The darkest blue indicates deeper water, but it's also this shade for another reason: the rich blue hue comes from dye added to speed up the rate at which
the water absorbs sunlight and warmth, aiding evaporation.
Not exact matches
There are more, however, including the amount of
sunlight an ice sheet is able to reflect; the larger an ice sheet, the more
sunlight is reflected, but the smaller an ice sheet, the more ocean there is surrounding the ice sheet to
absorb the
sunlight which in turn heats up the surrounding
waters increasing the melt which decreases the size of the ice sheet which in turn... and so goes the cycle.
The result is ammonium nitrate and ammonium sulfate, molecules that condense with others of their kind, plus
water, to form tiny particles in the air that
absorb sunlight and block visibility — smog.
Chloroplasts
absorb sunlight and use it in conjunction with
water and carbon dioxide gas to produce food for the plant.
Sunlight would strike the top electrode, which would
absorb photons and catalyse the
water - oxidation process.
But not all the
sunlight would be
absorbed by this electrode: light with a wavelength longer than 600 nanometres isn't
absorbed by the rust - coloured
water in the top cell so would pass through to strike the lower electrode, powering the production of hydrogen.
A possible cause for the accelerated Arctic warming is the melting of the region's sea ice, which reduces the icy, bright area that can reflect
sunlight back out into space, resulting in more solar radiation being
absorbed by the dark Arctic
waters.
They incorporated a photocatalyst in a moisture -
absorbing, semiconducting paint that can produce hydrogen from
water in the air when exposed to
sunlight.
Warmer temperatures melt the Arctic ice and exposes
water, which
absorbs more
sunlight than ice.
«The job of the photoanode is to
absorb sunlight and then use that energy to oxidize
water — essentially splitting apart the H2O molecule and rearranging the atoms to form a fuel.
The scientists focused on bismuth vanadate, a thin - film semiconductor that has emerged as a leading candidate for use as a photoanode, the positively charged part of a photoelectric cell that can
absorb sunlight to split
water.
Ice and snow scatter, transmit, and
absorb sunlight and radiant heat much differently than
water.
The Arctic is warming more than twice as fast as the rest of the planet, because as ice melts at the top of the world, there is less of it to reflect
sunlight back into space, so more of it is
absorbed by ocean
waters; more
absorbed sunlight means even warmer temperatures, which means more ice melt a circular process known as Arctic amplification.
Hot spring
water rich in silica and other minerals
absorbs all the colors of
sunlight except for the deep blues that make many of Yellowstone's hot springs so beautiful.
Through photosynthesis, phytoplankton
absorbs sunlight, which it stores in sugars it makes from CO2 and
water.
While staring at the ocean or at rivers spilling into Bristol Bay, he began to
absorb the way
sunlight, shadows, and wind affected the color and texture of the
water.
And what part of the SW of incoming
sunlight is
absorbed by
water vapour, and how much (W / m2)?
Some gases in Earth's atmosphere — mostly
water vapor and carbon dioxide — let
sunlight pass through mostly unhindered, but
absorb infrared light from the ground.
The exposed open
water caused by the wind divergence may
absorb some additional
sunlight and melt more ice than usual over the next few weeks (temperature - albedo feedback)[related NASA animation], but given that the sun is well on its way to setting for the winter, I think this effect will be fairly minimal.
If something triggers a cool spell, such as an orbital variation reducing incident
sunlight, then
water freezes at the poles, which increases the Earth's albedo, while the cooler oceans
absorb more CO2, reducing the greenhouse effect.
This is of particular concern to scientists because of the albedo effect, where the replacement of highly reflective sea ice with darker open
water greatly increases heat
absorbed from
sunlight.
When bright, white, reflective ice melts to reveal darker ocean
water,
sunlight that would normally bounce back into space is
absorbed instead.
Enhanced
water vapor
absorbs more incoming
sunlight and reflection from snow and ice declines.
Additionally, the less sea ice covers the surface of the ocean, the more
sunlight is
absorbed by the
water, which scientists warn could accelerate the Arctic's warming.
Water breeds more water because it absorbs most of the sunlight falling o
Water breeds more
water because it absorbs most of the sunlight falling o
water because it
absorbs most of the
sunlight falling on it.
Global warming has a larger affect in polar areas, as the loss of snow and ice leads to more open
water, which
absorbs more
sunlight and warmth.
Now if had bowl of
water and
sunlight shines thru the
water, the «dark light» would be
absorbed by the
water, yes?
We know that more open
water will put more
water vapor in the air, and increase the
sunlight absorbed each summer, both of which will lead to yet more warming.
Sunlight absorbed by the
water is the source of energy in the system (explained well by Bob Tisdale above) so it's ocean temperatures that drive the winds.
There is nothing implausible about dark
water absorbing more
sunlight energy than ice, and there is nothing implausible about more energy resulting in warmer temperatures.
It
absorbs 1 / 7th as much IR, heat energy, from
sunlight as
water vapor which has 188 times as many molecules capturing 1200 times as much heat making 99.9 % of all «global warming.»
They merely trigger the condensation of
water vapour (which saturates very easily in low pressure air) into cloud droplets which reflect back
sunlight to space, rather than
absorbing infrared as
water vapour does.
Basically, Dr Ferenc Miskolczi's life as a NASA climate research scientist was made hell because he discovered that the extra
water vapour being evaporated is not having a positive - feedback (increasing the CO2 warming effect by
absorbing more infrared from the sun), instead it is going into increased cloud cover, which reflects incoming
sunlight back to space.
Water vapour molecules absorb wideband infrared, so the sunlight filtered through water will tend to lose the far red end of the spectrum, and appear slightly b
Water vapour molecules
absorb wideband infrared, so the
sunlight filtered through
water will tend to lose the far red end of the spectrum, and appear slightly b
water will tend to lose the far red end of the spectrum, and appear slightly bluer.
And, in this case, what Dr. Meier is referring to is the fact that the albedo (reflectance) of ice is higher than
water so that when the arctic is ice - covered, more
sunlight gets reflected and less is
absorbed.
When
sunlight strikes ice and snow, most of it is reflected back into space, but if it instead strikes land or open
water, then much of the energy in the light is
absorbed and converted into heat, leading to higher temperatures.
A lot of visible
sunlight is
absorbed during the day by
water that is part of the subskin layer.
An example of a feedback loop is when melting ice turns to
water,
absorbs more
sunlight because
water is darker than ice, heats up, and causes more melting.
The process was accelerated because dark, open
water absorbed more
sunlight.
Water is fairly transparent to visible light allowing
sunlight to penetrate to a depth of about 100 meters before it is completely
absorbed.
While pollution in some areas provides nuclei for
water to condense on to form clouds, in other places there may be soot particles, which could
absorb sunlight and cause the cloud to burn off (evaporate) during the day, leaving less cloud to warm the night.
The only way CO2 could
absorb any more IR than it is already
absorbing is if 1) the surface started re-emitting more IR, which could only happen if more
sunlight reached the surface, or 2) atmospheric
water vapor levels dropped, freeing up more IR to be
absorbed by CO2, in which case, warming would not occur, because that radiation was already being
absorbed by the
water vapor that disappeared.
The caveat is that these molecules can weakly
absorb sunlight in the near IR and visible on combination and overtone bands, mostly of
water vapor, and on weakly
absorbing forbidden transitions such as the Chappius bands of ozone, and for very low concentrations of dimers.
By draping black, carbon - dipped paper in a triangular shape and using it to both
absorb and vaporize
water, they have developed a method for using
sunlight to generate clean
water with near - perfect efficiency.
I'm sure some of it is
absorbed by living organisms, that may do all sorts of things with it; most mpost of the ocean
waters don't have living organsims everywhere to use the
sunlight for something.
This is quite different from the positive feedback that follows when Arctic ice — which reflects
sunlight — melts and gives way to blue
water which
absorbs solar energy, thus accelerating the melting.