Sentences with phrase «temperature of water»

There's two buttons for single or double espresso and one for tea (which raises the temperature of the water and extracts for longer).

«The high temperature of the water kills bacteria and extracts the dirt out of the carpet,» says Tony Solis of All Points Carpet Care in Mooresville, N.C. «It's a very deep cleaning compared to dry cleaning.»

To lower your next water bill, drop the temperature of your water heater to warm (about 120 degrees).

«I'll test the temperature of the water incrementally, [and] I tend to try to decide early on whether I have a «push - cross» or «pull - cross.»

Near - drowning accidents can vary in severity, depending on a number of factors including the length of time the child is submerged, the temperature of the water, the type of water, the amount of water aspirated and the child's medical condition before the accident occurred.

Notice the temperature of the water.

It takes much more energy to raise the temperature of water than land, but it also cools much slower.

The temperature of the water below the surface can be considerably warmer than the surface due to SW radiation penetrating during the day and it tends to stratify.

Clouds can affect the temperature of the water going into the oscillations, and this I think is the likely cause of the 20th century global temperature pattern.

This instability occurs because the melting point temperature of water decreases as you go deeper in the ocean, where pressures are higher.

The point is opening the cold water tap moderated the warming effect of water flowing from the hot tap, thus the temperature of the water from the hot tap no longer correlated with the temperature of the water accumulating in the tub.

You posted an estimate of the 0.02 * C rise in temperature of that water.

During the war most measurements were by US ships which measured the temperature of water piped from the sea into the engine room.

Moreover, the change of temperature of the water that is problematic for the octopus, is favourable for the crab.

The instrument in that case is seeing the temperature of the water vapor very close the ground.

Ambient temperature of the water just increases the odds of any one molecule peeling off the surface as vapor.

As hot water drains from the tank, in - flowing cold water lowers the overall temperature of the water in the tank.

It works by sensing the increase in apparent microwave brightness temperature of the water surface caused by more foam as the wind increases.

At no point does the average temperature of the vapor exceed the average temperature of the water from which it sprang so the air near the surface never gets any warmer either.

... your uneasiness might arise from wondering how these models produce anything sensible given the temperature dependence of the saturation vapor pressure over water, the freezing temperature of water, and the dependence of feedbacks on temperature parameter space.

With regards to the evaporation, surely while it does lower the temperature of the water it can not raise the temperature of the air above that of the ocean.

8 21.1 Factors That Affect Climate Water Bodies • Large bodies of water such as lakes and oceans have an important effect on the temperature of an area because the temperature of the water body influences the temperature of the air above it.

What I am saying is if there was «extra heat» being stored in the deep sea it would most likely increase the temperature of the water and increase the speed of the «conveyor».

In other words, the stepwise increase of the back radiation by the additional 0.062 W / m ^ 2 per year results in the stepwise increase of the temperature of water (within the layer of 5 cm) by 0.00005 K per year.

The TEMPERATURE of the water (its average kinetic energy) determines the rate of both evaporation and radiation.

By analyzing the emission from the ocean, we can use S - B to calculate the temperature of the water that emitted photons.

As such, it represents the actual temperature of the water across a very small depth of approximately 20 micrometers....»

The results indicate the reduction of the temperature difference between the bulk temperature of water (5 cm below the surface) and the temperature of the surface skin layer (which is approximately 1 mm thick), by approximately 0.002 K / (W / m ^ 2) as compared to the temperature difference without the additional increase of back radiation.

i.e. if c is higher, then also dQ must be higher in order to get the same dT with the same m. Thus the same number of the longwave photons will give a smaller rise of temperature of water as compared to the material in the pavement.

250 feet below the ocean's surface: The above plot shows the temperature of the water in the Gulf of Mexico and northwestern Caribbean Sea in September, 2005, at a depth of 250 feet.

I'm fixing the skin temperature of the water and don't care about the details of how that's maintained.

Describe what happens to the temperature of the water and water vapor pressure.

This gives $ T = Q / (c * m) = 0.00005 K for the increase of the average bulk temperature of water (from surface and up to 5 cm deep) due to the increase of the back radiation by 0.062 W / m ^ 2.

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.

Excess heat from power - generating reactions increase the temperature of the water as it is discharged, which in turn raises the temperature of the overall aquatic environment.

It seems that only short wave radiation penetrating into water will actually result in a rise in temperature of the water volume.»

The temperature of the water plus alcohol warmed up several degrees, while the ice remained at its freezing point.

Judith Curry writes, «how [can] these models produce anything sensible given the temperature dependence of the saturation vapor pressure over water, the freezing temperature of water, and the dependence of feedbacks on temperature parameter space.»

Earth with no greenhouse gasses would have a equivalent emitting temperature commonly given as -18 C, well below the freezing temperature of water.

It forms the basis of such things as infrared cameras, which show the temperature of water as easily as that of solids.

The text quoted says «each inflow is not only variable in volume of water transported but also in the temperature of the water imported.»

Actually, the ice cube will displace exactly the same mass as it contains; therefore, the water level after the ice melts will be exactly the same as before the ice melted - if the temperature of the water is allowed to return to its starting point.

Observations suggest that variability in oceanographic conditions in the Arctic is very largely driven by the consequences of the flows through open passages to both Atlantic and Pacific Oceans, which themselves respond to the different and characteristic variability of the circulation patterns of each ocean: each inflow is not only variable in volume of water transported but also in the temperature of the water imported.

JC note: The freezing temperature of water depends on the salinity of the water — more salt means a lower freezing temperature (the same effect of salting your driveway in winter).

Note: Before I get hammered, I know this is a sloppy analogy because in it we are dealing with a phase transition and the temperature of the water will never rise above 100C.

Similarly the criteria for water readings to be taken immediately recognises that a small sample of water left in the sun quickly escalates in temperature and that a thermometer kept on a hook in the sun takes time to reflect the ambient temperature of the water (of course some buckets eventually contained an integral thermometer)

For the sipunculans, richness may be linked to the temperature of the water masses during the year [289], which reflects a physiological barrier between cold and warm water for cold - and warm - water species.

The temperature of the water will go up until those rates are matched again, but now the equilibrium temperature will be higher.

At Crater Lake, annual snowfall has decreased each decade since the 1950s, and the surface temperature of the water has increased by 6 degrees Fahrenheit.

The time series uses - an area - weighted average of the surface air temperature over land and the temperature of water at the ocean's surface.