Sentences with phrase «cold ocean water where»

The bloody swirls of cold ocean water where a cute little terrier wearing a fou - fou life vest for his yachtsman owner used to be represents the first pre-credits victim of Island Zero.

Not exact matches

I can't imagine breathing well in the east, I need the place where I am, I need these mountains, I need the ocean now, I need the cold lake water, I need rocky shores.

Forming in the system's colder outer regions, where volatile compounds such as water and carbon dioxide freeze out, makes it possible that the planets incorporated those ices and carried them along to a warmer place where they could melt, evaporate, and become oceans and atmospheres.

And around Antarctica, where even the surface ocean water is already quite cold and dense, some of that water in the ocean depths, which is also carbon rich, eventually warmed enough so that it became less dense than the water above it.

The fog is a gift of the Pacific Ocean's California Current where winds create upwellings that bring cold, deep, nutrient - rich waters to the surface.

Today, cold water sinks near the Arctic and flows deep below the surface of the Atlantic toward the southern oceans, where it rises up.

This moves water away from the coast, causing upwellings that bring cold, nutrient - rich water from the ocean floor to the surface, where it feeds innumerable microorganisms and algae.

Low - lying coastal regions like Chile's are subject to advection fog, where warm ocean air crosses a band of cold water before reaching land.

The ocean waters that are cleared of sea ice by strong winds blowing from the coast carve out a suitable enclave where marine organisms can thrive, unlike the rest of the icy cold Antarctic region.

For millions of years, fish species in the Pacific and Atlantic oceans have stuck resolutely to where they belong, kept from venturing between oceans by the cold water of the Arctic.

The researchers think these conditions may exist on the seafloor of Enceladus, where hot water from the interior meets the relatively cold water at the ocean bottom.

The Channel is an oceanographic transition zone where the cold waters north of Point Conception mix with the warm waters of Southern California, resulting in a complex system of water currents and a diversity of northern and southern ocean species.

This morning we were heading 1 1/2 hours south to the open expanse at the tip of Dall Island where the nutrient - rich, cold waters of the ocean meet the warmer waters of the archipelago's many inlets.

Puri Wirata Amed - Dive Resort and Spa is a budget PADI five - star resort located in Bunutan, a quiet fishing village along the coast of Amed, a premier diving destination in East Bali.The resort is a two - hour transfer from the Ngurah Rai International Airport in South Bali, and an hour from the breach resort area of Candidasa.Puri Wirata Amed offers a collection of ocean - view guestrooms and villas equipped with air conditioning, hot and cold water, balcony or terrace, four - poster beds with mosquito nets, personal safe, mini-bar, flat screen television and DVD players.Two ocean front swimming pools and direct beach access make for a memorable outdoors for guests staying at Puri Wirata, and an onsite restaurant that serves a variety of Indonesian, Balinese and Western dishes also makes for an ideal spot from where to enjoy the views with a cocktail at hand.

We pride ourselves with the fact that we have the only swimming pool in town where our guests, those not brave enough to face the cold waters of the ocean, can cool down.

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You'll find, just as examples: ``... another — possibly substantial — source of energy for mixing that's generated in the ocean where cold, heavy water collides with warm, light water.

We use some of the power to spread the cold water over the surface so that it does not sink below the layer where phytoplankton convert dissolved CO2 into organic matter that increases the mass of their bodies to feed other ocean creatures.

When upwelling brings cold water to the ocean's surface, cooling the atmosphere, where is that heat lost from the atmosphere «hiding»?

The ocean conveyor gets its «start» in the Norwegian Sea, where warm water from the Gulf Stream heats the atmosphere in the cold northern latitudes.

I have to raise an objection to the phrase «the only region of the world that has defied global warming» — that might be neglecting a certain area in the Pacific where England 2014 has identified a very obvious point where the «Pacific conveyor» was bringing in the last decade up a lot of cold water from the deep ocean and has possibly played a major role in the specific trends for that period.

Lawrence, yes, the accumulation of heat in the oceans is the primary metric of global warming, but it's distributed unevenly, and we don't know how much of it will be diluted in cold waters and how much, when and where it will be released to the atmosphere.

Consenquently, the associated SST pattern is slightly cooler in the deep convection upwelling regions of the Equitorial Pacific and the Indian Ocean, strongly cooler in the nearest deep convection source region of the South Atlantic near Africa and the Equator, warm over the bulk of the North Atlantic, strongly warmer where the gulf stream loses the largest portion of its heat near 50N 25W, and strongly cooler near 45N 45W, which turns out to be a back - eddy of the Gulf Stream with increased transport of cold water from the north whenever the Gulf Stream is running quickly.

The vertically integrated inventory of human emitted CO2 in the oceans is (not surprisingly) much greater in areas of cold deep convection, especially in the northern Atlantic (the falling leg of the thermohaline circulation), and much less in the tropics where the ocean is strongly stratified; absorption in the tropics really is more in the near - surface waters.

Since the whole world does not appear to freeze during a ice age, the must be massive ice making going at the pole driven by heat lifting oceans of water to the sky from the equator where it is pushed by the expanding air and vapor to the poles areas where it returns to the surface and follows cold land like a culvert between warmer expanding ocean air back down to the equatoral region.

First, CO2 outgases where cold water from the ocean depths surfaces at the equator to absorb solar radiation.

Icelandic scientists say they have discovered a new overturning site, where cold, dense, deep water is formed and transported through a separate route towards the Denmark Strait and further south into the Atlantic Ocean.

When the convective processes of the atmosphere remove enough water vapor from the oceans to drop sea levels and build polar ice caps, as has happened many times before, the top 35 meters of the oceans where climate models assume the only thermal mixing occurs, must heat up cold ocean water that comes from depths below the original 35 meter depth, removing vast more amounts of heat from the earth's surface and atmosphere.

As mentioned above, highest surface densities in the world ocean are reached where water is very cold, while lower densities are found in the saltier but warmer tropical and subtropical areas.

In Washington and Oregon, oysters farms are in coastal Pacific waters where upwelling currents are bringing up cold, deep water with higher amounts of CO2 and a more acidic pH. Watch and listen to two oyster farmers from Taylor Shellfish Farms in Washington state talk how about ocean acidification is impacting their young oysters.

Currents that move through the upper ocean then dive down to depth may move some of the surface heat to the deeper waters, especially where the currents have dived not just from cooling water (hot water would tend to go up, cold water would tend to go down) but because it is driven in «conveyor» systems which may run counter to expectations of where water should go when considering only local conditions, and especially, if the water is dropping because of an increase in salinity.

The second is a temperature driven process where cold water sinks at the poles cooling the deep ocean.

In the Atlantic Ocean, the current known as the Atlantic Meridional Overturning Circulation (AMOC) ferries warm surface waters northward — where the heat is released into the atmosphere — and carries cold water south in the deeper ocean layers, according to the National Oceanic and Atmospheric AdministraOcean, the current known as the Atlantic Meridional Overturning Circulation (AMOC) ferries warm surface waters northward — where the heat is released into the atmosphere — and carries cold water south in the deeper ocean layers, according to the National Oceanic and Atmospheric Administraocean layers, according to the National Oceanic and Atmospheric Administration.

The Arctic ocean sequesters carbon, and the oceans currents carry that cold water to other places, where they heat back up and release the CO2 again.

Warming bottom waters in deeper parts of the ocean, where surface sediment is much colder than freezing and the hydrate stability zone is relatively thick, would not thaw hydrates near the sediment surface, but downward heat diffusion into the sediment column would thin the stability zone from below, causing basal hydrates to decompose, releasing gaseous methane.

The temperature signal in deep ocean δ18O refers to the sea surface where cold dense water formed and sank to the ocean bottom, the principal location of deep water formation being the Southern Oocean δ18O refers to the sea surface where cold dense water formed and sank to the ocean bottom, the principal location of deep water formation being the Southern Oocean bottom, the principal location of deep water formation being the Southern OceanOcean.

On the contrary, whatever warm, hypersaline water sinks below the surface because of its great density is mixed relatively quickly by winds into the upper layer of the ocean, where it transfers its heat to colder parcels by conduction.

This is expected to affect coral reefs, cold water corals, and ecosystems (e.g., the Southern Ocean), where aragonite (used by many organisms to make their shells or skeletons) will decline or become undersaturated.

The Arctic Ocean is highly stratified with a roughly 50 metre thick layer of cold relatively fresh water above a thermocline where the water temperature and salinity both increase with depth.