Why don't photons get absorbed by all
the other water vapor molecules to cause warming?
I have read more than one paper on the topic, and my assessment is that cloud cover and
other water vapor effects are widely recognized as among the biggest unknowns going forward.
Cloud cover and
other water vapor effects for the future are completely unpredictable.
Not exact matches
Measurements of the
water vapor and of
other molecules, such as carbon monoxide, suggest there is enough gas to feed the black hole until it grows to about six times its size.
Intelligent design and automatic control - uses high temperature
water vapor to continuously disinfect and sterilize the bottles and
other items in a short period of time.
-- A 100 - story smokestack belches a roiling, white cloud of
water vapor, carbon dioxide and
other leftover gases after burning daily as much as 12,000 tons of coal at the Mountaineer Power Plant — a total of 3.5 million tons a year.
Water vapor is the strongest greenhouse gas; unlike
other greenhouse gases, it is controlled principally by temperature.
The atmosphere consists primarily of 78 percent nitrogen, 21 percent oxygen, a highly variable smattering of
water vapor, and trace amounts of argon, carbon dioxide, and
other gases.
The researchers do know that the presence of certain aerosols plays a large role in the formation of ice that leads to precipitation, but they also need to tease out the importance of that with
other factors, like the amount of available
water vapor and vertical storm winds.
Walter sees the benefits of using methane as an energy source as twofold: «Not only does it prevent a potent greenhouse gas from entering the atmosphere by converting it to weaker greenhouse gases —
water vapor and carbon dioxide — but using it on - site would also reduce the demand for
other fossil - fuel sources.»
Careful analysis of what frequencies are absorbed, and by how much, can directly reveal the presence of
water vapor and
other compounds, and can divulge climate parameters, such as temperature and pressure, that determine if liquid
water is sustainable.
So this effect could either be the result of natural variability in Earth's climate, or yet another effect of carbon dioxide and
other greenhouse gases like
water vapor trapping more heat and thus warming sea - surface temperatures.
Others using the secondary eclipse technique have detected evidence for
water vapor and methane in the atmosphere of HD 189733 b.
«Given that atmospheric rivers over the Atlantic and Pacific oceans appear as coherent filaments of
water vapor lasting for up to a week, and that Lagrangian coherent structures have turned out to explain the formation of
other geophysical flows, we wondered whether Lagrangian coherent structures might somehow play a role in the formation of atmospheric rivers,» said study coauthor Vicente Perez - Munuzuri, a physicist at the University of Santiago de Compostela in Spain.
Earth's relatively feeble gravity couldn't grab on to the
water vapor, or any
other gas for that matter.
This effect makes the atmosphere act somewhat like a blanket that becomes thicker when amounts of
water vapor, carbon dioxide and
other greenhouse gases, such as methane and nitrous oxide, increase.
The hydrogen bonds can be disrupted by
water vapor in the air, with each keratin binding to
water in the air instead of each
other.
In the harsh sunlight of the upper atmosphere, methane can react with
other gases to form
water vapor, which then breaks down into
other chemicals that destroy ozone.
«This is the first time
water vapor has been unequivocally detected on Ceres or any
other object in the asteroid belt and provides proof that Ceres has an icy surface and an atmosphere,» said Michael Küppers of ESA in Spain, lead author of a paper in the journal Nature.
To show that those atoms are bonded together into
water vapor or a similar substance, observations at
other wavelengths would be needed.
Here are some
other top successes: destroying stockpiles of chemical weapons globally as well as local stores of DDT in Tanzania; new cooking stoves to eliminate indoor air pollution in Ghana; separating copper mine tailings from the local
water supply in Chile; alternative fuels to reduce air pollution in New Delhi as well as treating arsenic in well
water in West Bengal; removing lead - contaminated soil in the Dominican Republic and Russia; reducing mercury
vapors from artisanal gold mining in Indonesia; and new sewage systems to clean up contaminated Suzhou Creek in Shanghai.
But
other experts say there's a big difference between
water vapor, as discovered in HD 189733b's atmosphere, and liquid
water, which is what astronomers are really hoping to nail down.
Reporting in the 12 July Nature, the scientists note that they can't tell the density of
water vapor in HD 189733b's atmosphere — in
other words, whether it is present in only trace amounts or at much higher levels.
Even models that correctly capture cloud behavior may fail to fully account for
other climate feedbacks from factors like changing snow and sea ice cover, atmospheric
water vapor content, and temperature.
The group also evaluated the permeability, with
water vapor, of the nanomesh conductor — along with those of
other substrates like ultrathin plastic foil and a thin rubber sheet — and found that its porous mesh structure exhibited superior gas permeability compared to that of the
other materials.
They suggest complex stomata evolved to help early plants control moisture in their spore capsules and that
other plants later exploited these pores to breathe in carbon dioxide and exhale
water vapor.
Each cell contains algorithms that reflect the interactions among the ocean, clouds,
water vapor, aerosols, trees, soil and
other tiny widgets.
The warm conditions of the earth get a big boost from
water vapor as well as several
other culprits, some of which never existed in the atmosphere prior to human influence.
The telescope's Wide Field Camera 3 had detected
water vapor in the atmospheres of 10 of these planets, and no
water on the
other nine.
By analyzing global
water vapor and temperature satellite data for the lower atmosphere, Texas A&M University atmospheric scientist Andrew Dessler and his colleagues found that warming driven by carbon dioxide and
other gases allowed the air to hold more moisture, increasing the amount of
water vapor in the atmosphere.
«We're looking for
water vapor or ice, as well as hydrocarbons and
other volatiles,» he says.
The
other obvious observation is that
water vapor has more relative effect in the tropics, where it is moister.
Scientists have detected
water vapor on
other planets in the past, but these detections could only take place under very specific circumstances, according to graduate student Alexandra Lockwood, the first author of the study.
For example, the spacecraft spotted geysers of
water vapor and
other material blasting from the south pole of the icy moon Enceladus.
It also would be far easier to get a
water sample from Enceladus, which has plumes of
water vapor, ice and particles shooting more than 300 miles off its surface, than from
other moons, such as Jupiter's Europa, where a massive ocean is believed to be buried beneath a thick icy crust.
«When a planet transits, or passes in orbit, in front of its host star, we can use information from this event to detect
water vapor and
other atmospheric compounds.
While there is at present no compelling reason to doubt the models» handling of
water vapor feedback, it is not out of the question that some unanticipated behavior of the hydrological cycle could make the warming somewhat milder — or on the
other hand, much, much worse.
With JWST, a few hours of integration time will be enough to detect Earth - like levels of
water vapor, molecular oxygen, carbon dioxide and
other generic biosignatures on planets orbiting a white dwarf; beyond that, observing the same planet for up to 1.7 days will be enough to detect the two CFCs in concentrations of 750 parts per trillion, or 10 times greater than on Earth.
Soon
other substances, including
water vapor, will begin pouring out, revealing their presence in the spectrum of light from the comet to instruments on the ground and those, like Spitzer, in space.
Knowing the right combination
other warming agents, such as
water vapor, nitrous oxide, and carbon dioxide, will also help us assess habitability of the hundreds of billions of
other Earth - like planets estimated to reside in our galaxy.
When the CLIMAP data proved to be wrong, and was replaced by more reliable estimates showing a substantial tropical surface temperature drop, Lindzen had to abandon his then - current model and move on to
other forms of mischief (first the «cumulus drying» negative
water vapor feedback mechanism, since abandoned, and now the «Iris» effect cloud feedback mechanism).
Knowing this, the researchers could look at the wavelengths of infrared light and, like a fingerprint, link it to what share was from a CO2 buildup in the air, and what share was due to
other things, such as
water vapor.
However, the surface warming caused by human - produced increases in carbon dioxide, methane, and
other greenhouse gases leads to a large increase in
water vapor, since a warmer atmosphere holds more moisture.
Its atmosphere is 95 percent CO2, compared with Earth's 78 percent nitrogen and 21 percent oxygen, with trace amounts of
other gases and
water vapor.
The abundance of
water vapor, oxygen, methane, and
other organic compounds in the atmosphere could be evidence of an active biosphere on the surface of a planet.
This empirical fast - feedback climate sensitivity allows
water vapor, clouds, aerosols, sea ice, and all
other fast feedbacks that exist in the real world to respond naturally to global climate change.
The factors that determine this asymmetry are various, involving ice albedo feedbacks, cloud feedbacks and
other atmospheric processes, e.g.,
water vapor content increases approximately exponentially with temperature (Clausius - Clapeyron equation) so that the
water vapor feedback gets stronger the warmer it is.
Greenhouse effect from
water vapor is filtered out, showing the contributions of
other greenhouse gases (Evans 2006).
the way greenhouse gases trap heat and feedbacks involving
water vapor, sea ice and
other factors amplifying or modulate that heat trapping
In particular, aircraft jet engines produce carbon dioxide (CO2),
water vapor (H2O), nitrogen oxides (NOx), carbon monoxide (CO), oxides of sulfur (SOx), unburned or partially combusted hydrocarbons (also known as volatile organic compounds, or VOCs), particulates, and
other trace compounds.