Not exact matches
Measuring - Temperature and Thermometers Classifying Components
of Mixtures Predicting - Surveying Opinion SAPA Part C, Directions for the Multiplication Game SAPA Part C and E, Multiplication Game SAPA Part D 1st Draft, c. 1972 The Whirling Dervish The Bouncing Ball The
Effect of Liquid on Living Tissue Rate
of Change Observing Growth from Seeds An Intro to Scales Forces on Static and Moving Objects Observations and Inferences Using Punch Cards to Record a Classification Using Maps to Describe Location A Tree Diary SAPA Part D 2nd Draft Observations and Inferences The Bouncing Ball Rate
of Change A Tree Diary An Intro to Scales and Scaling Observing Growth from Seeds (The Bean - It Came Up) Forces on Static and Moving Objects Using Punch Cards to Record a Classification Relative Position and Motion Inferring - The
Water Cycle Predicting 4 - The Suffocating Candle The Big Cleanup Campaign 2 - D Representation
of Spatial Figures Using Maps to Describe Location SAPA Part D Tryout Draft, 1972 Observations and Inferences The Bouncing Ball Measuring Drop by Drop Rate
of Change Predicting 4 - The Suffocating Candle Forces on Static and Movign Objects Observing Growth from Seeds Using Space / Time Relationships -2-D Representation
of Spatial Figures Using Punch Cards to Record a Classification An Introduction to Scales and Scaling The
Effect of Liquid on Living Tissue Inferring - The
Water Cycle Relative Position and Motion Using Maps to Describe Location The Big Cleanup Campaign A Tree Diary SAPA II Module (s), c. 1973 1, Tentative Format Sample, Perception
of Color 9, Sets and Their Members 6, Direction and Movement, Draft 34, About How Far?
Abundant
liquid water newly discovered underneath the world's great ice sheets could intensify the destabilizing
effects of global warming on the sheets.
Researchers say this antifreeze
effect makes it possible for
liquid water to be widespread just below the surface
of Mars, but point out that even if it is there, it may be too salty to support life as we know it.
«The sources
of this
liquid water will require more observational studies; however, the research shows that the
effects of relatively small amounts
of water on Mars in forming features on the surface may have been widely underestimated.
Wet Earth Erin Wayman's article «Faint young sun» (SN: 5/4/13, p. 30), about how the early Earth stayed warm enough for
liquid water, made me wonder about the
effect of the temperature
of the planet itself.
Results from these and other studies are yielding important insights into the cooperativity
effects in hydrogen bonding, aqueous solvation, and hydrogen - bond network rearrangement dynamics, which promise to enhance our understanding
of solid and
liquid water behavior.
The outer boundary is defined by the «maximum greenhouse limit,» where the greenhouse
effect fails as CO2 begins to condense out
of the atmosphere and the surface becomes too cold for
liquid water.
Greenwald, T.J., G.L. Stephens, S.A. Christopher, and T.H.V. Haar, 1995: Observations
of the global characteristics and regional radiative
effects of marine cloud
liquid water.
A side
effect of this organized pattern is that the moon's gravitational tug pulls at Earth — but since the planet's surface is covered in
liquid water, it simply sloshes over to appease that tug, creating tides.
Four and a half billion years after its birth, the shrouded planet is much too hot to support the presence
of liquid water on its surface because
of its dense carbon dioxide atmosphere and sulfuric acid clouds, which retain too much radiative heat from the Sun through a runaway greenhouse
effect.
Add
liquid drops
of chlorophyllin to
water and drink throughout the day to proactively fight against the deleterious
effects of toxins.
Daily performances based on passages in the books — including a performer drawing in
water on the walls and tabletop surfaces, in Book
of Liquid Pages (2016)-- are held with the intent
of activating the space; but, curiously, they seem to have almost the opposite
effect, signaling the inability to create the time, place and
effects of Kim's original project.
In this estimate, only 4.2 mm per month
of liquid water equivalent are due to the mass added by enhanced precipitation; the vast majority
of the
effect (72 mm per month
of decreased ablation) is due to the
effect of precipitation on reflectivity.
Liquid water and ice have identical compositions but the health
effects of being hit with 10 gallons
of water are not the same as being hit with a chunk
of ice.
Similarly, we have not been able to tell how much
of the aerosol is capable
of interacting with
liquid or ice clouds (which depends on the different aerosols» affinity for
water), and that impacts our assessment
of the aerosol indirect
effect.
A hydrophilic surface would also be preferable for condensation (reduced surface tension
effect for a given mass
of liquid water in a droplet), though I've never heard
of that being important in the atmosphere.
Corresponding time for surface + tropospheric equilibration: given 3 K warming (including feedbacks) per ~ 3.7 W / m2 forcing (this includes the
effects of feedbacks): 10 years per heat capacity
of ~ 130 m layer
of ocean (~ heat capacity
of 92 or 93 m
of liquid water spread over the whole globe)
The latter,
of course, stems from a complete lack
of understanding
of the
effect of CO2 on the world's climate, which is derived from models that do not even consider the
effect of the world's main climate control mechanism, namely the energy transfer between
water in solid,
liquid and gaseous forms.
Less well appreciated is that clouds (made
of ice particles and / or
liquid water droplets) also absorb infrared radiation and contribute to the greenhouse
effect, too.
Liquid water in the ocean generates its own greenhouse
effect because, you see, visible light from the sun easily penetrates to a depth
of about 30 meters to warm the
water.
The main difference between H2O and CO2 (apart from the numerical differences
of their specific physical properites such as degree
of freedom, thermal capacity, physical mass, etc) in terms
of their
effects on the atmosphere is that
water is capable
of condensing into
liquid to form clouds and readily and rapidly moves between surface and atmosphere, daily, seasonally, annually and on even greater time scales, but CO2 does not liquify in the biosphere and transfers over mostly long time periods between surface (primarily oceans, seas, etc) and the atmosphere.
There is NOT a «logarithmic input
of effect» by «
water» as the energy inputted to Kinetic Induction is also powering Turbulence, such energy NOT being measurable as «temperature»
of the mass being «moved» and this is in precedence to any measure
of «temperature» especially in a Gas, but also in a
liquid.
Experiment 1 demonstrates that incident LWIR on the surface
of liquid water does not have the same
effect on cooling rate as it does on other materials.
As said on cards n ° 1, n ° 6 and n ° 15, for an atmosphere in a gravitation field, the tropospheric lapse rate is dT / dz = — g / (Cp + Ch) where g = 9,8 m / s ², Cp = 1005 J / kg, and Ch summarizes the
effect of the heating
of the air (1) by absorption
of the solar infrared by
water vapour or
liquid and (2) by the condensation
of the
water vapour.
Presumably the
effect is much greater in
liquid water since the first 30 feet
of it is equal the entire weight
of the atmosphere above it and the first foot
of it equal to the weight
of all the
water vapor above it.
Depending a bit how you weight the overlapping spectral absorptions
of the different greenhouse gases the contribution
of CO2 to the total greenhouse
effect is about 20 % (with
water vapour giving 50 % and 25 % for clouds, which we are sure that Allègre realises are made
of condensate (
liquid water and ice) and not vapour...).