I would say that there is a partitioning
of atmospheric layers, aligned by the fluid dynamic actions of the whole atmospheric mass, mediated by gravity, pressure, and convective heat transport.
Without the cutesy back radiation into a warmer surface invention, it might be easier to explain the potential radiative impact of CO2 and with a better model
of the atmospheric layers, understand why it is not living up to its potential.
What is more, because Jupiter's microwave emissions vary in wavelength based on the pressure (as well as temperature)
of the atmospheric layers where they originate, observations at multiple wavelengths allow researchers to create a cross-section through the atmosphere.
But it's also very probable than high SST will induce an higher instability
of the atmospheric layer.
The atmospheric layer will absorb the amount Bs * [1 — exp -LRB--- TAU)-RSB-, where TAU is the optical depth
of the atmospheric layer.
Note that both the top and bottom sections
of the atmospheric layer will absorb a tiny fraction Bs * [1 — exp -LRB--- dTAU)-RSB-, and they will similarly radiate the essentially equal amounts of energy 2 * Ba * [1 — exp -LRB--- dTAU)-RSB-.
Ray: «The IR flux from the warmer surface excites much of the CO2 — much more than would be excited at thermal equilibrium at the temperature
of the atmospheric layer where the photon is absorbed.»
If this heat were instantly trans - ferred to the lower 10 km of the global atmosphere it would result in a volume mean warming
of this atmospheric layer by approximately 36 C (65 F).
Urban pollution concentrations depend on the magnitude of local emissions sources and the prevailing meteorological ventilation of the area — i.e., the height
of the atmospheric layer through which the pollutants are being mixed and the average wind speed through that layer.
If this heat were instantly transferred to the lower 10 km of the global atmosphere it would result in a volume mean warming
of this atmospheric layer by approximately 36 C (65 F).»
Not exact matches
This «would create a persistent
layer of black carbon particles in the northern stratosphere that could cause potentially significant changes in the global
atmospheric circulation and distributions
of ozone and temperature,» they concluded.
We know that contained in these ice
layers there are bubbles
of atmospheric gases, particulate matter and other distince indicators
of the climate at the time the
layers were formed.
This month, NASA aircraft will begin studying a natural
atmospheric laboratory off the coast
of Namibia, where a
layer of smoke wafts over a low cloud deck.
Those techniques have led to everything from the development
of catalysts that remove poisonous carbon monoxide from car exhaust to the understanding
of how ice crystals in stratospheric clouds supercharge
atmospheric chlorine's ability to destroy the planet's protective ozone
layer.
To survive 50 millennia and return its payload to Earth intact, KEO must have many
layers of shielding — aluminum to protect against oxidation, tungsten and titanium to protect against meteors and cosmic rays, ceramic to protect against the heat
of atmospheric reentry.
Rather, they are the result
of the peculiar processes that unfold in a place cold enough that
atmospheric carbon dioxide can freeze into snowy
layers of dry ice.
Black carbon aerosols — particles
of carbon that rise into the atmosphere when biomass, agricultural waste, and fossil fuels are burned in an incomplete way — are important for understanding climate change, as they absorb sunlight, leading to higher
atmospheric temperatures, and can also coat Arctic snow with a darker
layer, reducing its reflectivity and leading to increased melting.
That heated surface air then rose into the
atmospheric boundary
layer — the lowest level
of the troposphere — doubling its height to more than 4 kilometers, and creating a thick blanket
of heat.
Understanding the transition between the
atmospheric layer and the more rigid
layers that lie beneath will be revealed during the remainder
of Juno's primary mission over the next couple
of years.
The meeting was the first large - scale attempt to bridge the gap between scientists and policymakers on a wide range
of atmospheric problems, including not just the greenhouse effect but also acid rain and the depletion
of the protective
layer of ozone in the stratosphere.
To investigate the
layers and composition
of clouds and tiny airborne particles like dust, smoke and other
atmospheric aerosols,, scientists at NASA's Goddard Space Flight Center in Greenbelt, Maryland have developed an instrument called the Cloud - Aerosol Transport System, or CATS.
The lead surrounding the stars — which was part
of the original cloud
of gas and dust from which these stars formed, not generated by reactions in the evolving stars themselves — may be dispersed within an
atmospheric layer as much as 100 kilometers thick (depicted patchily in pink) that altogether weighs up to 100 billion metric tons.
This
atmospheric layer includes molecules that absorb ultraviolet and visible light, acting as a kind
of «sunscreen» for the planet it surrounds.
Extensive
layers of atmospheric haze can be seen in images
of Pluto taken by New Horizons.
As a result
of this, more
of the CO2 bound in organic matter remains in the surface
layer, which reduces the ocean's potential to take up
atmospheric CO2.»
Reactions in and on sea - salt aerosol particles may have a strong influence on oxidation processes in the marine boundary
layer through the production
of halogen radicals, and reactions on mineral aerosols may significantly affect the cycles
of nitrogen, sulfur, and
atmospheric oxidants.
In the new study, the researchers used a state -
of - the - art 3D computer model
of atmospheric chemistry to investigate what would have happened to the ozone
layer if the Montreal Protocol had not been implemented.
Instead, a new study suggests, the phenomena occur when four types
of slow - moving, high - altitude
atmospheric waves merge over a small region and, in turn, temporarily drive a 10 - fold - or - stronger brightening
of an ever - present glow in the upper atmosphere (green
layer in the image above).
This investigation also provides detailed information on the
atmospheric structure
of the thermosphere, the
layer of the Earth's atmosphere directly above the mesosphere and below the exosphere, by comparing and helping to refine models based on de-orbit data.
Because the vast plateau at such altitudes absorbs a huge amount
of solar radiation, the
atmospheric layer above it in summer is much warmer than air at similar elevations over lower land or the oceans.
University
of Washington
atmospheric scientist Qiang Fu and his colleagues used a second channel, sensitive almost exclusively to the stratosphere, to quantify this
layers exact contribution to channel 2 readings.
Pollutants that gather from India and China in the lowlands around the mountains can be boosted as high as 18 kilometers, reaching the stratosphere — the
atmospheric layer directly above the troposphere that contains most
of Earth's ozone.
The new study, published in the June 1 issue
of the Astrophysical Journal, suggests that clouds or haze
layers could be preventing a substantial amount
of atmospheric water from being detected by space telescopes.
So it was a surprise when NASA's MAVEN spacecraft found
layers of atmospheric metal ions (Geophysical Research Letters, doi.org/b5nf).
Prior to
atmospheric entry at 14:42 GMT, contact via the Giant Metrewave Radio Telescope (GMRT), the world's largest interferometric array, located near Pune, India, was established just after it began transmitting a beacon signal 75 minutes before reaching the upper
layers of the Martian atmosphere.
The council is to step up its research into
atmospheric pollution, and says that this could result in the re-routeing
of aircraft to avoid damage to the ozone
layer.
But these cores formed under the weight
of their planets» outer
layers, under pressures
of around 500 gigapascals — 5 million times
atmospheric pressure on Earth — and typical temperatures
of about 6,000 kelvin.
The corona is heated to millions
of degrees, yet the lower
atmospheric layers like the photosphere — the visible surface
of the Sun — are only heated to a few thousand degrees.
But recently teams have been able to observe that at pressures
of 2 - to - 3.5 million times normal
atmospheric pressure it transforms into an unexpected structure consisting
of layered sheets, rather than a close - packed metal as had been predicted many years ago.
Regional trends are notoriously problematic for models, and seems more likely to me that the underprediction
of European warming has to do with either the modeled ocean temperature pattern, the modelled
atmospheric response to this pattern, or some problem related to the local hydrological cycle and boundary
layer moisture dynamics.
Propose numerical experiments aiming to refine numerical techniques and the formulation
of atmospheric physics processes, boundary
layer processes and land surface processes in models.
While the large
atmospheric pressure at the surface and the high altitude
of the Venusian cloud
layer appears to exclude the possibility
of cloud - to - ground lightning (Gurnett et al. 2001; Aplin 2006), several authors have suggested that lightning discharges above, between or within clouds may occur (Borucki 1982; Russell & Scarf 1990; Gurnett et al. 2001).
Pluto — Norgay Montes (left foreground); Hillary Montes (skyline); Sputnik Planitia (right) Near - sunset view includes several
layers of atmospheric haze.
This corresponds in scope (not un-coincidentally) to the
atmospheric component
of General Circulation Models (GCMs) coupled to (at least) a mixed -
layer ocean.
Application
of remotely piloted aircraft systems in observing the
atmospheric boundary
layer over Antarctic sea ice in winter, Polar Research, 34 (25651)
«Data collected by satellites and balloon - borne instruments since 1979 indicate little if any warming
of the low - to mid - troposphere — the
atmospheric layer extending up to about 5 miles from the Earth's surface.
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.
Name one detrimental effect
of UV light when it is not stopped by ozone in upper
atmospheric layers.
Wang, W., and M. Schlesinger, 1999: The dependence on convection parameterization
of the tropical intraseasonal oscillation simulated by the UIUC 11 -
layer atmospheric GCM.
«People had considered whether you could get a subsurface
layer of water somewhere on Pluto» states New Horizons co-investigator Richard Binzel, professor
of earth,
atmospheric and planetary sciences at MIT.