The matte black paper
absorbs the heat while solar radiation from the sun is reflected from the aluminium foil onto the food.
Crafted of durable polyester, the stylish panel features subtle texturing in the weave that helps
absorb heat while reducing light and noise.
Not exact matches
Once all the water is
absorbed, turn off the
heat and leave to sit, covered,
while you prepare the rest of the salad.
While most ingredients
absorb heat from the pan, sugar actually generates its own
heat as it breaks down.
Turn off the
heat and stir in the oats and allow to stand for a few minutes
while the oats
absorb the moisture from the vegetable mix.
Some reflect sunlight, cooling the climate,
while others
absorb heat from the sun, warming the climate.
While drifting in the atmosphere or after settling on the ground, soot efficiently
absorbs sunlight, warms up, and radiates
heat.
«
Absorbing electromagnetic energy
while avoiding the
heat: First demonstration of a metal - free metamaterial that can
absorb electromagnetic energy.»
Using engineered nanophotonic materials the team was able to strongly suppress how much
heat - inducing sunlight the panel
absorbs,
while it radiates
heat very efficiently in the key frequency range necessary to escape Earth's atmosphere.
Describing the albedo effect — the phenomenon that explains how lighter substances reflect sunlight
while darker items
absorb its
heat — she said permafrost thaw is also a growing concern.
Urban land use creates a
heat - island effect because asphalt, brick, and concrete
absorb and conduct solar energy,
while the cooling effect of evaporation from soil and vegetation is reduced.
[Dirk Zeuss et al, Global warming favours light - coloured insects in Europe] Lighter colors reflect sunlight
while dark colors
absorb it and
heat up.
Sandia engineers developed and tested the new receivers at the National Solar Thermal Testing Facility, studying their ability to withstand high temperatures and pressures
while absorbing sunlight as
heat that can be stored or transferred to a power cycle to generate electricity.
The coat radiates more
heat to the cold sky than it
absorbs from its surroundings, the team reports, causing the temperature to drop below that of the surrounding air,
while thick insulation reduces body
heat loss from the skin.
Phytoplankton are tiny organisms that are critical in offsetting climate change because they undergo a process called photosynthesis, whereby they
absorb large enough amounts of
heat - trapping carbon dioxide to cool Earth's warming environment
while releasing much of oxygen we breathe.
Green roofs, green streets, rainwater gardens, and bioswales can
absorb storm water runoff,
while also cooling city blocks suffering from the urban
heat - island effect during hot summers.
And
while CO2 lets light reflect back into space from Earth's surface, it
absorbs heat.
While NASA's Wide - field Infrared Survey Explorer (WISE) failed to the tell - tale warmth of gas giants like Saturn within 10,000 AUs and larger than Jupiter objects out to 26,000 AUs (NASA / JPL news release), an icy «super-Earth», would have been too cold and faint for WISE to detect — even if the hypothesized planet has a small internal
heat source and
absorbs some sunlight.
Easily
absorbed by the skin without greasy feeling just like putting a lotion on it
while a pure coconut oil has a greasy feeling because it has been
heated in the process.
This pizza stone
heats evenly - making sure there are no hot spots -
while moisture is
absorbed so the crust is nice and crisp.
At Currently Crushing, we have the tips, direction and info that you need to stay cool
while absorbing the summer
heat.
The best basking platforms will
absorb heat and stay warm (like dark rocks), this way the basking platform will be warm to the touch which can warm your beardies underside
while he / she basks beneath the light.
While some dogs will dive straight in and splash about, other more water - shy pooches will need more encouragement — but even getting them to stand in the water for a short time is a really effective way of cooling them down rapidly as dogs
absorb and release
heat through their paws.
That
heat must be dissipated to space, and CO2 (which does not
absorb in the UV or visible range), adds to the emissivity of the stratosphere at the warmed temperature,
while adding much less to the absorptivity.
While it is true that infrared is
absorbed in a thin skin at the top of the water, even if the water were completely quiescent this would still lead to the skin layer
heating up until emission (plus evaporation and all the other terms we include in the surface budget) equalled the energy input.
Carbon dioxide, methane, etc are called greenhouse gases precisely because they can
absorb infra - red (IR)
heat energy,
while the other 99 + % of the atmosphere can not.
Herschel used three thermometers with blackened bulbs (to better
absorb heat) and, for each color of the spectrum, placed one bulb in a visible color
while the other two were placed beyond the spectrum as control samples.
While the warming of average global surface temperatures has slowed (though not nearly as much as previously believed), the overall amount of
heat accumulated by the global climate has not, with over 90 percent being
absorbed by the oceans.
«In recent years, from 2004 to 2011,
while the upper ocean is not warming, the ocean continues to
absorb heat at depth (e.g., Levitus et al. 2012; von Schuckman and Le Traon 2011), here estimated at a rate of 0.56 W m - 2 when integrating over 0 — 1800 m.»
While I have not found good numbers for the IR albedo (of either planet), the data I've seen indicates that most of the IR energy is either reflected back into space or
absorbed in the upper atmosphere (that's right - it does NOT
heat the surface).
As to the absorption of long - wave radiation from the earth's surface,
while it may be true that carbon dioxide and water together do
absorb certain frequency ranges of that radiation, I don't think that that matters a whole lot because most of the
heat from the surface is transported to the top of the troposphere by conduction, convection and latent
heat of vaporization of water during the day.
Ozone is abundant here and it
heats the atmosphere
while also
absorbing harmful radiation from the sun.
So the first explanation for how this works, the original, is the now classic «greenhouse glass like barrier stopping longwave from the Sun from entering the atmosphere
while visible travels through and is
absorbed heating the Earth's surface which then radiates out thermal infrared, longwave.
This long period signal is topmost modulated which controls all scale - components,
while GHGs is almost the unique factor to directly
heat the air by
absorbing the longwave radiation from the Earth surface.
Volcanic eruptions and El Niño events are identified as sharp cooling events punctuating a long - term ocean warming trend,
while heating continues during the recent upper - ocean - warming hiatus, but the
heat is
absorbed in the deeper ocean.
A slight change of ocean temperature (after a delay caused by the high specific
heat of water, the annual mixing of thermocline waters with deeper waters in storms) ensures that rising CO2 reduces infrared
absorbing H2O vapour
while slightly increasing cloud cover (thus Earth's albedo), as evidenced by the fact that the NOAA data from 1948 - 2008 shows a fall in global humidity (not the positive feedback rise presumed by NASA's models!)
Global warming seems to have slowed over the past 15 years
while the deep ocean has been observed in
absorbing the
heat instead.
While methane doesn't stay in the atmosphere as long as carbon dioxide, it
absorbs 84 times more
heat, making it very harmful to the climate.
Over the past 50 years, the oceans have
absorbed about 90 % of the total
heat added to the climate system
while the rest goes to melting sea and land ice, and warming the land surface and atmosphere.
What is ACTUALLY happening now is that the atmospheric greenhouse effect is getting stronger; and at the same time the circulations of water and air and
heat and cloud and so on around the globe are going on their merry chaotic way, meaning that we are going to have unpredictable short term variations
while there is a continual flow of
heat into the ocean from the energy imbalance between what is being emitted and what is being
absorbed.
Because of its molecular structure, carbon dioxide is a greenhouse gas, which means it allows visible light from the Sun to pass through the atmosphere
while absorbing and reemitting infrared energy,
heating the Earth.
The small balls are held by the rotation of the chamber as in a centrifuge on its inner wall
while absorbing the
heat.
Not only will melting Arctic sea ice raise global sea levels, it will also allow the earth to
absorb more
heat from the sun because ice reflects the sun's rays
while blue open water
absorbs it.
While a range of factors can contribute to warmer seawater, both the frequency and severity of these bleaching events is expected to increase in line with global temperatures, as the ocean
absorbs much of the extra
heat.
(having eye problems at the moment so could take quite a
while, also try to ignoro typos) But from the descriptions, these new calculations seem to deal with the actual sites and at - site changes in
heat absorbing surfaces.
When this wells to the surface in the tropics it
absorbs vast quantities of (missing)
heat, increasing in temperature by about 20C
while releasing CO2.
While a greenhouse warms the air by allowing in and retaining
heat and not allowing in cooling air, greenhouse gases warm the planet by
absorbing the Sun's
heat and then reemitting it into the atmosphere.
While the location of the hottest place on Earth might shift from year to year, the conditions that give rise to it remain the same: Dry, rocky and dark - colored lands are good at absorbing heat, while lighter sand will tend to reflect more sunl
While the location of the hottest place on Earth might shift from year to year, the conditions that give rise to it remain the same: Dry, rocky and dark - colored lands are good at
absorbing heat,
while lighter sand will tend to reflect more sunl
while lighter sand will tend to reflect more sunlight.
This 3W / m ^ 2 of
absorbed radiation that the models currently under represent, chiefly from earlier observed spring snow melts
while they allegedly «match» the 20th century climate, will be added as the models project the next 100 years, catching up with the snow melt, an addition of
heat comparable to the projected CO2 forcing.
The black, back surface of each bottle
absorbs heat,
while reflective inner surfaces reflect UV rays within the water itself.