Walter & Group...
From Jerry Puckett :
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Gordy,
Just thinking now without any scientific evidence--greater lift in
dry air, less lift in humid air.
Does the fly line generate lift when casting? I am able to
throw a side arm cast and watch the loop rise as the cast lengthens.
In 1978 I observe an altimeter setting of 26.81 flying in Hurricane
Federick and remember a high setting on a clear cold Autumn day
of 30.21--thus a great disparity exist in air pressure depending on
weather conditions.
As for fog there are several types and by definition fog is a cloud
that begins within 50 feet of the surface and is formed when the air is
saturated with moisture and can longer hold condensation nuclei. Fog
is classified in the manner in which it is formed
If you are interested I will will relay info from the "FAA handbook
of Aeronautical Knowledge" regarding radiation fog, advection
fog, up-slope fog, and steam fog.
As far as the fly line traveling less on high humid days verse dry
day I remain in the fog but I am thinking on this!
Jerry Puckett
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Jerry....
I'd be interested in what you find out re
fog.
In the past, I was skeptical of claims
that a traveling fly line loop can have "lift". Then I started
noting some evidence that this can occur. I really couldn't tell
while observing my own casts, but I have seen what may be true lift as I
watched others cast. Some have called this the CLIMBING
LOOP.
Perhaps others in our Group have more
information about this.
Gordy
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Jerry followed up with more detailed
info. on fog. I placed in in the second & third
attachments. G.
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HUMIDITY
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From Ralph Tomacio:
Hi Gordy,
You said: “Now I'm guessing. Fact IS that I can't reach my max distances when casting here in the tropics at sea level on days when the humidity is high. This might be due to an effect upon the fly line (???) and not have anything to do with the air density. Someday I'll have the answer!”
Have you ever factored in that we, as people who are not infallable and sometimes inconsistent, may not be casting as efficiently as when it’s not humid? I know that when it’s too humid and I’m not the least bit comfortable, I don’t perform anywhere near how I do when conditions are comfortable. When and how much do we factor in the human element and it’s inconsistencies when comparing conditions as described above? Maybe someone who tolerates humidity well wouldn’t notice any difference in their casting. Whereas, for another, that effect on the fly line may not have anything to do with the air density but, rather, with the caster.
This is just a WAG on my part and I may be way off base. If so, please disregard my response altogether. Just trying to get into the nitty-gritty of the science behind casting.
Ralph Tomaccio ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ Ralph .... You may be right about that ! Gordy ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
Aerial ments .... Quiz
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Gary Davison has sent another set of good
answers. I placed it in an attachment.
G.
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From: Gary
[GulfCoastSpey@xxxxxxxxxx] Sent: Sunday, April 26, 2009 5:48 PM To: Gordy Hill Subject: Re: SLP- Loop / Practicing aerial mends
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Fog, by definition, is a cloud that begins within 50 feet of the
surface. It typically occurs when the temperature of air near the
ground is cooled to the air's dewpoint. At this point, water vapor
in the air condenses and becomes visible in the form of fog. Fog is
classified according to the manner in which it forms and is dependent upon
current temperature and the amount of water vapor in the air.
On clear nights, with relatively little to no wind present,
radiation fog may develop. Usually, it forms in low -lying areas
like mountain valleys. This type of fog occurs when the ground cools
rapidly due to terrestrial radiation, and the surrounding air
temperature reaches its dewpoint. As the sun
rises and the temperature increases, if radiation fog is less than 20 feet
thick, it is known as ground fog.
When a layer of warm, moist air moves over a cold surface,
advection fog is likely to occur. Unlike radiation fog, wind
is required to form advection fog. Winds of up to 15 knots
allow the fog to form and intensify; above a speed of 15 knots, the
fog usually lifts and forms low stratus clouds. Advection fog is
common in coastal areas where sea breezes can blow the air over cooler
landmasses.
In the same coastal areas upslope fog is likely as
well. Upslope fog occurs when moist, stable air is forced up sloping
land features like a mountain range. This type fog also requires
wind for formation and continued existence. Upslope and advection,
unlike radiation fog, may not burn off with the morning sun, but can
persist for days. They can also extend to greater heights than
radiation fog.
Steam fog, or sea smoke, forms when cold, dry air moves over
warm water.
as the water evaporates, it rises and resembles smoke. This
type of fog is common over bodies of water during the coldest times of the
year. Low-level turbulence and icing are commonly associated
with steam fog.
Ice fog occurs in cold weather when the temperature is much
below freezing and water vapor forms directly into ice
crystals. Conditions favorable for its formation are the same as for
radiation fog except for cold temperature, -25 degrees F or colder.
It occurs mostly in the arctic regions during the cold season.
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One more point on radiation fog, as the sun rises, and the
temperature increases. radiation fog will will lift and eventually burn
off. Any increase in wind will also speed the dissipation of
radiation fog.
During the sixties I would fly up the intercoastal
waterway at Cape Kennedy and wait for the moon shots as the fog lifted and
dissipated.. Awesome orange glow in the fog as the rockets
motors ignited.. I was at 1O,500 feet, by the time the rocket pass my
altitude at about three miles distance it had reached bullet speed.
Also have landed at Miami International airport at 12 pm and rolled
into advection fog half way down the runway into zero visibility.
Took a slow forever taxi to reach the terminal!
I think there is one more type of fog called affection fog that forms
in the brain when two teenagers fall in
love! |