Sentences with phrase «clouds at»

- Stephen Coonts We woke up at 3 am to catch our (first) flight from Birmingham, Alabama to Port - au - Prince, Haiti on Saturday, February 21, 2015, and we watched the sun rise up above the clouds at 40,000 feet.
I turned to him and said «Blue skies with pink clouds at sunset.»
It seems an appropriate time for those lawyers, ethics committees, bar associations and legal regulators who have an interest in how the cloud will serve the public interest as well as the needs of lawyers, clients and cloud developers to get involved and start looking at clouds from both sides now, both up and down, as it seems that, at this early point in its development, we really don't know the ethics of clouds at all...
None taken, I've been insulted by experts everywhere from Tamino to Deltoid; as for feedback from clouds I think I said clouds were a moderator [sic] and this can be contrary as my night example shows; that is, clouds at night warm whereas clouds at day cool; as for Professor Pinker, my friend Steve Short summed up her findings and cloud feedback thus:
The study, by experts at the DLR German Aerospace Center, estimated that the net warming effect for the Earth of contrails and related cirrus clouds at any one time was 31 milliwatts per square meter, more than the warming effect of accumulated CO2 from aviation of 28 milliwatts.
Working back from the clouds at a height of say 4kilometers and applying the adiabatic lapse rate of 9.8 K / km we arrive at the planet surface temperatures of around 15C.
This causes me to speculate that an increase in boundary layer humidity could increase the likelihood of clouds at the top of the boundary layer.
By now modelers were attempting to incorporate the different properties of different types of clouds at different heights.
Since 76 % of this radiation is reflected by clouds, and most of the rest of the radiation is absorbed by these clouds at the top of Venus» atmosphere, only a tiny 2.5 % of the solar radiation ever reaches Venus» surface.
I asked a friend if he knew how many cloudless days they got - it happened to be overcast with high clouds at the time and he (only partly in jest) said, «You mean sunny like this?
The release of 2,300,000 J per kilogram of H2O vapour keeps the temperature of the clouds at a high value.
As a hurricane spins counterclockwise, the clouds at its center move faster and faster in a circle, which narrows until it falls apart, to be replaced by a new circle of eye - wall clouds.
The clouds at 5Km are far better radiators than gaseous CO2 or H2O.
Modtran gives a rough interpretation of the effect of CO2 and other greenhouse gases (water vapour) and clouds at different heights.
And that's the forcing of all clouds at a certain percentage of coverage.
Svensmark et al. (2009) found large global reductions in the aerosol Ångström exponent from AERONET, liquid water path from SSM / I, and cloud cover from MODIS and ISCCP after large Forbush decreases, but these results were not corroborated by other studies who found no statistically significant links between GCR and clouds at the global scale (Calogovic et al., 2010; Kristjánsson et al., 2008; Laken and Calogovic, 2011).
So Svensmark tweaked his theory: Though clouds at middle and high levels are unaffected by cosmic rays, he said, low - level cloud formation was still highly correlated.
Continental total cloud cover has similarities to the PDO low - level, mid-level, and high clouds at 0.159.
Discrimination between radiation effects of clouds at different altitudes is not trivial.
Clouds during the day cause lower temperatures (assuming no wind) and clouds at night cause warmer than normal temperatures because heat isn't radiating into space.
The Ka - band ARM zenith radar (KAZR) remotely probes the extent and composition of clouds at millimeter wavelengths.
The Moderate Resolution Imaging Spectroradiometer (MODIS) aboard NASA's Terra satellite captured this image of clouds at 11:35 a.m. local time (10:35 a.m. UTC).
The Ka - band zenith radar remotely probes the extent and composition of clouds at millimeter wavelengths.
That gives me pause to say something major is missing, or a major systemic error etc. (e.g., Major ocean oscillations are missing as well as Cosmic rays / clouds at least).
By June 2007 she was a postdoctoral associate at PNNL, studying arctic clouds at first but never giving up her fascination with convective clouds: the kind she gazed at in wonder as a girl in China, leading the family cow to pasture.
I still remember the pink clouds at sun rise the next morning looked more beautiful.
George Tselioudis, a climate scientist at NASA's Goddard Institute for Space Studies and Columbia University in New York City, was interested in which air currents were shifting clouds at high altitude — between about three and a half and six miles high — toward the poles.
Climate researchers still have a lot of work to do when it comes to understanding clouds, says Trenberth, who believes the state of the science is still like that old Joni Mitchell song Both Sides Now, in which she sings, «I really don't know clouds at all.»
It's at least more credible than Hansen's «runaway greenhouse» nonsense, which can be dismissed on rather elementary grounds (without clouds at least), but I think Tamino's post before about «changing the dice» a bit to land more higher numbers, and possibly a few 19's and 20's, is a much more appropriate analogy than the argument that the system behavior will deviate substantially from smoothly varying statistics
The latter results in far longer lines of air mass mixing with more clouds at those lengthened air mass boundaries.
it is evident in the atmosphere but is upset by clouds at low level and UV absorption at higher altitudes.
For instance, researchers still don't completely understand the role of aerosols in the atmosphere, the variable effects of clouds at different heights, and the influence of feedback mechanisms such as the changing reflectivity of the Earth's surface and the release of gases from permafrost or deep seabeds.
«Evaluation of water permittivity models from ground - based observations of cold clouds at frequencies between 23 and 170 GHz.»
IR is absorbed totally at some wavelengths but it penetrates even trough the clouds at other wavelengths.
Now, if our earth has a thermostat and does not allow all the water to boil away, i.e. a shield, like clouds, then we have an oscillatory system: the water cycle creates more clouds at high solar output and diminished clouds at low solar output.
No, clouds at night, if cooler than the surface, can only slow the rate of cooling of the surface.
The convergence of these wind systems enhances the development of convective rain clouds at the tropics.
That is, it follows the paths of the long - wave photons downward and upward in the air, up to 60 km in the stratosphere as if there were no clouds at all.
2) The warmed water vapour rises up in the air... and as it rises it cools... and frequently forms clouds at altitude.
For orographic cumulus clouds, the G - 1 measurements will characterize in - cloud dynamics, microphysics, and aerosols, as well as the environmental variability around the clouds focusing on conditions upstream and downstream of clouds at multiple altitudes in the vicinity of the AMF1 site.
The condensation level at the top of the boundary layer will prevent this increased humidity reaching further up into the atmosphere, because it will be rained out from the clouds at the condensation level.
A good friend of mine (who's a scientist in an area far removed from climate) was arguing some time ago that the climate models are useless because they don't include clouds at all or in such a crude way that their effect is totally meaningless.
More work is needed to know clouds at all.
This provides a stable reference temperature structure for the fast feedback processes to operate and maintain the amounts of atmospheric water vapor and clouds at their quasi-equilibrium concentrations.
Why not, for example, more clouds at night and in winter?
In his 1939 Birds of the Bagaduce, the sky occupies the bulk of the canvas, a backdrop to clouds at once fleshy and nearly abstract.
Benfey writes: «They seem, in fact, to register quite distinct aesthetic programs, as though what Constable is classifying isn't clouds at all, but rather whole schools of painting, along with their dominant moods.
In «Untitled # 10,» what seem like pink - orange clouds at sunset quickly shift to suggest other, more corporeal references.
The backbone of the sale, to be held just before the Frieze art fair opens, are works by German artists led by a Gerhard Richter abstract, at # 7 million to # 10 million, followed by a realist Richter painting of clouds at # 5 million to # 7 million.
Edge of Lahar (mudflow), Looking NE (Mount St. Helens behind clouds at left), 5.5 miles SE of Mount St. Helens, Washington, 1983 9 7/8 x 23 7/8 inches Gelatin silver print; printed 1984
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