the bottom of the sea, taking greenhouse gas with them and cooling the
world.
Small filter - feeding animals in the
world's
oceans take in bits of plastic and excrete them in pellets that
sink to the
ocean floor.
«It essentially means that, through multiple means, in a
world with mixotrophs, more organic carbon is
sinking into the deep
ocean than in a
world without mixotrophs,» Follows says.
Here was a gigantic laboratory flask with a whole tropical forest and an
ocean inside it — models of what many scientists suspected were the two biggest carbon
sinks in the
world.
And the warming of the upper 2 kilometers of the
world ocean — a huge heat
sink relative to the atmosphere — continued apace through the 2000s.
Their effect was only to expand the
world's calcium carbonate
sinks from the shallow continental shelves to some of the deeper
ocean (Westbroek 1991).»
Of the carbon that gets pumped into the air, about 30 to 40 percent
sinks into the
world's
oceans, lowering the pH of the water and making it more acidic each year.
Set your gaze to the
ocean horizon on Maui's south shore, and there, about 3 miles off in the distance, you'll spot the half -
sunken cinder cone MOLOKINI, a
world - class snorkel and dive location that can be reached only by boat.
Perhaps Zanzibar's pristine beaches and azure Indian
Ocean would have been the perfect place for some to let the excitement of the safari
sink in before returning to the working
world.
We offer the PADI referral course over just two days (4
Ocean Dives) and includes dives at some of Bali's best dive sites around Padang Bai and Tulamben, most notably the ship wreck of the USAT Liberty ship wreck,
sunk during
World War 2.
As sims tend to be, it was as slow as you can imagine as you sail the waters of the Pacific
Ocean during
World War II and finding enemy ships to
sink with your torpedoes by utilizing realistic tactics, hoping that they don't do the same to you in the process.
Photos by Hiroshi Sugimoto document famous Pequod locales (the Nantucket site from which it launched and the Pacific
Ocean, where it
sank), Argentine artist Adrián Villar Rojas crafts a giant clay sculpture of a white whale in real time, Angela Bulloch contemplates the night sky, and Kirsten Pieroth collects samples of water from the
world's
oceans.
Whereas PPM Data is immediate and accurately measurable and comparable to the «real
world» be it back to human emissions, be it sources, be it
sinks, be it
ocean acidity, be it climate forcing long term and more than anything the dynamics of PPM is easily explained and communicated as a Definitive Yardstick or success or failure in meeting Goals (imho).
Many of the surface currents of the
world oceans (i.e., the
ocean «gyres» which appear as rotating horizontal current systems in the upper
ocean) are driven by the wind, however, the
sinking in the Arctic is related to the buoyancy forcing (effects that change either the temperature or salinity of the water, and hence its buoyancy).
For example, conditions at the poles affect how much heat is retained by the earth because of the reflective properties of ice and snow, the
world's
ocean circulation depends on
sinking in polar regions, and melting of the Antarctic and Greenland ice sheets could have drastic effects on sea level.
After
sinking, the water circulates around the
world ocean (eventually rising up in the Indian and North Pacific
oceans).
The new findings will boost our understanding of the supply chain to the
world's biggest carbon
sink — the bottom of the
ocean.
Because only very cold surface water is able to
sink, it is simple to understand that the deep
ocean can never warm up, regardless of how warm the surface
ocean around the
world may become.
The
world's
oceans are carbon
sinks that sequester a third of the carbon dioxide released into the atmosphere.
The
ocean is the
world's biggest carbon
sink.
Melting glaciers have long been linked to rising sea levels but the melting ice has also added so much water to the
world's
ocean that the seabed now
sinks underneath the increasing weight.
The tiny Pacific nation of Tuvalu is urging the rest of the
world to do more to combat global warming, before the island - state
sinks beneath the
ocean's lapping waves.
They wanted to simulate what would happen to the carbon
sinks on the land and the
ocean for each model as the
world gets warmer.
Being denser than warm water it then
sank and flowed out along the bottom of the
ocean in deep
ocean currents, eventually filling the depths of the
ocean basins around the
world.
«The paper by Skinner provides important evidence the Southern
Ocean is at least a substantial source of the CO2 increase (by showing a 50 % decrease of 14C in the atmospheric CO2), which is a critical piece of the puzzle when trying to understand, model, and quantify the CO2 source /
sink behaviour of the Southern
Ocean in a warming
world today and in the future.
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To test this theory, researchers compared the abundance of algae in the surface waters of the
world's
oceans with the amount of carbon actually
sinking to deep water.
Their effect was only to expand the
world's calcium carbonate
sinks from the shallow continental shelves to some of the deeper
ocean (Westbroek 1991).»
Despite the total area of these three carbon
sinks being only about 2 percent of the
world ocean's surface area, they bury more than four times more carbon than the
oceans (table 1).
The
world's
oceans are one of the biggest carbon pools, or
sinks, in the global carbon cycle.
Soon, the mathematics of the UCSB researchers will help reveal that given differences in
ocean temperature, for example, in an especially a real
world example of the Earth rotating on its axis with warm water at the bottom of an
ocean of colder water on the top, that the cold water will
sink.