Joe Fischer
2005-09-21 17:06:25 UTC
There seems to be a serious lack of understanding by
TV personalities about how a tropical cyclone gets it's energy, how
that effects the water temperature, and how that energy translates
into lower atmospheric pressure, higher winds, etc.
First, the wind of the cyclonic causes evaporation
of the water at the surface by at least two processes, it carries
away the air with equalized "vapor pressure", and the difference
in temperature of the warm water and the cooler storm air temperatures
increases evaporation.
Evaporation is the mechanism for the removal of
energy from the water surface and transportation to the atmosphere.
FOR EACH POUND OF WATER EVAPORATED
FROM THE SURFACE, ABOUT 1,000 BTU OF HEAT ENERGY
IS CARRIED INTO THE ATMOSPHERE.
It only takes evaporation of 100 pounds of water;
per hour, to equal the output of a home furnace
Next, humid air has a lower specific gravity than
dry air, so it exerts less pressure dur to gravity (gravity is the
power that creates atmospheric pressure, without gravity the
air would escape into space).
The lower localized atmospheric pressure causes
surrounding higher pressure air to move toward the center of
the lower pressure area, and the rotation of the Earth causes
the motion toward the center to translate to a rotation, the direction
of the rotation depending on the hemisphere, North or South.
This is a simplistic description of how the energy
gets into the storm and how it gets organized.
The conversion of this humid air to heat released
into the upper airr can only take place with condensation,
and the accompaning precipitation (meteorologists have
developed a more complicated description of water vapor,
clouds, and the production of rain, sleet, hail and snow).
A factor not fully appreciated is that the
precipitation reduces local atomspheric pressure by the
conversion of a larger volume of water vapor into a smaller
volume of condensed water!!!!!!
This is part of the process of the extreme lowering
of atmospheric pressure in the center of the cyclonic, or rather
in the area of the greatest precipitation rate.
Tropical cyclonics probably do not produce much
hail, where tornados do produce a substantial amount of hail,
resulting in a much greater rate of transfer of energy, and the
resulting higher wind speeds.
But the massive amounts of precipation over large
areas in a tropical cyclonic can reduce the atmospheric pressure
over a large area substantially, primarily by the reduction of
volume of the water that is airborn, in addition to the lesser
specific gravity of the humid air before precipitation.
And another mechanism contributes to the volume
of humid air water vapor precipation.
The condensation-precipitation releases the 1,000
BTU per pound back into the surrounding air, causing it to
move upward due to bouyancy, and as surrounding humid
air is carried upward, it interacts with colder air and colder
falling rain, accelerating the condensation-precipation.
All these processes, working together, cool the
water surface, create high rotational winds, great amounts
of precipation, and heating of the upper atmosphere.
Joe Fischer
TV personalities about how a tropical cyclone gets it's energy, how
that effects the water temperature, and how that energy translates
into lower atmospheric pressure, higher winds, etc.
First, the wind of the cyclonic causes evaporation
of the water at the surface by at least two processes, it carries
away the air with equalized "vapor pressure", and the difference
in temperature of the warm water and the cooler storm air temperatures
increases evaporation.
Evaporation is the mechanism for the removal of
energy from the water surface and transportation to the atmosphere.
FOR EACH POUND OF WATER EVAPORATED
FROM THE SURFACE, ABOUT 1,000 BTU OF HEAT ENERGY
IS CARRIED INTO THE ATMOSPHERE.
It only takes evaporation of 100 pounds of water;
per hour, to equal the output of a home furnace
Next, humid air has a lower specific gravity than
dry air, so it exerts less pressure dur to gravity (gravity is the
power that creates atmospheric pressure, without gravity the
air would escape into space).
The lower localized atmospheric pressure causes
surrounding higher pressure air to move toward the center of
the lower pressure area, and the rotation of the Earth causes
the motion toward the center to translate to a rotation, the direction
of the rotation depending on the hemisphere, North or South.
This is a simplistic description of how the energy
gets into the storm and how it gets organized.
The conversion of this humid air to heat released
into the upper airr can only take place with condensation,
and the accompaning precipitation (meteorologists have
developed a more complicated description of water vapor,
clouds, and the production of rain, sleet, hail and snow).
A factor not fully appreciated is that the
precipitation reduces local atomspheric pressure by the
conversion of a larger volume of water vapor into a smaller
volume of condensed water!!!!!!
This is part of the process of the extreme lowering
of atmospheric pressure in the center of the cyclonic, or rather
in the area of the greatest precipitation rate.
Tropical cyclonics probably do not produce much
hail, where tornados do produce a substantial amount of hail,
resulting in a much greater rate of transfer of energy, and the
resulting higher wind speeds.
But the massive amounts of precipation over large
areas in a tropical cyclonic can reduce the atmospheric pressure
over a large area substantially, primarily by the reduction of
volume of the water that is airborn, in addition to the lesser
specific gravity of the humid air before precipitation.
And another mechanism contributes to the volume
of humid air water vapor precipation.
The condensation-precipitation releases the 1,000
BTU per pound back into the surrounding air, causing it to
move upward due to bouyancy, and as surrounding humid
air is carried upward, it interacts with colder air and colder
falling rain, accelerating the condensation-precipation.
All these processes, working together, cool the
water surface, create high rotational winds, great amounts
of precipation, and heating of the upper atmosphere.
Joe Fischer