Most atmospheric air is comprised of roughly 21 % oxygen.
Not exact matches
Keeping
atmospheric concentrations of greenhouse gases below 550 ppm, let alone going back to 350 ppm or below, will not only require a massive shift in human society — from industry to diet — but also,
most likely, new technologies, such as capturing CO2 directly from the
air.
«We found that the Antarctic microbes have evolved mechanisms to live on
air instead, and they can get
most of the energy and carbon they need by scavenging trace
atmospheric gases, including hydrogen and carbon monoxide,» she says.
For the
most recent glacial periods ice cores provide climate proxies from their ice, and
atmospheric samples from included bubbles of
air.
Although observatories are built at sites that typically have clear skies and relatively calm
air layers, the only ways to get truly sharp images is go above the atmosphere (think Hubble Space Telescope) or to build highly complicated adaptive optics systems that correct for the
atmospheric turbulence (and even
most imperfections of the telescope itself).
He painted en plein
air, and the majority of his
most important paintings depict rainy weather while documenting street life and
atmospheric effects.
When the reseachers at the Center for International Climate and Environmental Research — Oslo (CICERO) applied their computer «model and statistics to analyse temperature readings from the
air and ocean for the period ending in 2000, they found that climate sensitivity to a doubling of
atmospheric CO2 concentration will
most likely be 3.7 °C, which is somewhat higher than the IPCC prognosis.»
Instead, the researchers found that disturbances in
atmospheric circulation, the large - scale movement of
air, have the
most effect on drought because they can affect factors that will cause it to rain more or less.
Several of the
most disconcerting
atmospheric problems include smog and
air pollution, which are responsible for a higher incidence of respiratory diseases and death; acid rain, which contaminates numerous other ecosystems such as watersheds and forests; and finally, one particularly serious issue, climate de-stabilization caused by the accelerated rate of global warming.
I hope they are not trying their suggestion of igniting the
atmospheric methane that now covers
most of northern hemisphere — that would be a serious fuel
air bomb.
Keeling's record of data from Mauna Loa is considered one of the best and
most consistent climate records anywhere, though scientists also use other sources for
atmospheric data, including samples of
air trapped in polar ice, to analyze CO2 levels in past millennia.
Leaf area index, which is also enhanced by increasing
atmospheric carbon dioxide, was the second
most important factor, contributing an additional 21.8 percent, followed by climate change (precipitation and
air temperature together) and the fraction of photosynthetically active radiation, which accounted for the remaining 18.3 and 14.6 percent increase in NPP, respectively.
Working with a total of 2,196 globally - distributed databases containing observations of NPP, as well as the five environmental variables thought to
most impact NPP trends (precipitation,
air temperature, leaf area index, fraction of photosynthetically active radiation, and
atmospheric CO2 concentration), Li et al. analyzed the spatiotemporal patterns of global NPP over the past half century (1961 — 2010).
By 1970 the US
Air Force Cambridge Laboratories had the
most highly developed science on
atmospheric optical effects.
Its location next to a subtropical high - pressure belt of descending
air produces stable
atmospheric conditions over
most of its surface area, and the climate generally is dry.
28 29 7.4.5.2 Physical Mechanisms Linking Cosmic Rays to Cloudiness 30 31 The
most widely studied mechanism proposed to explain the possible link between GCR and cloudiness is 32 the «ion - aerosol clear
air» mechanism, in which
atmospheric ions produced by GCR facilitate aerosol 33 nucleation and growth ultimately impacting CCN concentrations and cloud properties (Carslaw et al., 2002; 34 Usoskin and Kovaltsov, 2008).
The
most widely studied mechanism proposed to explain the possible link between GCR and cloudiness is the «ion - aerosol clear
air» mechanism, in which
atmospheric ions produced by GCR facilitate aerosol nucleation and growth ultimately impacting CCN concentrations and cloud properties (Carslaw et al., 2002; http://www.sciencemag.org/content/298/5599/1732.abstract
The Korea Meteorological Administration announced that the average
atmospheric concentration of particulate matter measuring 10 micrometers (PM10) on the day was 228 micrograms per cubic meter, the
most dangerous level in its five - level
air pollution scale.
Long wave cloud forcing is the contribution to
atmospheric thermal energy flux
most relevant to
air temperature.
[26] Historically, the
most intense storms and precipitation events in California have been tied to wintertime
atmospheric rivers that fed on high levels of water vapor in the
air.
One of the
most striking changes is the decline of sea ice concurrent with changes in
atmospheric circulation and increased surface
air temperature.
All that is needed is to add heat carried upwards past the denser atmosphere (and
most CO2) by convection and the latent heat from water changing state (the majority of heat transport to the tropopause), the albedo effects of clouds, the inability of long wave «downwelling» (the blue balls) to warm water that makes up 2 / 3rds of the Earth's surface, and that due to huge differences in enthalpy dry
air takes far less energy to warm than humid
air so temperature is not a measure of
atmospheric heat content.
However, because
atmospheric concentrations of water vapor tend to be at
most only a few percent of the amount of
air (and usually much lower), they are both often expressed in units of grams of water vapor per kilogram of (moist or dry)
air.
It is ignored in
most assessments of
atmospheric gases; they record only dry
air at sea level.
Hence,
atmospheric GEM concentrations inferred from Greenland firn
air and global anthropogenic Hg emissions have exhibited consistently similar trends during the
most recent decades (Fig. 2), suggesting that the
atmospheric reservoir of mercury at mid - and high - northern latitudes has been driven mainly by anthropogenic emissions during the last decades.
Most anthropogenic sources have been located at temperate northern latitudes, and global
atmospheric circulation transfers to Greenland
air masses from North America, Europe, and, to a lesser extent, Asia (46).
One of the
most well - known effects of global warming is an intensification of the water cycle, with higher
air temperatures leading to increased evaporation from the seas and soils, and more
atmospheric water vapor contributing to more frequent heavy precipitation events.