Sentences with phrase «dry air rises»

A packet of dry air rises.

When hot dry air rises, it cools at a lapse rate of 9.78 °C / km - this is known as the dry adiabatic lapse rate (DALR).

These winds start with hot, dry air rising into overhead thunderstorms, Henson explained.

Not exact matches

sherri, I would make a guess that it's your dry (compared to our humid, rainforest - like humidity) air, the flour is sucking up lots more liquid than mine, I think... that might explain Ruhlman's slack dough, since Cleveland is more humid, even, than up here... add more water until you get a dough that feels right to you, the starter should have plenty of power to make it rise!

So when I bake bread in the wintertime, it takes a bit longer to rise since the air is not only a bit colder, but quite a bit drier.

It's very absorbent, has a high rise, can be customized quite well for absorbancy, has a nice narrow in between the legs area, is nice and soft after air drying then tumble dry on low heat or no heat... and yeah, great diaper.

Rising temperatures also tend to degrade air quality, whether through dusty dry plains, soot from wildfires or ozone in cities, leading to asthma attacks and heart troubles.

A low - altitude flow of warm, moist air from an ocean area combined with a flow of cold, dry polar air high up creates maximum instability, which means that parcels of air heated near the surface rise rapidly, creating powerful updrafts.

These storms result from the vertical circulation of water in the top layers, leaving large areas where air descends and becomes dry like the Sahara desert, and other areas where water rises to form the thunderstorms.

The rising air corresponds to areas of unsettled, rainy weather, while the sinking air creates a stable, dry clime.

The eastward shift in the Walker Circulation means the normal area of rising air and rainy weather is shifted eastward as well, leaving the Indonesian area high and dry during much of the year.

As the air rises and moves poleward, it dries, cools, sinks, and returns back to the surface completing this atmospheric cycle both north and south of the equator.

On days when you want to air dry your rose blonde hair and go, spritz on the L'Oréal Paris Advanced Hairstyle AIR DRY IT Wave Swept Spray and let your hair air ddry your rose blonde hair and go, spritz on the L'Oréal Paris Advanced Hairstyle AIR DRY IT Wave Swept Spray and let your hair air dDRY IT Wave Swept Spray and let your hair air drydry.

I really like, and use, some of the masks, the Seaberry Face Oil was lovely and effective for helping to heal the latter stages of my last Rosacea flare - up; Black Tea Corset Cream; Black Tea Firming Overnight Mask; for lots of moisture if your skin is very dry try tiny bits of Rose Deep Hydration Face Cream (which I use more of in the arid air of Colorado).

The air tends to be driest around March 1st, when the relative humidity falls below 42 % (comfortable) three days out of four, whilst it's usually at its most humid around March 29th, when the relative humidity rises above 84 % (humid) three days out of four.

The air is driest around May 1st, when the relative humidity falls below 57 % (mildly humid) three days out of four, whilst it's at its most humid around May 6th, when it rises above 81 % (humid) three days out of four.

The air is usually at its driest around September 1st, when the relative humidity falls below 65 % (mildly humid) three days out of four, whilst it is at its most humid around September 23rd, when it rises above 85 % (very humid) three days out of four.

The air is usually at its driest around February 5th, when the relative humidity falls below 53 % (mildly humid) three days out of four, whilst the air is often at its most humid around February 25th, when it rises above 71 % (humid) three days out of four.

The air is usually at its driest around February 25th, when the relative humidity falls below 41 % (comfortable) three days out of four, whilst it's often at its most humid around February 19th, when it rises above 77 % (humid) three days out of four.

The air is usually driest around July 1st, when the relative humidity falls below 75 % (humid) three days out of four, whilst it's usually at its most humid around July 5th, when it rises above 91 % (very humid) three days out of four.

In the north, the air is driest around May 22nd, when the relative humidity falls below 64 % (mildly humid) three days out of four, whilst it's at its most humid around May 9th, when it rises above 88 % (very humid) three days out of four.

In the south, the air is driest around March 8th, when the relative humidity falls below 58 % (mildly humid) three days out of four, whilst it's at its most humid around March 21st, when it rises above 76 % (humid) three days out of four.

In the south, the air is driest around May 1st, when the relative humidity drops below 59 % (mildly humid) three days out of four, whilst it's at its most humid around May 31st, when it rises above 76 % (humid) three days out of four.

The air is predicted to be driest around June 1st, when the relative humidity drops below a comfortable 35 % three days out of four, whilst the most humid is expected to be around June 4th, where humidity levels could rise above a humid 78 %.

The air is driest around September 1st, when the relative humidity falls below 66 % (mildly humid) three days out of four, whilst it's at its most humid around September 27th, when it rises above 98 % (very humid) three days out of four.

The air tends to be driest around June 1st, when the relative humidity falls below 61 % (mildly humid) three days out of four, whilst it's often at its most humid around June 30th, when it rises above 89 % (very humid) three days out of four.

The air tends to be at its driest around December 12th, when the relative humidity falls below 57 % (mildly humid) three days out of four, whilst the air is at its most humid around December 1st, when it rises above 70 % (humid) three days out of four.

The air is driest around February 1st, when the relative humidity falls below 61 % (mildly humid) three days out of four, whilst it's at its most humid around February 16th, when it rises above 78 % (humid) three days out of four.

Positive feedback caused by rise in water vapour (caused by warming) accounts for perhaps half of the estimated warming and this will be located most where the air is humid in contradiction to Dyson's «cold and dry».

Overnight lows are rising, so the air stays drier after dusk.

Seems to me the debate about AGHG global warming and increasing TC frequency / intensity / duration boils down to the fact that as sea surface temperatures, as well as deeper water temperatures rise, the wallop of any TC over warmer seas without mitigating circumstances like wind sheer and dry air off land masses entrained in the cyclone will likely be much more devastating.

Air from the mid latitude cell, on the other hand procedes north at the surface (in the NH) before again rising to great altitude, drying it.

3) Cooler, (usually) drier air descends to replace the heated water vapour that has risen up to form clouds.

People are confused over whether I was questioning why moist air surounded by dry would rise, or why moist air would be surrounded by dry.

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The vapour, being lighter than air then rises, in the process altering the lapse rate from the dry rate to the moist rate.

So the whole rising air mass experiences less cooling than it would in a dry atmosphere.

Because temperatures can rise more quickly in drier air and than moister air, does a rising air temperature indicate more heat is trapped or less moisture is available?

However, there is also the expansion of the Hadley Cells where water vapor from tropical ocean evaporation rises, water in the form of rain falls out as the air cools with increased altitude, then dry air descends at poleward edge of the cells in the dry subtropics.

Heated by condensation on the rise, the descending dry air would adiabatically heat up at 9.8 deg C per 1000 meters and so that it would rapidly become warmer than surrounding atmosphere having a standard lapse rate of 6.5 deg C per 1000 meters.

The research found that fire - induced air pollution, including fine particulates and a rise in ozone, could be linked to thousands of deaths during El Nino years when dry conditions worsen human - set fires.

During the winter months, air that is heated inside the home rises toward the attic and can condense once it meets the colder exterior wall and roof surfaces, attic fans work to mitigate both these occurrences by replacing the attic air with ambient air, which is cooler and drier than the existing air space.

Wikipedia starts with «The dry adiabatic lapse rate (DALR) is the rate of temperature decrease with height for a parcel of dry or unsaturated air rising under adiabatic conditions.»

At low altitude and high temperatures (greater than 30 °C or 86 °F), over the ocean, it can reach 4.3 % or more of the atmosphere and is less dense than dry air, causing it to rise.

«The dry adiabatic lapse rate (DALR) is the negative of the rate at which a rising parcel of dry or unsaturated air changes temperature with increasing height, under adiabatic conditions.

So where there is water to evaporate the surface doesn't get warmer but instead the cloud deck rises about 100 meters per doubling and where there was once dry cool air above the clouds there's now a warm cloud occupying that layer in the atmosphere instead.

All it would take for the Makarieva Effect to work, would be for a rising moist air mass to be more diabatic than a dry air mass.

What can be said easily is that the dry case leads to a circulation with hot air rising and cold subsiding as long as cold means colder than the temperature that the hot air has when it has reached the top and cooled according to the dry adiabat.

Air containing water in vapour form will rise higher than dry air because it is lighter so when the vapour is removed it must fall back to its «correct» height but because of the air around it becoming warmer as it descends it will remain too dense for its height until it reaches the ground and receives more energy from the irradiated surfaAir containing water in vapour form will rise higher than dry air because it is lighter so when the vapour is removed it must fall back to its «correct» height but because of the air around it becoming warmer as it descends it will remain too dense for its height until it reaches the ground and receives more energy from the irradiated surfaair because it is lighter so when the vapour is removed it must fall back to its «correct» height but because of the air around it becoming warmer as it descends it will remain too dense for its height until it reaches the ground and receives more energy from the irradiated surfaair around it becoming warmer as it descends it will remain too dense for its height until it reaches the ground and receives more energy from the irradiated surface.

One interesting question is to what extent they fall in the rising column and to what extent the end up outside that in drier air where evaporation occurs rapidly and changes the properties of adjoining air.