Sentences with phrase «absorb more heat as»

As you opting for a black color, be wise that black color absorbs more heats as compared with other colors.

Not exact matches

The first is that our planet's oceans act as a massive watery heat - sink, and currently absorb more than 90 percent of increased atmospheric heat that are associated with human activity.
If you're using a more mild buffalo sauce, but you like a ton of heat, you may add a little bit of ground cayenne to the lentils as they're absorbing the buffalo sauce.
As a final note, if you cover the milk after heating it and let it sit for 10 minutes, covered, it will absorb more bouquet from the vanilla bean.
As the climate changes, Southern Ocean upwelling may increase, which could accelerate ice shelf melting, release more carbon into the atmosphere and limit the ocean's ability to absorb heat and carbon dioxide from the atmosphere.
The tiny particles also serve as condensation nuclei for clouds and are trapped between cloud particles, where their ability to absorb heat helps dry up those clouds and allows more sunlight to reach Earth.
For example, photonic crystals could funnel excess heat from a power plant's generator and release it over a much smaller band of frequencies to drive engines — such as those in electric - powered cars that can absorb energy only within a small range — much more efficiently.
But as the food starts getting a bit brown, that brown part gets darker and darker and begins to absorb more and more heat.
Hyperthermia (hyperpyrexia), in its advanced state referred to as heat stroke or sunstroke, is an acute condition which occurs when the body produces or absorbs more heat than it can dissipate.
As ammonium levels in the heated soil increased, trees grew faster and absorbed more carbon.
As the sun flushes heat into our atmosphere at a mind - boggling rate of 175 quadrillion watts, the air near the equator absorbs more energy than the air near the poles.
For as much as atmospheric temperatures are rising, the amount of energy being absorbed by the planet is even more striking when one looks into the deep oceans and the change in the global heat content (Figure 4).
This also produced heavy elements that were not on earth before the flood (elements heavier than lead, such as bismuth, polonium, radon, radium, thorium, uranium, etc.) The greater the heat, the more heavy elements formed and absorbed that heat.
The underlying logic is sound: as sea ice melts, it exposes darker ocean water, which absorbs more of the sun's heat, causing the water temperatures to increase.
You may need to add slightly more water during cooking, as the water can be absorbed at different speeds depending on the shape of your pan and the heat under it.
Also, avoid wearing the black color outfit as it absorbs more heat and you'll feel very hot!
You might try putting the bag with the desiccants in light as it will heat up the bags and cause them to absorb more humidity.
Traditional roofs are a dark color and, as many of us know, dark absorbs more heat.
Ice crystals block the airflow, less heat is absorbed into the evaporator, more ice is formed, less airflow... The TXV bulb will radically drop in pressure as the evap temperature approaches freezing, and cause the TXV to completely shut off liquid refrigerant flow into the evaporator to prevent this condition.
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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.
The changes seen in the MSU 4 data (as even Roy Spencer has pointed out), are mainly due to ozone depletion (cooling) and volcanic eruptions (which warm the stratopshere because the extra aerosols absorb more heat locally).
As things heat up, I would therefore expect that hotter air will create less dense air and that said, air expansion would push the jet streams north and south as the tropics get more sunlight and the heat is trapped in the climate system, and absorbed slowly by the oceanAs things heat up, I would therefore expect that hotter air will create less dense air and that said, air expansion would push the jet streams north and south as the tropics get more sunlight and the heat is trapped in the climate system, and absorbed slowly by the oceanas the tropics get more sunlight and the heat is trapped in the climate system, and absorbed slowly by the oceans.
Since it is later in the afternoon, this gives the ground a chance to heat up, and as a consequence, rather than being absorbed, the precipitation is more likely to evaporate, drying out the soil, the plants, etc..
There are subtle effects such as the planet losing more heat from the open sea than from ice - covered region (some of this heat is absorbed by the atmosphere, but climates over ice - covered regions are of more continental winter character: dry and cold).
But by changing the planet's albedo through a large seasonal variation, the total insolation is changed — more sunlight is reflected back into space without being absorbed as heat.
To summarize this concept, do you agree that when a layer's temperature is due to heat absorbed by CO2 alone, more CO2 will increase the temperature, whereas if the temperature includes heating from something else as well, more CO2 can help rid the layer of that extra heat?
According to the scientist conducting the study, the soot — which comes from the Chindia belt, as well as the Western world — and which is black, absorbs heat from the sun more readilly than white ice, thereby accelerating the warming and melting of the glaciers even more than the Greenhouse effect.
CO2 traps heat According to radiative physics and decades of laboratory measurements, increased CO2 in the atmosphere is expected / predicted to absorb more infrared radiation as it escapes back out to space.
Isn't it evident that as the surface warms the ocean heat sink will tend to absorb more heat, and that if the surface cools then the ocean releases heat?
As we lose ice, less heat gets reflected and more heat gets absorbed and ice melts even more.
In the Arctic, the tipping points identified in the new report, published on Friday, include: growth in vegetation on tundra, which replaces reflective snow and ice with darker vegetation, thus absorbing more heat; higher releases of methane, a potent greenhouse gas, from the tundra as it warms; shifts in snow distribution that warm the ocean, resulting in altered climate patterns as far away as Asia, where the monsoon could be effected; and the collapse of some key Arctic fisheries, with knock - on effects on ocean ecosystems around the globe.»
For as much as atmospheric temperatures are rising, the amount of energy being absorbed by the planet is even more striking when one looks into the deep oceans and the change in the global heat content (Figure 4).
Still, they indicate that some areas of the ocean are heating up especially fast, such as the Arctic Ocean — which this year had its lowest winter ice year on record — and is absorbing much more solar energy as melting ice cover exposes new dark surfaces.
Bobby, I believe most of the heat is absorbed and light that reflects would likely be sent right back out to space - granted some of it would hit clouds and turn to some heat there, but generally, the light that hits the earth now stays on the earth - if it's reflected back out to space as light then that's where it goes, back out to space and therefore it would actually cool the earth more to reflect it back to space.
Note, for example, how the temperature trend in the first decade of the 21st century was generally flat because an upward push by anthropogenic forces was temporarily offset by a downward pull as solar activity decreased and the oceans absorbed more heat than usual from the atmosphere (sea water temperatures continued to rise).»
For example, the scientific explanation that temperatures have not risen since 2001 is because an «upward push by anthropogenic forces was temporarily offset by a downward pull as solar activity decreased and the oceans absorbed more heat than usual from the atmosphere (sea water temperatures continued to rise)».
The heating is uneven, because of night and day, because different surfaces (such as rocks and trees) absorb and reflect sunlight in different amounts, and because sunlight hits the equator more directly than the poles.
«As sea ice melts, the Arctic waters absorb more heat in the summer, having lost the reflective powers of vast packs of white ice.
This is a fortuitous thing, for if there was not this alteration of the energy flow, with the oceans absorbing more heat being the excellent heat sink they are, we'd have a much faster warming troposphere as greenhouse gases increase.
As the snow and ice that reflect much of the sun's energy melt, more heat is absorbed, accelerating the melting and amplifying global warming.
But if a little more energy is absorbed, then CO2 is acting like a little black soot in the atmosphere and it will, in turn, radiate more toward space as a black box would from the added heat and this might compensate for the change in albedo.
Bill Gray has a favorite diagram, taken from a 1985 climate model, showing little nodules in the center with such labels as «thermal inertia» and «net energy balance» and «latent heat flux» and «subsurface heat storage» and «absorbed heat radiation» and so on, and they are emitting arrows that curve and loop in all directions, bumping into yet more jargon, like «soil moisture» and «surface roughness» and «vertical wind» and «meltwater» and «volcanoes.»
Both wetland drying and the increased frequency of warm dry summers and associated thunderstorms have led to more large fires in the last ten years than in any decade since record - keeping began in the 1940s.9 In Alaskan tundra, which was too cold and wet to support extensive fires for approximately the last 5,000 years, 105 a single large fire in 2007 released as much carbon to the atmosphere as had been absorbed by the entire circumpolar Arctic tundra during the previous quarter - century.106 Even if climate warming were curtailed by reducing heat - trapping gas (also known as greenhouse gas) emissions (as in the B1 scenario), the annual area burned in Alaska is projected to double by mid-century and to triple by the end of the century, 107 thus fostering increased emissions of heat - trapping gases, higher temperatures, and increased fires.
If the heat isn't released, the next day the thermal mass will absorb more heat and start acting as a heater, emitting or radiating heat, and contributing to the overheating risk.
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.
Those claims have resonated; two years ago, the United Nation's Intergovernmental Panel on Climate Change felt the need to explain why the Earth was not heating up as expected, listing such reasons as volcanic eruptions, reduced solar radiation and the oceans absorbing more heat.
Since to me (and many scientists, although some wanted a lot more corroborative evidence, which they've also gotten) it makes absolutely no sense to presume that the earth would just go about its merry way and keep the climate nice and relatively stable for us (though this rare actual climate scientist pseudo skeptic seems to think it would, based upon some non scientific belief — see second half of this piece), when the earth changes climate easily as it is, climate is ultimately an expression of energy, it is stabilized (right now) by the oceans and ice sheets, and increasing the number of long term thermal radiation / heat energy absorbing and re radiating molecules to levels not seen on earth in several million years would add an enormous influx of energy to the lower atmosphere earth system, which would mildly warm the air and increasingly transfer energy to the earth over time, which in turn would start to alter those stabilizing systems (and which, with increasing ocean energy retention and accelerating polar ice sheet melting at both ends of the globe, is exactly what we've been seeing) and start to reinforce the same process until a new stases would be reached well after the atmospheric levels of ghg has stabilized.
As obvious on figures 6 - A and 6 - B, Ttop and Ptop are determined by the water vapour that radiates over some 1900 cm - 1 much more than the 40 cm - 1 of the tropospheric CO2 near 614 cm - 1 and 718 cm - 1.; stratospheric radiation to the cosmos is not very important because the cooling of each layer is exactly equal to its heating mostly by UV absorbed by Ozone.
The less cloud formation the more heat is absorbed by earth (the oceans act as buffers for this energy).
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