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March 1st 06, 05:58 PM
HI,

Where does a pilot use the dew-point? Why is the volmet transmiting
this info?

Thanks
frank

Peter R.
March 1st 06, 06:06 PM
> wrote:

> Where does a pilot use the dew-point?

A close temperature/dewpoint spread (less than 5 degree Celsius difference
between the two) can indicate the presence or possibility of fog.

--
Peter

March 1st 06, 06:19 PM
Thanks
joe

Jose
March 1st 06, 06:22 PM
> A close temperature/dewpoint spread (less than 5 degree Celsius difference
> between the two) can indicate the presence or possibility of fog.

Also, knowing the temperature and dew point one can estimate the cloud
bases (using a standard lapse rate of 2 deg/1000 feet).

Jose
--
Money: what you need when you run out of brains.
for Email, make the obvious change in the address.

Tauno Voipio
March 1st 06, 07:07 PM
wrote:
> HI,
>
> Where does a pilot use the dew-point? Why is the volmet transmiting
> this info?


A rule of thumb for the base of convection clouds
is 400 feet / degree C of temperature - dewpoint
difference.

--

Tauno Voipio
tauno voipio (at) iki fi

Larry Dighera
March 1st 06, 07:21 PM
On Wed, 01 Mar 2006 18:22:11 GMT, Jose >
wrote in >::

>> A close temperature/dewpoint spread (less than 5 degree Celsius difference
>> between the two) can indicate the presence or possibility of fog.
>
>Also, knowing the temperature and dew point one can estimate the cloud
>bases (using a standard lapse rate of 2 deg/1000 feet).

The Relative Humidity, of which due point and temperature are an
indicator, is useful in predicting induction system icing in
carbureted engines.


http://www.lycoming.textron.com/main.jsp?bodyPage=/support/publications/keyReprints/operation/inductionIcing.html
Every pilot who flies an aircraft powered by a carbureted engine
should be thoroughly educated about carburetor ice. They should
know that under moist conditions (a relative humidity of 50% to
60% is moist enough), carburetor ice can form with any outside air
temperature from 20o to 90oF. It is most likely in the 30o to 60oF
range. Temperatures in the carburetor can drop 60o to 70oF
(refrigerator effect) as a result of fuel vaporization and the
carburetor venturi effect. It also happens that carburetor ice
forms more readily when the engine is operated in the lower power
range. It will form while taxiing and this makes it very important
to check engine power before takeoff and to remove the ice if
necessary. Care should be taken to avoid dusty or dirty conditions
when utilizing carburetor heat on the ground.

Peter R.
March 1st 06, 08:25 PM
Morgans > wrote:

> A close spread like stated above could also mean that carb ice will form
> more easily.

Thanks, Jim.

Not having flown a carburetor-equipped aircraft since 1990 and considering
the fuel-injected BE35 I now own, I certainly overlooked the issue of carb
ice.



--
Peter

Mortimer Schnerd, RN
March 1st 06, 08:43 PM
Morgans wrote:
>> A close temperature/dewpoint spread (less than 5 degree Celsius difference
>> between the two) can indicate the presence or possibility of fog.
>
> A close spread like stated above could also mean that carb ice will form
> more easily.


The same 2-3 degree difference between dewpoint and temperature may make the
difference in deciding to go or not. If it occurs as the sun is rising, going
is probably safe as the temperature is going to rise, widening the spread.
Conversely, if the sun is going down, it's a pretty good chance fog is going to
get you if you decide to fly.



--
Mortimer Schnerd, RN


Robert M. Gary
March 1st 06, 08:53 PM
Live for one winter in Sacramento and you won't ask that question. Near
sunrise most pilot have ATIS continuously tuned monitoring the dew
point second by second. If the spread is right, the moment the first
bit of sun touches the earth the fog forms, sometimes going from CAVU
to 1/2 vis in just minutes.

-Robert

Morgans
March 1st 06, 09:10 PM
"Peter R." > wrote in message
...
> > wrote:
>
> > Where does a pilot use the dew-point?
>
> A close temperature/dewpoint spread (less than 5 degree Celsius difference
> between the two) can indicate the presence or possibility of fog.

A close spread like stated above could also mean that carb ice will form
more easily.
--
Jim in NC

Jim Macklin
March 1st 06, 09:20 PM
A dew point above about 50 F indicates that storms are
possible and above 60 F that sever storms are likely due the
available supply of latent heat.
A close spread indicates that fog is possible, also a dew
point around 60 with a air temp of 90 is a good indicator of
carb ice conditions.



--
James H. Macklin
ATP,CFI,A&P

--
The people think the Constitution protects their rights;
But government sees it as an obstacle to be overcome.
some support
http://www.usdoj.gov/olc/secondamendment2.htm
See http://www.fija.org/ more about your rights and duties.


"Peter R." > wrote in message
...
| > wrote:
|
| > Where does a pilot use the dew-point?
|
| A close temperature/dewpoint spread (less than 5 degree
Celsius difference
| between the two) can indicate the presence or possibility
of fog.
|
| --
| Peter

Steve Foley
March 1st 06, 09:27 PM
Why does sun touching the earth form fog? I've seen it happen, but I've
never understood why.
"Robert M. Gary" > wrote in message
ups.com...
> Live for one winter in Sacramento and you won't ask that question. Near
> sunrise most pilot have ATIS continuously tuned monitoring the dew
> point second by second. If the spread is right, the moment the first
> bit of sun touches the earth the fog forms, sometimes going from CAVU
> to 1/2 vis in just minutes.
>
> -Robert
>

Robert M. Gary
March 1st 06, 10:11 PM
> Why does sun touching the earth form fog? I've seen it happen, but I've
> never understood why.

I"m sure if I get this wrong someone on the list will correct me. In
Sacramento we receive two types of fog...
1) Advection Fog. This gets blown up from the Bay Area and usually
forms late at night and will often stay around until mid-day.
2) Radition Fog. This is the stuff that forms out of the blue. I
believe what happens is that the ground is already very moist but the
moisture is held in the ground. Once the sun hits it the water on the
ground warms releasing the moisture into the cool calm air. Sometimes
you'll drive by a field and see the field totally engulfed in fog while
the road you are on is clear. Unfortunately airports seem to be
composed of a lot of grass and dirt areas. Perhaps if you paved the
entire airport boundry you'd have less fog. I know some airports have
used helicopter to just fly around and blow the fog around.This fog
forms very, very fast at dawn. However, I've never been able to predict
it. Sometimes given the same temp/dew points and winds fog will form,
other times it will not. I'm not sure what all the factors are.

Jim Macklin
March 1st 06, 11:42 PM
It causes some vertical motion which stirs the air a little,
casing the fog to form.



"Steve Foley" > wrote in message
news:EkoNf.1255$v34.1168@trndny02...
| Why does sun touching the earth form fog? I've seen it
happen, but I've
| never understood why.
| "Robert M. Gary" > wrote in message
|
ups.com...
| > Live for one winter in Sacramento and you won't ask that
question. Near
| > sunrise most pilot have ATIS continuously tuned
monitoring the dew
| > point second by second. If the spread is right, the
moment the first
| > bit of sun touches the earth the fog forms, sometimes
going from CAVU
| > to 1/2 vis in just minutes.
| >
| > -Robert
| >
|
|

Icebound
March 2nd 06, 04:08 PM
"Jim Macklin" > wrote in message
news:%mqNf.107786$QW2.7653@dukeread08...
> It causes some vertical motion which stirs the air a little,
> casing the fog to form.
>
>
>


Yes!

The very coldest air at that time of morning is right at the surface of the
earth. As it starts to mix with air above it, it cools a whole layer of 50
or a hundred feet or so, instead of just the thin surface layer. If the
average moisture content through that layer is such that the cooling drops
the temperature down to the average dew-point, bingo.

If you watch weather reports carefully, you will find that in those
clear-morning situations, the lowest temperature occurs *after* sunrise,
when you would have expected that warming is started. But when this mixing
starts, that coldest air at the surface (as part of the slight turbulence)
reaches up to the 1 metre level where the "official" thermometers are kept.

If you check a weather observing site which observes "grass" temperatures,
such as an experimental farm or the like, you will see just how great this
temperature difference between the grass level and the official 1 meter
level can be at sunrise... exceeding 5 degrees Celsius in clear-sky cases.

Jim Macklin
March 2nd 06, 06:37 PM
That is also why it takes just a slight breeze to get thick
fog. No wind at all, no fog, stronger winds push the cloud
bases up a few hundred feet and IFR becomes possible when
ILS minimums are reached.


--
James H. Macklin
ATP,CFI,A&P

--
The people think the Constitution protects their rights;
But government sees it as an obstacle to be overcome.
some support
http://www.usdoj.gov/olc/secondamendment2.htm
See http://www.fija.org/ more about your rights and duties.


"Icebound" > wrote in
message ...
|
| "Jim Macklin" > wrote
in message
| news:%mqNf.107786$QW2.7653@dukeread08...
| > It causes some vertical motion which stirs the air a
little,
| > casing the fog to form.
| >
| >
| >
|
|
| Yes!
|
| The very coldest air at that time of morning is right at
the surface of the
| earth. As it starts to mix with air above it, it cools a
whole layer of 50
| or a hundred feet or so, instead of just the thin surface
layer. If the
| average moisture content through that layer is such that
the cooling drops
| the temperature down to the average dew-point, bingo.
|
| If you watch weather reports carefully, you will find that
in those
| clear-morning situations, the lowest temperature occurs
*after* sunrise,
| when you would have expected that warming is started. But
when this mixing
| starts, that coldest air at the surface (as part of the
slight turbulence)
| reaches up to the 1 metre level where the "official"
thermometers are kept.
|
| If you check a weather observing site which observes
"grass" temperatures,
| such as an experimental farm or the like, you will see
just how great this
| temperature difference between the grass level and the
official 1 meter
| level can be at sunrise... exceeding 5 degrees Celsius in
clear-sky cases.
|
|
|
|
|
|
|
|
|

Jim Macklin
March 2nd 06, 06:40 PM
On a clear night, the ground cools by radiation (IR) and the
air is cooled by conduction to the ground. Inversions are
common. If there is an overcast, the IR cooling doesn't
happen and the temperature will not drop as far.


--
James H. Macklin
ATP,CFI,A&P

--
The people think the Constitution protects their rights;
But government sees it as an obstacle to be overcome.
some support
http://www.usdoj.gov/olc/secondamendment2.htm
See http://www.fija.org/ more about your rights and duties.


"Robert M. Gary" > wrote in message
oups.com...
| When I flew the J-3 in Sacramento I would often take off
in the butt
| cold morning only to find it quite warm at altitude of 500
feet.
|
| -Robert
|

Peter R.
March 2nd 06, 06:51 PM
Jim Macklin > wrote:

> On a clear night, the ground cools by radiation (IR) and the
> air is cooled by conduction to the ground. Inversions are
> common.

Late one very clear night last year, I was flying back to Syracuse, NY, and
the temperature at 10,000 feet was around -5 Celsius.

As I started to descend for the approach, the cabin of the aircraft got
noticeably colder (I didn't have the heat on). When I retrieved the ATIS
for the airport, the temperature on the ground was a -25 Celsius. This
was one of the more extreme examples of an inversion I have experienced.


--
Peter

Jose
March 2nd 06, 07:14 PM
> I think you mean.... "using the rule of thumb that the height (in feet) of
> the bases of convective cloud is approximately 400 times the
> temperature-dewpoint spread at the surface (in degrees Celsius)"

Yes, that's it... not so much the lapse rate as the conversion rate.

Jose
--
Money: what you need when you run out of brains.
for Email, make the obvious change in the address.

Jose
March 2nd 06, 07:40 PM
> conversion rate.
convergence rate.

Jose
--
Money: what you need when you run out of brains.
for Email, make the obvious change in the address.

Mortimer Schnerd, RN
March 3rd 06, 01:52 AM
Peter R. wrote:
> Late one very clear night last year, I was flying back to Syracuse, NY, and
> the temperature at 10,000 feet was around -5 Celsius.
>
> As I started to descend for the approach, the cabin of the aircraft got
> noticeably colder (I didn't have the heat on).


Why? CO leak? Or are you just a polar bear?


--
Mortimer Schnerd, RN


Private
March 5th 06, 03:21 AM
> wrote in message
oups.com...
> HI,
>
> Where does a pilot use the dew-point? Why is the volmet transmiting
> this info?
>
> Thanks
> frank
>

The dew point is also used to forecast the expected overnight low
temperature. This will be used most by pilots who may be concerned about
their gardens and whether they need to be covered to protect from frost.

Happy landings,

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