Stillwell R. A., R. R. Neely, J. P. Thayer, M. D. Shupe and D. D. Turner (February 2018): Improved cloud - phase determination of low - level liquid and mixed -
phase clouds by enhanced polarimetric lidar.
Not exact matches
The star system consists of a young star still in an early development
phase and three gas
clouds which are rapidly condensing
by gravitational forces.
Modeling experiments
by Tan and two other scientists focused on inbetweeners — mixed -
phase clouds, such as undulating stratiform and fluffy stratocumulus
clouds, which are abundant over the vast Southern Ocean and around the Northern Hemisphere north of New York.
Results: A team led
by Pacific Northwest National Laboratory (PNNL) researchers has presented two processes, or explanations, for how extra ice crystals form in mixed -
phase clouds —
clouds containing both water and ice — which are prevalent throughout the Arctic.
Atmospheric scientists at Pacific Northwest National Laboratory are adding pieces to the climate change puzzle
by studying Arctic mixed -
phase clouds.
The main mode, which is involved in the formation of ice crystals in mixed -
phase clouds (
clouds formed
by ice particles and water droplets), is the immersion freezing mode.
A new paper
by Andrew Dessler of Texas A&M University bolsters the established view of
clouds» role as a feedback mechanism — but not driver — in climate dynamics through a decade of observation and analysis of El Nino and La Nina events (periodic warm and cool
phases of the Pacific Ocean).
However, there is stronger anticorrelation between the model's sulfate generated
by gas -
phase oxidation and
cloud cover.
However the only way to achieve strong anticorrelation between total sulfate and
clouds is
by correcting our treatment of aqueous -
phase sulfate production.
This substantial and rapid change of
phase permits large ice crystals in a
cloud surrounded
by a large number of supercooled
cloud droplets to grow quickly (often in less than 15 minutes) from tiny ice crystals to snowflakes.
The 12 - and 11 - µm ΔBT helps to distinguish between high, thick
clouds and high, thin
clouds by delineating
cloud phase (ice or liquid water) and
cloud particle size (small or large).
Evidence suggests that thermodynamics prevails at least two - thirds, and a significant role in the thermodynamics is played
by «latent heat» in evaporated water which leap frogs up into the
cloud levels and is then released up there
by phase change.
This bias may be explained
by a misrepresentation of mixed -
phase extratropical
clouds, often pinpointed as playing a key role in driving global -
cloud feedback and uncertainties in climate sensitivity estimates (e.g., Tan et.
Shown are changes in the radiative effects of
clouds and in precipitation accompanying a uniform warming (4 °C) predicted
by four models from
Phase 5 of the Coupled Model Inter-comparison Project (CMIP5) for a water planet with prescribed surface temperatures».
The effects of tropical cyclones early in the year were followed
by regular northwest
cloud - band activity between May and mid-July, when waters northwest of the continent were unusually warm as part of a negative
phase of the Indian Ocean Dipole.
Using liquid and ice microphysics models reduces the biases in
cloud optical thicknesses to ≲ 10 %, except in cases of mistaken
phase identification; most of the remaining bias is caused
by differences between actual
cloud particle sizes and the values assumed in the analysis.
«Retrieving the Polar Mixed -
Phase Cloud Liquid Water Path
by Combining CALIOP and IIR Measurements.»