They also looked at whether craters made by the comets hitting the surface could excavate enough nitrogen — but that would require
a very deep layer of nitrogen ice at the surface, which is not proven.
Not exact matches
But I do think they bear a
deep accountability to the congregation understood in depth and at all of the different
layers of its life» — understood, she says, in ways that the congregations themselves don't yet understand, since they haven't been engaged in
very deep congregational studies either.
Also, the
layers fall after they come out of the oven, so while I thought I had nice thick
layers, I ended up with
very thin
layers about 1»
deep.
The
very existence of this
layer is understood from seismic imaging, as it lies far too
deep underground to be sampled directly.
If the training is sufficiently long (again, the training is
very computer - intensive) and the images are processed in
deep enough networks — those with many
layers of processing elements — the neural network generalizes and can accurately recognize a new photograph as containing a feline.
Scientists thought most of Vesta outside the south polar region might be flat like the Moon, yet some of the craters outside that region formed on
very steep slopes and have nearly vertical sides, with landslides often occurring in the regolith, the
deep layer of crushed rock on the surface.
In a separate paper, we show how gradients can be combined with neuroevolution to improve the ability to evolve recurrent and
very deep neural networks, enabling the evolution of DNNs with over one hundred
layers, a level far beyond what was previously shown possible through neuroevolution.
In the East Pacific, the warm surface waters are a
very shallow
layer on top of the
deep cold waters.
Abyssal zone
Layers of the pelagic zone The abyssal zone is the abyssopelagic
layer or pelagic zone that contains the
very deep benthic communities near the bottom of oceans.
That's not really surprising, considering that this is a
very delicate balancing act that involves providing your body with enough good quality calories and reducing calorie intake exactly as much as needed to encourage burning of the
deepest layers of fat.
Since 5E lessons provide differentiated instruction in their
very nature, your students will complete the unit with a
deep understanding of: • Earth's
Layers • Continental Drift • Thermal Convection • Earth's Plates • Plate Boundaries • Hotspots • Earthquakes • Seafloor spreading ** Your students will also confront and overcome the following misconceptions.
Hydroplaning, if the water was
deep enough, and / or the tread on your tires was worn enough, the car may have been floating on a
layer of water, giving the brakes
very little traction.
A
very large twenty gallon aquarium with toys and a
deep layer of bedding help to provide the Robos with activities and a great place to tunnel.
The game's strategy
layer is
very deep, rewarding thoughtful and methodical gameplay, while punishing the hasty.
The intimacy of Scully's creative process, in which paint is
layered while he manipulates it using brush strokes and sensitivity, offers a
very sensual and tactile materiality while colors, often subtly harmonized, evoke
deep emotional associations.
Even the
very thickness of the white paint, whether a thin film or
layered deep, demands his attention.
Now, for some purposes if you were looking at the
very long term response to a
very slowly varying radiative forcing, you might get away with treating the ocean with a
deeper equivalent mixed
layer.
A lot of reseach energy is being devoted to the study of Methane Clathrates — a huge source of greenhouse gases which could be released from the ocean if the thermocline (the buoyant stable
layer of warm water which overlies the near - freezing
deep ocean) dropped in depth considerably (due to GHG warming), or especially if the
deep ocean waters were warmed by
very,
very extreme changes from the current climate, such that
deep water temperatures no longer hovered within 4C of freezing, but warmed to something like 18C.
As far as I understand it, hurricanes actually warm the
deeper layers (though they do temporarily cool the surface which adjusts through air - sea exchange
very quickly after the storm has passed).
Because minimum temperatures in the stable boundary
layer are not
very robust measures of the heat content in the
deep atmosphere and climate models do not predict minimum temperatures well, minimum temperatures should not be used as a surrogate for measures of
deep atmosphere global warming.»
As discussed in the following section, the absence of significant warming in the Circumpolar Ocean of the Southern hemisphere is attributable mainly to the large thermal inertia of the ocean, which results from
very effective mixing between the surface
layer and the
deeper layers of ocean in this region.
One line of argument seems to be that a
very slow exchange between surface and
deep ocean means that the response of the surface
layer to additional forcing will be rather rapid since
deep diffusion is slow.
If you had box 2 as part of the well - mixed
layer, taking heat rapidly from it, but giving it up slowly to
deeper waters — again,
very little difference.
Fracing sometimes breaks through into rock
layers very deep in the earth containing salt water (such as the Ellenberger in the Barnett field).
Very little interaction with the thermocline from
deeper layers and even that would be undetectable.
This is because the
deepest layers are
very old and mix
very slowly with the surface.
The last graph, temperatures of
layers with different thicknesses, is particularly misleading - the large rise in surface temperature (
very little energy involved) shown over the
deep layer temperature changes (a huge amount of energy) is a case of apples / oranges.
It is all
very self - consistent if one assumes half the heat entering the ocean is sequestered by diffusing to
deeper layers.
However the tidal currents coming into contact with the relief of the ocean bottom (even if this is
very deep) creates waves which are propagated at the interface between two
layers of different densities.
Callendar suggested that the top
layer of the ocean, that interacts with the atmosphere, would easily become saturated with carbon dioxide and that would affect its ability to absorb more, because, he thought, the rate of mixing of shallow and
deep oceanic waters was likely to be
very slow.