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 2005, while exploring the Saturn system, the Cassini spacecraft made a startling discovery: Cryovolcanoes on Enceladus were spewing
jets of water vapor and ice into space, possibly from a liquid water source beneath the surface.
Not exact matches
In 2005, NASA's Cassini spacecraft spied
jets of water ice and
vapor erupting into space from fissures on Enceladus, evidence
of a salty ocean beneath the saturnian moon's placid icy surface.
Jet engine exhaust contains carbon dioxide, oxides
of sulfur and nitrogen, unburned fuel, soot and metal particles, as well as
water vapor.
The
jets in another nebula, K3 - 35, are so powerful, reports Luis Miranda
of Spain's Astrophysical Institute
of Andalucia, that they are squashing clouds
of water vapor at their tips, 450 billion miles from the star, and causing the
water to mase - emit laserlike beams
of microwaves.
For example, Cassini discovered that the Saturn satellite Enceladus is a mini-world
of active
jets — geyser - like phenomena that blast out
water vapor and ice particles from the huge, salty ocean that lies beneath the moon's icy crust.
«The
jets must be supersonic, with Mach numbers
of two or greater, but because
of cooling
of the
water vapor in the eruption throat, the actual velocity may not be as high as we thought previously,» said Larry Esposito, a conference organizer and a professor
of astrophysical and planetary sciences in the Laboratory for Atmospheric and Space Physics (LASP) at the University
of Colorado, Boulder.
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.
Simple physics dictates that with less sea ice there is magnified warming
of the Arctic due to powerful albedo feedback; this in turn reduces the equator to pole temperature gradient which slows the
jet stream winds causing them to become more meridional; this combined with 4 % more
water vapor in the atmosphere (compared to 3 decades ago) is leading to much more extremes in weather.
However, to support the assertion that global warming is responsible for a great deal
of damage from such events, it is sufficient to show that such events have the «signature»
of global warming — for example, that specific global warming - related factors such as abnormally high sea surface temperatures, elevated
water vapor levels, and altered
jet stream patterns contributed to making Hurricane Sandy what it was — even if those factors can not be precisely quantified.
A cloud for blocking sunlight is formed in the sky from the
water vapor jetted to reduce the temperature
of the earth surface.
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.
As we have noted, one
of the Achilles heels for the US aviation industry could be the complex mixture
of greenhouse gases and precursors — carbon dioxide,
water vapor, and oxides
of nitrogen — injected directly into the atmosphere by every
jet and turboprop in the sky.
The level
of scientific understanding
of radiative forcing is ranked by the AR4 (Table 2.11) as high only for the long - lived greenhouse gases, but is ranked as low for solar irradiance, aerosol effects, stratospheric
water vapor from CH4, and
jet contrails.