Comparisons of a sequence of the fifth - generation Pennsylvania State University — National Center for Atmospheric Research Mesoscale Model (MM5) predictions and GOES level - 2B retrievals of
ice cloud tops for the convectively active second mission period showed that the MM5 cirrus areal extent was somewhat greater than the GOES depictions.
Not exact matches
This drink that's reminiscent of bubble tea is made with a coffee jelly base, then
topped with a caramel Frappuccino blended with milk, coffee, and
ice, and finished with a whipped cream
cloud.
And, whimsy did surface with the dessert course when we ordered «The
Cloud» — a flaming cotton candy dessert comprised of Angel food cake topped with white chocolate cremeux, strawberry ice cream, strawberry compote, and whipped cream all ensconced within a cloud of cotton c
Cloud» — a flaming cotton candy dessert comprised of Angel food cake
topped with white chocolate cremeux, strawberry
ice cream, strawberry compote, and whipped cream all ensconced within a
cloud of cotton c
cloud of cotton candy.
I make a chocolate cake — rich, bouncy and well rounded, with a chewy brownie outside,
cloud - light chocolate
icing and a dreamy chocolate glaze to
top everything off.
These arcs, on the other hand, form when light hits the
top of
ice crystals — like those contained in some kinds of
clouds — and is then refracted out through the side of the crystals.
The key finding:
cloud particles at the
top of the great storm are composed of a mix of three substances: water
ice, ammonia
ice, and an uncertain third constituent that is possibly ammonium hydrosulfide.
I hope: * A Snow /
Ice course * A Jungle / Mangrove course * A Neon course in the
top of Skyscrapers (probably not, but I want it) * A course where take place in the
clouds
What this argument fails to consider is that the greater SST also produces a more vigorous updraft, so that the rising moist air has less time in which the collision / coalescence process can work before the air reaches the upper
cloud layers where spontaneous
ice nucleation takes place (at somewhere around -40 C, reached near the
top of the troposphere).
It is based on observations of
cloud cover, sea -
ice concentration, and
top - of - atmosphere broadband albedo.
Measure the temperatures of sea
ice, ocean surface, and
cloud tops using IR images and sensors deployed on the USCG C - 130
Views through another filter capture images deeper down, at the
tops of ammonia
ice clouds, where solar heating is weak but closer to where weather originates.
With
cloud tops warmer than -38 degrees Celsius,
ice formation depends on aerosols that preferentially freeze at warm temperatures, referred to as
ice nuclei.
Based on this study, we conclude that GOES level - 2B
cloud -
top retrievals are a reliable tool for prediction evaluations but the algorithm's retrievals of
ice water path are not.
And the H2O wavelengths seem to be in between, more like upper atmosphere and perhaps indicative of
cloud tops or
ice crystals.
Because of the different intramolecular forces between water molecules as vapor in air, water, and
ice, the wavelengths of emission and absorption are shifted; some of the radiation from the water /
ice droplets at the
top of a
cloud can escape to space because the atmosphere above it is transparent at its wavelengths, whereas the same radiation from droplets at the bottom of a
cloud will be absorbed and re-emitted in random directions from the droplets above, including back down to the originating droplets.
This is true for the surface of the ocean, as well as
ice crystals in the
tops of thunder
clouds.