Situated 150 light - years from Earth, HD 209458b is a planet that holds
traces of water vapor in its atmosphere, and also contains basic organic compounds that, on Earth, foster the development of life.
Not exact matches
Water vapor is an important
trace gas that reveals the nature
of the quasar.
The
vapor accompanying these particles was mostly
water but contained
trace amounts
of simple organic compounds, as well as carbon dioxide and ammonia — all ingredients important for the sustenance and even origin
of life.
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.
«There likely will be little
traces of the hydrocarbons in the
water that is condensed to form rain, but it will likely make up less than normal pollution does,» says research meteorologist Frank Marks, director
of hurricane research at NOAA's Atlantic Oceanographic and Meteorological Laboratory in Miami, Fla. «The amount
of water vapor evaporated that might contain hydrocarbons related to the spill will be very, very small.»
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.
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.
Its instruments can't capture microbes or detect life, but in a couple
of dozen passes through the plumes
of Enceladus, it has detected various molecules associated with life:
water vapor, carbon dioxide, methane, molecular nitrogen, propane, acetylene, formaldehyde and
traces of ammonia.
The most possible cause, according to researchers, for the observed
water vapor traces around Europa is the presence
of erupting
water plumes on the moon's surface, not unlike those that have been directly observed on Saturn's moon Enceladus by the Cassini spacecraft.
Enceladus» southern polar region is also home to occasional jets
of water vapor and icy particles (with
traces of carbon dioxide and monoxide, volatile gases, and hydrocarbons) that spew from vents within the moon's so - called «tiger stripe fractures,» which create a huge plume
of vapor and icy particles that extends into space and affects Saturn's magnetosphere.
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.
The relative contribution
of each
trace GHG to increased Eocene and Cretaceous land temperatures at 4 × CO2, assessed with multiple separate coupled - ocean atmosphere HadCM3L model simulations, revealed methane and associated increases in stratospheric
water vapor dominate, with nitrous oxide and tropospheric ozone contributing approximately equally to the remainder.
Only molecules made
of at least three atoms absorb heat radiation and thus only such
trace gases makes the greenhouse effect, and among these CO2 is the second most important after
water vapor.
The principles
of absorption and emission
of radiation by various atmospheric
trace gases like
water vapor and CO2 rely on the theory
of quantum mechanics.
Instead atmospheric physics uses the fundamental equations (the radiative transfer equations) which determine absorption and emission
of radiation by
water vapor, CO2, methane, and other
trace gases.
Indeed, strong observational evidence and results from modeling studies indicate that, at least over the last 50 years, human activities are a major contributor to climate change.Direct human impact is through changes in the concentration
of certain
trace gases such as carbon dioxide, chlorofluorocarbons, methane, nitrous oxide, ozone, and
water vapor, known collectively as greenhouse gases.
As the concentration
of gaseous
water (
water «
vapor») in the atmosphere is on the order
of 3o, 000 to 40,000 ppm, this
trace greenhouse gas really * is * the invisible 800 lb gorilla in the room even if we ignore the phase change effects.
The abstract
of this report says most
of the absorption [and thus radiation] observed in the atmosphere is due to its
trace components such as
water -
vapor, carbon dioxide and ozone.
WebHubTelescope, after 100 years
of human emission
of CO2, the atmosphere still consists about 78 % Nitrogen, 21 % oxygen, 0.9 % Argon, 1 %
water vapor, 0.039 % CO2, and other
trace gasess.
However,
water vapor, carbon dioxide, methane, and other
trace gases are opaque to many wavelengths
of thermal infrared energy.»
The world's climate is way too complex... with way too many significant global and regional variables (e.g., solar, volcanic and geologic activity, variations in the strength and path
of the jet stream and major ocean currents, the seasons created by the tilt
of the earth, and the concentration
of water vapor in the atmosphere, which by the way is many times more effective at holding heat near the surface
of the earth than is carbon dioxide, a non-toxic,
trace gas that all plant life must have to survive, and that produce the oxygen that WE need to survive) to consider for any so - called climate model to generate a reliable and reproducible predictive model.
States that other feedbacks likely to emerge are those in which key processes include surface fluxes
of trace gases, changes in the distribution
of vegetation, changes in surface soil moisture, changes in atmospheric
water vapor arising from higher temperatures and greater areas
of open ocean, impacts
of Arctic freshwater fluxes on the meridional overturning circulation
of the ocean, and changes in Arctic clouds resulting from changes in
water vapor content
About 50 %
of global warming may be attributed to
water vapor, about 25 % clouds, and
trace gases are the last 25 %, which we have increased substantially since the beginning
of the industrial age.
Alexandrov, M.D., A.A. Lacis, B.E. Carlson, and B. Cairns, 2001: MFRSR - based climatologies
of atmospheric aerosols,
trace gases, and
water vapor.
Water vapor is just a
trace gas, less than one half
of one percent
of the air in the atmosphere.
One
of the few articles that recognizes the specific heat capacities
of the major atmospheric gases — Nitrogen, Oxygen, Ozone and Argon — as well as the atmospheric
trace gases —
water vapor and Carbon Dioxide.