Lin, B., B. Wielicki, P. Minnis, and W. Rossow, 1998: Estimation of
water cloud properties from satellite microwave, infrared and visible measurements in oceanic environments: 1.
MacFarlane, S.F., K.F. Evans, and A.S. Ackerman, 2002: A Bayesian algorithm for the retrieval of liquid
water cloud properties from microwave radiometer and millimeter radar data.
Alexandrov, M.D., B. Cairns, A.P. Wasilewski, A.S. Ackerman, M.J. McGill, J.E. Yorks, J.E. Hlavka, S.E. Platnick, G.T. Arnold, B. van Diedenhoven, J. Chowdhary, M. Ottaviani, and K.D. Knobelspiesse, 2015: Liquid
water cloud properties during the Polarimeter Definition Experiment (PODEX).
Not exact matches
«Astronomers find evidence of
water clouds in first spectrum of coldest brown dwarf: Difficult spectroscopic observations reveal
properties of the coldest known object outside of our solar system.»
These fingerprints allowed the team to extract the signatures from various elements and molecules — including
water — and to distinguish between cloudy and
cloud - free exoplanets, a
property that could explain the missing
water mystery.
Every land - owner, the judge ruled, had
property rights over
clouds and the
water they contained passing over their land; and, while men should not play God, if the government decided that
cloud seeding was in the public's interest, it should proceed.
«Probability density function,» a statistical representation of the likelihood of something occurring at any point in time, was used to examine
cloud properties, including vertical motion, liquid and ice
water content, and the conditions of
cloud particle growth, including how ice crystals grow at the expense of liquid droplets.
In one sentence: Researchers at Pacific Northwest National Laboratory found that when miniscule particles of airborne dust, thought to be a perfect landing site for
water vapor, are modified by pollution, they change
cloud properties via ice crystal number concentration and ice
water content.
Taking a closer look at the
properties of
water droplets and ice crystals within
clouds, the team found that pollution resulted in smaller droplets and ice crystals, regardless of location.
In 102 characters: Researchers measure supercooled
water properties, fleshing out their understanding of rain and
clouds.
In one sentence: For first time, researchers measure
properties of
water at deeply supercooled temperatures, fleshing out their understanding of rain and
clouds.
While the amounts and distribution of
water vapor and
clouds are feedbacks, the intrinsic
properties are «externally - imposed» by the physics, as is the case with snow and ice, etc..
That was holding the distribution of solar heating steady, which would require removing
water vapor,
cloud, and ozone LW optical thickness but still leaving behind their SW (solar) optical
properties.
There can / will be local and regional, latitudinal, diurnal and seasonal, and internal variability - related deviations to the pattern (in temperature and in optical
properties (LW and SW) from components (
water vapor,
clouds, snow, etc.) that vary with weather and climate), but the global average effect is at least somewhat constrained by the global average vertical distribution of solar heating, which requires the equilibrium net convective + LW fluxes, in the global average, to be sizable and upward at all levels from the surface to TOA, thus tending to limit the extent and magnitude of inversions.)
Climate projections, such as those used by the Intergovernmental Panel on Climate Change, rely on models that simulate physical
properties that affect climate, including
clouds and
water vapor content.
The
water vapor condensation in troposphere begets
clouds, which to a considerable degree determine the reflective
properties of the planet, i.e., its albedo A.
Developed specifically for the ARM Facility, the Raman lidar is an active, ground - based laser remote sensing instrument that measures
water - vapor mixing radio and several
cloud and aerosol
properties.
One can't arbitrarily choose feedbacks for
water vapor, ice / albedo,
clouds, etc., without looking to see how these phenomena are actually behaving — e.g., what are the radiative
properties of
water vapor, how is relative humidity changing, what is happening to low
cloud cover, high
cloud cover, and the high / low
cloud ratios, etc.?.
The physics that must be included to investigate the moist greenhouse is principally: (i) accurate radiation incorporating the spectral variation of gaseous absorption in both the solar radiation and thermal emission spectral regions, (ii) atmospheric dynamics and convection with no specifications favouring artificial atmospheric boundaries, such as between a troposphere and stratosphere, (iii) realistic
water vapour physics, including its effect on atmospheric mass and surface pressure, and (iv)
cloud properties that respond realistically to climate change.
Based on the understanding of both the physical processes that control key climate feedbacks (see Section 8.6.3), and also the origin of inter-model differences in the simulation of feedbacks (see Section 8.6.2), the following climate characteristics appear to be particularly important: (i) for the
water vapour and lapse rate feedbacks, the response of upper - tropospheric RH and lapse rate to interannual or decadal changes in climate; (ii) for
cloud feedbacks, the response of boundary - layer
clouds and anvil
clouds to a change in surface or atmospheric conditions and the change in
cloud radiative
properties associated with a change in extratropical synoptic weather systems; (iii) for snow albedo feedbacks, the relationship between surface air temperature and snow melt over northern land areas during spring and (iv) for sea ice feedbacks, the simulation of sea ice thickness.
Scientists measured
properties of
water at deeply supercooled temperatures — which may help theorists flesh out their understanding of
water and help atmospheric scientists better understand rain and
clouds.
(And I still can't see how a newly open and increasingly warm summer Arctic Ocean won't produce more
water vapor, vapor whose GHG
properties will further accelerate Arctic warming — or is that completely offset by increased
cloud formation??)
They include «remote sensors for measuring
clouds, trace gases and temperatures above and below the aircraft, as well as instruments to measure
water vapor,
cloud properties, meteorological conditions, radiation fields and numerous trace gases around the aircraft.»
Water clouds have both cooling effects (due to reflection) and warming effects (due to infrared properties of wa
Water clouds have both cooling effects (due to reflection) and warming effects (due to infrared
properties of
waterwater).
The atmosphere ECV breakout group was asked to consider 10 ECVs related to observations of the atmosphere: Earth radiation budget (including solar irradiance); aerosol
properties; ozone; carbon dioxide, methane, and other greenhouse gases;
cloud properties; precipitation;
water vapor; surface wind speed and direction; upper - air wind; and upper - air temperature.
Topics that I work on or plan to work in the future include studies of: + missing aerosol species and sources, such as the primary oceanic aerosols and their importance on the remote marine atmosphere, the in -
cloud and aerosol
water aqueous formation of organic aerosols that can lead to brown carbon formation, the primary terrestrial biological particles, and the organic nitrogen + missing aerosol parameterizations, such as the effect of aerosol mixing on
cloud condensation nuclei and aerosol absorption, the semi-volatility of primary organic aerosols, the importance of in - canopy processes on natural terrestrial aerosol and aerosol precursor sources, and the mineral dust iron solubility and bioavailability + the change of aerosol burden and its spatiotemporal distribution, especially with regard to its role and importance on gas - phase chemistry via photolysis rates changes and heterogeneous reactions in the atmosphere, as well as their effect on key gas - phase species like ozone + the physical and optical
properties of aerosols, which affect aerosol transport, lifetime, and light scattering and absorption, with the latter being very sensitive to the vertical distribution of absorbing aerosols + aerosol -
cloud interactions, which include
cloud activation, the aerosol indirect effect and the impact of
clouds on aerosol removal + changes on climate and feedbacks related with all these topics In order to understand the climate system as a whole, improve the aerosol representation in the GISS ModelE2 and contribute to future IPCC climate change assessments and CMIP activities, I am also interested in understanding the importance of natural and anthropogenic aerosol changes in the atmosphere on the terrestrial biosphere, the ocean and climate.