Red light penetrates to
deeper atmospheric layers where cloud structures are prominent.
Not exact matches
Here we present a chronology for the
deep part of the core (67.8 - 31.2 ka BP), which is based on stratigraphic matching to annual -
layer - counted Greenland ice cores using globally well - mixed
atmospheric methane.
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The standard assumption has been that, while heat is transferred rapidly into a relatively thin, well - mixed surface
layer of the ocean (averaging about 70 m in depth), the transfer into the
deeper waters is so slow that the
atmospheric temperature reaches effective equilibrium with the mixed
layer in a decade or so.
It's what drives the
atmospheric circulation and the ocean currents that mix the upper warm
layers of the ocean with the
deeper colder
layers, and vice versa.
To enjoy getting into those claims you would have to consider the impacts of differing rates of advection in the different ocean and
atmospheric layers from the stratopause to the
deep oceans.
Deep in the ice sheets of Greenland are annual
layers that record what the
atmospheric gases and the air temperature were like over each of the last 250,000 years.
«The basic problem of this research is to determine how to merge data from nine instruments to produce a useful time series of
deep -
layer atmospheric temperatures.