And white roofs can reduce precipitation as well, by reducing the amount of warm,
humid air rising and, thus, the number of clouds and eventual rainfall.
The warm water evaporates from the ocean surface, and the light, warm and
humid air rises, leading to deep convection in the form of towering cumulonimbus clouds and heavy precipitation.
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!
That is thanks to a fortunate natural thermostat: when
humid air gets hot, it
rises and causes storms that cool things down.
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.
Strangely, the
air also tends to be at its most
humid around April 1st, when the relative humidity
rises above 83 % (
humid) three days out of four.
On the other hand, June 21st is when the
air is at its most
humid, when relative humidity levels
rise above 92 % three days out of every four.
On the other hand, the
air is at its most
humid on March 17th, when the humidity tends to
rise above 84 % three days in 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.
The
air is at its most
humid around December 19th, when it
rises above 79 % (
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».
Since water vapor is lighter than the main constituents of
air,
air containing water vapor is lighter and so
rises above less
humid air.
I would expect a temperature
rise that increased evaporation would, once equilibrium was reached, cause * all * the
air to become more
humid.
As the
air rises, it expands and cools, and water vapour condenses, releasing even more heat,» much like how a hurricane frees energy by drawing warm
humid air from its base (usually tropical sea water) and then releasing cold, wet
air 7 miles (12 kilometers) up in the troposphere.
The warm,
rising air enhances the seasonal northward flow of
humid monsoon winds, forcing moisture and hot
air up the slopes of the Himalayas.
As the sun heats the
humid air, pillars of black smoke begin to
rise above the vast Agbogbloshie Market.
«This H2O negative - feedback effect on CO2 is ignored in models that assume that warm moist
air does not
rise and form sunlight - reflecting clouds, but remains as
humid air near sea level, absorbing infrared radiation from the sun, and approximately doubling the temperature
rises predicted from atmospheric CO2 increases.
This
rising air is replaced by more warm,
humid air from the ocean below.
Shown here, notice how the
humid air above the place where the ice is melting causes the formation of clouds, which
rise up onto the main portion of the land due to convection.