Sentences with phrase «more water absorption»

The cookies may be slightly more gummy because of the finer grind and more surface area of the milled flour, which causes more water absorption and retention.

Not exact matches

Soaking nuts in warm salt water helps to minimize or eliminate the enzyme inhibitors they contain, increases B vitamin levels, and makes the proteins in the nuts more readily available for absorption.

The researchers, led by Giovanna Tinetti based at the Institut d'Astrophysique in Paris, France, say their new analysis is more reliable because the observations were taken in infrared light, which is far better at detecting light - absorption patterns unique to water.

It may seem counterintuitive, but showering in chlorinated water can lead to more chlorine absorption than drinking chlorinated water.

When you soak chia in water, it creates a gel that helps slow the absorption of sugars, and helps coat the gut lining... Read More»

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In the morning, if there is still salt at the bottom of the jar the water has absorbed its maximum amount and the Sole is ready to use; if all salt is absorbed, add a little more until water has reached maximum absorption.

What is meant by the statement you quoted is that you are taking into account water weight when you eat brown rice so you will get full quicker because it takes up more space due to the liquid absorption from boiling.

As hypertonic drinks contain more glucose than body fluids, absorption from the gut and rehydration is slower than if you drink just water.

Patented water - soluble formula increases fatty acid and nutrient absorption 3 - 5 times more efficiently than traditional oil or emulsified products

[Response: There is a fundamental difference btw the stratosphere and the troposphere because of the presence of massive amounts of water vapour — implying that the LW absorption is far more (spectrally) widespread than in the stratosphere.

It's more useful to think of the stratosphere and above as being radiatively heated / cooled in specific bands (as opposed to a more general absorption / emission in the troposphere — mainly due to water vapour).

Note that ocean water has a lower albedo than most coastal terrains — rising sea levels mean more absorption.

Thus, if the absorption of the infrared emission from atmospheric greenhouse gases reduces the gradient through the skin layer, the flow of heat from the ocean beneath will be reduced, leaving more of the heat introduced into the bulk of the upper oceanic layer by the absorption of sunlight to remain there to increase water temperature.

As the absorption spectra of water vapour and CO2 overlap, Hug's experiment fails to take into account the fact that CO2's effects would be more pronounced at higher altitudes and lower temperatures, hence his number is far too low.

It is the only technology that acts to directly reduce the temperature of the ocean (it was estimated one degree Fahrenheit reduction every twenty years for 10,000 250 MWe plants in» 77), eliminates carbon emissions, and increases carbon dioxide absorption (cooler water absorbs more CO2) at the same time.

The vertically integrated inventory of human emitted CO2 in the oceans is (not surprisingly) much greater in areas of cold deep convection, especially in the northern Atlantic (the falling leg of the thermohaline circulation), and much less in the tropics where the ocean is strongly stratified; absorption in the tropics really is more in the near - surface waters.

Also you focused on re-radiating meaning emitting long - wave spectrum - which possible, but I was thinking more about emitting the same wavelength, as mentioned in this quote: «However, aerosols (which often contain water and if so can absorb red wavelengths) are usually larger than visible wavelengths and therefore absorb and reflect all wavelengths of light equally (this is not technically scattering, although it is often called that; it technically involves absorption and re-radiation, or reflection).»

For a while there is no LTE, there is more absorption by the water than emission.

(1) exaggerates the warming from more CO2 because it does not account of the overlapping absorption bands of water vapor and ozone, but we will use it for a «worst case» analysis.

As a result, it would be more accurate to represent about half of the CO2 absorption (bar width) as being absorbed by water vapor.

Ocean waters globally have become 30 % more acidic due to absorption of large amounts of human - produced carbon dioxide (CO2) from the atmosphere.

To make things more exciting I'll raise the temperature of the top wall from 293.15 K to 373.15 K. Two things happen immediately, the temperature of the water vapor goes up by conduction and absorption of radiation from the top wall and so does the temperature of the surface of the water.

We need to explain how warmer waters absorbing less CO2 could become less alkaline as seems to have been happening... Less CO2 absorption should mean more alkaline oceans but they have been getting less alkaline.

«how it is supposed to work» = according to non-real-world theoretical models that say CO2 molecules that are spaced together 1/20, 000 ths more closely today than they were in 1990 function just like a blanket draped over the ocean waters, and this CO2 blanket determines the net heat changes in the depths of the ocean more so than variations in direct shortwave radiation absorption does.

The ocean's absorption of anthropogenic CO2 has already resulted in more than a 30 % increase in the acidity of ocean surface waters, at a rate likely faster than anything experienced in the past 300 million years, and ocean acidity could increase by 150 % to 200 % by the end of the century if CO2 emissions continue unabated (Orr et al. 2005; Feely et al. 2009; Hönisch et al. 2012)

Carbon absorption can initiate a feedback loop in which underoxygenated waters breed different kinds of microbes that turn the water still more «anoxic,» first in deep ocean «dead zones,» then gradually up toward the surface.

It follows from this that the logarithmic dependence of the outgoing longwave radiation (which by the way, has to do the the exponential decay of the absorption coefficient away from the center of the absorption line) can still lead to significant temperature changes, particularly since water vapor enhances the value of λ and smoothes out a plot of the outgoing radiation vs. temperature (making it more linear than T ** 4).

He finds that UV radiation is high near water bodies and sand because there is more reflection than absorption of solar radiation.

What is also happening here is «absorption», the longer wave lengths of light get absorbed by water earlier than the shorter waves lengths, red light doesn't penetrate as deeply as blue light because it gets absorbed more readily.