However, it was shown that significant amount of DIC and DOC may be exported
from ocean margins to the open ocean (Cai et al. 2003).
Not exact matches
For eons, the mineral iron, which once saturated
oceans, likely bonded with phosphorus, and sank it down to dark
ocean depths, far away
from those shallows — also called continental
margins — where cyanobacteria would have needed it to thrive and make oxygen.
Although roughly 15 percent of the world's
oceans overlie continental
margins, these bands suffer
from the logistical drawbacks of land and deep sea: inconveniently deep water and uncomfortably complex terrain.
We recognize that atmospheric and Pacific
Ocean conditions
from beyond our geographical scope influence the coastal
margin.
All is Lost, the second feature
from Oscar nominated writer / director J.C. Chandor (of
Margin Call previously), stars Robert Redford and only Redford as the sole captain of a sailboat that ends up lost at sea after being damaged in the Indian
Ocean.
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Selfdrive - The drive
from Cairns to Port Douglas is well worth taking the time to soak up the serenity of the
ocean.
By a very very big
margin, the net flow of latent and sensible heat is
from ocean to atmosphere on a global basis.
We show that the influx of water into the volume created by this subsidence produces a sea - level fall at locations distant
from these
margins — indeed over the major
ocean basins — that is comparable in amplitude to the syphoning mechanism isolated by Mitrovica and Peltier (1991).»
According to the submission, in geological and geomorphological terms, the continental
margin of Canada in the Atlantic
Ocean extends continuously
from offshore Nova Scotia in the south, along the Grand Banks to the northern tip of Labrador, although each of the three regions has unique characteristics.
The European Union's Copernicus Climate Change Service said on Thursday that last year was the warmest on record by a wide
margin, stoked by greenhouse gases and an El Nino weather event that released heat
from the Pacific
Ocean.
The European Union's Copernicus Climate Change Service said on Thursday that past year was the warmest on record by a wide
margin, stoked by greenhouse gases and an El Nino weather event that released heat
from the Pacific
Ocean.
Whereas at the three sites
from the central Arctic
Ocean an extended to perennial sea ice cover was probably predominant, sea ice conditions were much more variable along the northern Barents Sea continental
margin as reflected in the data of Core PS2138 - 2 (Fig. 2d).
a Last Glacial Maximum (LGM) and MIS 1 conditions for selected cores
from the central Arctic
Ocean (CAO), the Barents Sea continental
margin (BSCM) and Fram Strait (FS) 36 and Early Holocene (EH) and Middle - Late Holocene (MLH) data
from Fram Strait Core MSM5 / 5 -71232).
These cores were recovered
from areas characterized by different sea ice conditions today, ranging
from perennial sea ice in the central Arctic
Ocean to seasonal sea ice conditions along the Barents Sea continental
margin (Fig. 1; see Methods for more details).
In developing a scenario for the death of the AAG, the birth of the Southern
Ocean, and the transition
from Paleogene greenhouse Earth to Neogene icehouse Earth, the neritic record of the northern
margin is more in accord with the «Dinocyst biogeographic hypothesis» than with the «Tasman gateway hypothesis.»
In short: methane release
from the
ocean floor may have caused a weakness in the sediments that contributed to development of these huge dents in the Norwegian continental
margin.
While the winter / spring 2008 sea - ice extent has rebounded
from the 2007 negative mega-anomaly, the age - class distribution at present is negatively skewed compared to satellite climatology and even the values for 2007, as is ice concentration within the ice -
ocean margin that defines extent.
At present, most mass loss
from ice sheets occurs at their marine
margins, through iceberg production and melting by the
ocean.
Josh Willis, a lead NASA scientist for the Jason missions, which measure sea level rise
from space and
Ocean's Melting Greenland (OMG), is a passionate communicator about human - caused global warming.Come listen to a talk on what his team has found out about the role of the
oceans in ice loss around the
margins of the Greenland Ice Sheet.
Elucidating such patterns
from this and other
ocean margin regions, in particular their relationships with oceanographic and climatic variations and shifts in primary production, will be an essential part of the critical task of predicting future trends in both ecosystem biochemistry and trophic dynamics.
It could be evenly distributed in the global
ocean causing an almost imperceptable rise in its temperature well beyond the
margin of detection error or it could be rejected by more efficient means of transport
from surface to space or by a change which prevents it
from ever reaching the surface in the first place.
I insist that consideration of relative contributions of carbon fluxes without considering the error
margins is an utter nonsense, especially if the difference between two big numbers (uptake and intake
from oceans) is a prime concern.