Sentences with phrase «for deeper ocean waters»

It takes a long time for deeper ocean waters to mix with the surface.

Since it takes several hundred years for the deep ocean water to cycle up to the top, where it can be warmed up and lose CO2, it makes sense to suppose that if a warming event is initiated by something else (like changes in the amount and spatial distribution of incoming solar radiation,) the concomitant rise in atmospheric CO2 (which would enhance the initial warming) might lag behind by several hundred years.

Not exact matches

Depth may not be as much of an issue for you if you tend to fish in shallow waters, but if you fish in the ocean or deep lakes and rivers, having a maximum depth of 100 meters or more can be crucial to finding your next big catch.

Researchers can measure annual changes in how the melt rate occurs, for example, or the effects of a single pulse of warm deep - ocean water.

In a recent paper published in Nature Geoscience, his team identified two deep underwater cavities beneath the glacier that they note could be pathways for relatively warm ocean water to reach the underside of the glacier, enhancing its melting.

«The ocean bed is quite complex, and there are some regions that provide access for warm, deep ocean water to those glaciers,» Scheuchl says.

«We need to do more studies to be able to determine if this new species, which we are yet to name, only lives in the shallow waters of the western Mediterranean or if it is also found in other deep water basins in the eastern Mediterranean or Atlantic Ocean, for example,» highlights Conxita Àvila.

This enabled the research team to reconstruct, for the first time, a detailed picture of the environmental conditions at the ocean's surface, as well as in deeper water layers, over the last 30,000 years.

In his letter on ocean thermal energy conversion (OTEC), Graham Cox suggests it could be used to fertilise surface waters with nutrient - rich deep water to promote plankton growth for carbon capture (1 December, p 31).

A new study led by the University of Texas Institute for Geophysics has found that wind over the ocean off the coast of East Antarctica causes warm, deep waters to upwell, circulate under Totten Ice Shelf, and melt the fringes of the East Antarctic ice sheet from below.

Washington, which produces farmed oysters, clams and mussels, is particularly vulnerable to acidification, for two reasons: seasonal, wind - driven upwelling events bring low - pH waters from the deep ocean towards the shore, and land - based nutrient runoff from farming fuels algal growth, which also lowers pH.

A month after Deepwater Horizon exploded, the Australian government reaffirmed its commitment to ocean drilling, putting 31 offshore blocks up for bidding, 17 of them in deep waters.

Most methane hydrates are buried in ocean water so deep that the journey through the water column is too far for the gas to ever reach the atmosphere, according to Ed Dlugokencky, a researcher at the National Oceanic and Atmospheric Administration.

The deep waters of the modern Arctic flow into the North Atlantic via the Nordic seas, contributing up to 40 percent of the water that becomes North Atlantic Deep Water — known as the «ocean's lungs» for delivering oxygen and salt to the rest of world's ocedeep waters of the modern Arctic flow into the North Atlantic via the Nordic seas, contributing up to 40 percent of the water that becomes North Atlantic Deep Water — known as the «ocean's lungs» for delivering oxygen and salt to the rest of world's ocwater that becomes North Atlantic Deep Water — known as the «ocean's lungs» for delivering oxygen and salt to the rest of world's oceDeep Water — known as the «ocean's lungs» for delivering oxygen and salt to the rest of world's ocWater — known as the «ocean's lungs» for delivering oxygen and salt to the rest of world's oceans.

Researchers from Northwestern University and the University of New Mexico report evidence for potentially oceans worth of water deep beneath the United States.

For years, perhaps decades, Gray has been ascribing all sorts of climate changes and hurricane cycles to fluctuations in the Thermohaline Circulation (THC), an overturning circulation in the Atlantic ocean associated with formation of deep water in the North Atlantic.

In the North West US along the Pacific Coast the oyster industry has been having a hard time for the last two or three years, partly because of ocean acidification, which is related with the upwelling of deep water.

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She's now ahead for Deep Water instead of The Light Between Oceans.

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It should be noted that only the highly experienced divers should attempt diving for whale shark viewing due to the required deep - water depths and ocean diving.

Our Fiji fishing locations are a haven for sport fishers, as the shallow reef waters soon give way to deep ocean where prized sport fish are feeding.

Humboldt Bay is the only deep water bay between the San Francisco Bay and Coos Bay, Oregon, and the Port of Humboldt Bay is the only protected deep water port for large ocean - going vessels for the large region.

Guests wade knee - deep in the balmy ocean waters to board a waiting boat for a 20 - minute crossing to a warm island reception.

Travis explained to us how each time he first goes into the water for a surfing session, as he gets out into the white wash he lies face down floating in the water between waves and gives deep thanks to Mother Ocean.

For this reason, it is best that you are comfortable swimming in deep, open ocean water for this particular toFor this reason, it is best that you are comfortable swimming in deep, open ocean water for this particular tofor this particular tour.

The first will consist of 72 - square metre ocean view rooms with a panoramic view suite on the top floor, complete with a plunge pool, while families can opt for a room or suite in one of three family - designated buildings featuring water slides, pool access and the brand signature Planet Trekkers Programme, which allows families to explore the world together and cultivate a deeper understanding of the world around them.

The abundant waters of the Sea of Cortez and the Pacific Ocean offer a plethora of sport - fish for deep - sea fishing aficionados.

Located on Playa Flamingo, designated a Blue Flag beach for ecological purity and tourism safety: 120 beautifully decorated guest rooms & suites, 2 outdoors swimming pools (with waterfalls), Serenity Spa, covered childrens pool with water features and adjacent play area, swim - p pool and snack bar, tennis court (lit for night play), breakfast and All Inclusive plan available, new restaurant and weekly theme buffets, new rooftop sunset lounge with spectacular ocean view, casino and piano bar, fitness center, beauty salon with select spa services available, sundry shop, two souvenir shops, tour desk featuring optional (volcano, rain forest, white water rafting, deep - sea fishing, and other tours), on site scuba and snorkeling Shop, table games area (Billiards & Air Hockey.

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In a sense, you have to wait for those deeper waters to finish warming before they stop removing energy from the upper ocean.

The oceans are not a single reservoir for CO2, but a combination of near surface waters and deeper layers.

However, the ocean is very strongly stratified, and the interaction with the bulk of the deep cold water is very slow — it is generally the upper ocean that determines the time scale for the transient warming we might expect.

It is difficult to establish the exact mechanism for this stronger heat flux to deeper water, given the diverse internal variability in the oceans.

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.

The surface heat capacity C (j = 0) was set to the equivalent of a global layer of water 50 m deep (which would be a layer ~ 70 m thick over the oceans) plus 70 % of the atmosphere, the latent heat of vaporization corresponding to a 20 % increase in water vapor per 3 K warming (linearized for current conditions), and a little land surface; expressed as W * yr per m ^ 2 * K (a convenient unit), I got about 7.093.

«Since the ocean component of the climate system has by far the biggest heat capacity», I've been wondering if the cool waters of the deep ocean could be used to mitigate the effects of global warming for a few centuries until we have really depleated our carbon reserves and the system can begin to recover on its own.

Deep ocean fish and other animals probably exist in a fairly high CO2 environment normally, but much higher concentrations from deep - water injections would likely be awful for tDeep ocean fish and other animals probably exist in a fairly high CO2 environment normally, but much higher concentrations from deep - water injections would likely be awful for tdeep - water injections would likely be awful for them.

They haven't reached the point of development when we are sure that they are doing everything right for the right reasons, and so my instinct is to be very cautious in interpreting ocean model results that rely on shifts in the location of deep water production etc..

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.

Even assuming that the dataset is comprehensive: Considering that the upper - ocean cooling is seen mainly at 30N and 30S, another explanation for this cooling is increased ocean — to — atmosphere heat transfer in these regions (possibly aided by hurricane - mixing of the upper ocean layer, and advection of deeper cold water as a result).

For a rough estimate, downwelling water to the deep ocean in convection zones is about 40 Sv (10 ^ 6 m3 / s), assuming that comes in with say 2 deg C, and leaves (through upwelling, isopycnal and diapycnal diffusion), that is a heat flux of 320 TW, thus at least an order of magnitude larger than the geothermal fluxes.

They then looked at the challenges that warmer oceans delivered for crustaceans, molluscs, sponges, deep sea invertebrates, the warm and cold water corals that provide habitat for one - fourth of the ocean's variety, the pelagic or surface - swimming fish, and the demersal or deep - sea denizens that live longer, reproduce more slowly and are thus less likely to evolve and adapt to changing conditions.

That may be true on a total mass basis, however, the comparison of the water mass versus the mass of only the top crust, that part that is visible for example, down a few kilometers, say to the depth of the deepest part of the ocean — water would be a significantly higher proportion of the mass than you have stipulated.

Instead, they discuss new ways of playing around with the aerosol judge factor needed to explain why 20th - century warming is about half of the warming expected for increased in GHGs; and then expand their list of fudge factors to include smaller volcanos, stratospheric water vapor (published with no estimate of uncertainty for the predicted change in Ts), transfer of heat to the deeper ocean (where changes in heat content are hard to accurately measure), etc..

While such a «missing heat» explanation for a lack of recent warming [i.e., Trenberth's argument that just can not find it yet] is theoretically possible, I find it rather unsatisfying basing an unwavering belief in eventual catastrophic global warming on a deep - ocean mechanism so weak we can't even measure it [i.e., the coldest deep ocean waters are actually warmer than they should be by thousandths of a degree]...

The land in turn creates warmer rivers which then enter the ocean and follow the bottom out to deep water so for diving buoys that don't come near shore the heat is not observed passing through the open ocean surface.

The coralline sponges also indicate that your formula doesn't hold for the period after 1940, as increased plant uptake + increased deep ocean release of CO2 (the only other fast source of huge quantities of CO2) both should increase the d13C level of the atmosphere and the upper ocean waters.

But mapping with ice - penetrating radar has revealed a low - lying region cut by glacially carved channels that drop as far as 8,500 feet below sea level — perfect for guiding warm ocean water deep into the heart of the ice sheet.