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From: Dave Kruger <kdruger_at_pacifier.com>
subject: [Paddlewise] Effect of Barometric Pressure on Tide Height: Debunking the Myth
Date: Mon, 23 Dec 2002 17:56:59 -0800
A couple of folks have noted that during a storm (low atmospheric pressure)
that high tides run higher than normal -- the well-named "storm surge."
This surge can run several feet, as it has on many occasions on the Gulf
Coast.  Along with the huge waves generated by hurricane-force winds, the
storm surge causes massive damage to coastal areas.

Alas, it is not the direct effect of the low pressure that raises the height
of the tide by several feet.  Even in the center of the worst storms, when
the barometric pressure drops below 29 inches of mercury, the equivalent
rise in column of water is only a foot or so at the maximum  (density of
water is about 13.6 times smaller than that of mercury).  Normal sea level
air pressure is about 29.9 inches of mercury.  A low pressure of 28.5 inches
mercury (extremely low for the atmosphere at sea level -- about what you get
in the eye of a hurricane) only changes the tide height by 19 inches.

In short, it is a different effect, mainly the effect of the storm center's
winds, that pushes a bulge of sea water ashore along with the storm center.
Here is a pretty good description of the effect:
http://www.comet.ucar.edu/nsflab/web/hurricane/313.htm complete with
animation (takes a while to load).

Note that the highest levels of tide (worst storm surges) are to the right
of the eye of the hurricane (Northern hemisphere), and __not__ at the
location of lowest pressure.

On the coast of Oregon, storm surges are common, and run 1 to 2 feet.  When
the tide is at its monthly maximum, and a heavy rainfall is on us, the
combined effects near the mouths of rivers make for a lot of flooding in the
lowlands.

Just debunking the myth.

--
Dave Kruger
Astoria, OR

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From: Dave Gorjup <dgorjup_at_cox.net>
subject: Re: [Paddlewise] Effect of Barometric Pressure on Tide Height: Debunking the Myth
Date: Tue, 24 Dec 2002 00:03:03 -0500
I wasn't perpetuating a myth, just using a common natural event to 
illustrate a point. If you look at the bottom paragraph in the web page you 
cited you will see that low barometric pressure is an important component 
of storm surge. The first part seems to gloss over atmospheric pressure so 
if you don't read the whole page you miss a good bit.

In any event, the question was, does barometric pressure have an effect on 
sea state? The answer is yes, it does.

BTW, a standard day is defined as 29.92 inches at 70 degrees F. I'd like to 
see a more factual definition of the height of water rise in a low pressure 
center than a comparison of water vrs mercury density. There's a good bit 
more to it than that.

Regards,
Dave G.

At 05:56 PM 12/23/2002 -0800, Dave Kruger wrote:

>Just debunking the myth.
>
>--
>Dave Kruger
>Astoria, OR


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From: <djop_at_yahoo.com>
subject: Re: [Paddlewise] Effect of Barometric Pressure on Tide Height: Debunking the Myth
Date: Tue, 24 Dec 2002 12:11:31 -0800 (PST)
I must be missing part of the web page, for the three factors that appear to be cited are:
- winds.  
- waves, i.e perodic surface phenomena
- sea-level rise (ie. the overall mass of water displaced by the storm).
Am I correct that you ascribe #3 primarily to barometric pressure as opposed to an overall (DC component if you like) effect of surface wind on water?
What the material on the website  truly appears to say is that you can have storm surge without an explicit hurricane eye, and that the onset or maximum water level of storm surge need not coincide with an idealised center of the storm.
I offer for discussion  the example of the lagoon of Venice, where there are no hurricanes as such.   It sits at the north end of a narrow sea, at the silted-up mouth of a river, and storm winds tend to be southerly.    One sees flood-level tides almost reliably from October to April.
 Dave Gorjup <dgorjup_at_cox.net> wrote:I wasn't perpetuating a myth, just using a common natural event to 
illustrate a point. If you look at the bottom paragraph in the web page you 
cited you will see that low barometric pressure is an important component 
of storm surge. The first part seems to gloss over atmospheric pressure so 
if you don't read the whole page you miss a good bit.

In any event, the question was, does barometric pressure have an effect on 
sea state? The answer is yes, it does.

BTW, a standard day is defined as 29.92 inches at 70 degrees F. I'd like to 
see a more factual definition of the height of water rise in a low pressure 
center than a comparison of water vrs mercury density. There's a good bit 
more to it than that.

Regards,
Dave G.

At 05:56 PM 12/23/2002 -0800, Dave Kruger wrote:

>Just debunking the myth.
>
>--
>Dave Kruger
>Astoria, OR




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From: Dave Kruger <kdruger_at_pacifier.com>
subject: Re: [Paddlewise] Effect of Barometric Pressure on Tide Height: Debunking the Myth
Date: Fri, 27 Dec 2002 02:27:32 -0800
Dave Gorjup <dgorjup_at_cox.net> wrote:

>>I wasn't perpetuating a myth, just using a common natural event to
illustrate a point. If you look at the bottom paragraph in the web page you
cited you will see that low barometric pressure is an important component
of storm surge. The first part seems to gloss over atmospheric pressure so
if you don't read the whole page you miss a good bit.

In any event, the question was, does barometric pressure have an effect on
sea state? The answer is yes, it does.

BTW, a standard day is defined as 29.92 inches at 70 degrees F. I'd like to
see a more factual definition of the height of water rise in a low pressure
center than a comparison of water vrs mercury density. There's a good bit
more to it than that.>>

I should have been more explicit.  There is a very small rise in local sea
level in direct response to a drop in air pressure.  The density of water is
13.6 times smaller than that of mercury.  That makes it easy to calculate
what the rise will be:  a column of water that exerts the same pressure as
29.92 inches of mercury will be 13.6 times 29.92 inches (about 407 inches =
33.9 feet of water).  Consequently, if local air pressure __drops__ by an
inch of mercury, then the local sea level will rise by 13.6 inches of water.
That's the effect Dave and others described.  That's no myth.  It is,
however, very small, albeit enough to drown out your campfire if you have it
no higher than a foot or so above the surface of a large lake or sea.

The myth is that larger rises are directly due to the local air pressure.
Read that web site again and you'll find that it is the __wind-generated
waves__ associated with a storm center that cause the much larger (many
feet -- sometimes up to ten feet) rise called "storm surge."  And, that rise
is __not__ at the center of low pressure, it is off to the side.  In
addition, a big surge demands a specific type of local shore :  shallow
slope.  One could say that the low pressure caused the surge, but it's
really the effects of the storm.  Wind-generated waves from a distant source
can cause the same effect, so the local ari pressure can remain relatively
constant while a surge occurs.

Hope that sorts it out.

--
Dave Kruger
Astoria, OR

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From: Dave Gorjup <dgorjup_at_cox.net>
subject: Re: [Paddlewise] Effect of Barometric Pressure on Tide Height: Debunking the Myth
Date: Fri, 27 Dec 2002 10:55:04 -0500
This is my last post on this subject.

Some have said that talking about the low pressure effects on sea state are 
a myth and/or have minimal effect. An example of an approximately 13" rise 
in sea level for a one inch drop in mercury was given.

While barometric pressure is not the most significant component of storm 
surge, it is certainly worthy of consideration. If one takes into 
consideration the size of a storm low pressure system, which can be many 
hundreds, if not thousands of square miles, the amount of additional water 
weight and/or pressure added by that one foot addition of water, can add to 
the effect extensively.

Take it from me, as some one who lives about 4 feet above mean low water on 
the Chesapeake Bay, every inch makes a difference. When the ditch in the 
back yard is full of tide water, I know that we are in spring or fall neap 
tide and a nor'easter is brewing. ;-)
Dave G.
Poquoson, Va.

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From: ralph diaz <rdiaz_at_ix.netcom.com>
subject: Re: [Paddlewise] Effect of Barometric Pressure on Tide Height: Debunking the Myth
Date: Fri, 27 Dec 2002 12:09:40 -0500
----- Original Message -----
From: "Dave Gorjup" <dgorjup_at_cox.net>

> Some have said that talking about the low pressure effects on sea state
are
> a myth and/or have minimal effect. An example of an approximately 13" rise
> in sea level for a one inch drop in mercury was given.
>
> While barometric pressure is not the most significant component of storm
> surge, it is certainly worthy of consideration.

Since I started the whole thing about barometric pressure affecting the
height of tides, I think I should pipe in again.  Barometric pressure was
one of a number of influences on the height of tides that was included to be
complete in terms of how tide (and currents) prediction tables are almost
always going to be off in terms of heights (and speeds) and timing.  The
reason is that you cannot predict a year ahead of time variables such as
wind speed, wind direction, rainfall, snow meltoff, and barometric pressure.
Also unpredictable or constantly changing are manmade structures that can
affect currents and even tides.  For example, here on the Hudson, a number
of piers have been pulled out and this changes how water moves along the
river.  As for tides, in a narrow passage such as the Kill Van Kull that
leads to Newark Bay, dredging operations can improve flow of water and tides
but they can also hinder it while the dredging is being done as the barges
and apparatus used during the dredging impede passage of water.

ralph diaz

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From: Chuck Holst <cholst_at_bitstream.net>
subject: RE: [Paddlewise] Effect of Barometric Pressure on Tide Height: Debunking the Myth
Date: Thu, 26 Dec 2002 10:35:31 -0600
I once experienced a storm surge on Lake Superior. I was camped with 
friends on a low beach in a bay in Pukaskwa National Park when a rainstorm 
passed by the mouth of the bay. Suddenly the water rose several inches and 
swirled onto the beach, putting out the fire in the Coleman double-burner 
stove I was cooking dinner on. The water remained high several minutes, 
then slowly drained away. I always assumed that low pressure associated 
with the rainstorm caused the surge. An alternate explanation would be the 
wake from an ore or grain ship that was over the horizon. However, Pukaskwa 
is far from the shipping lanes, so that explanation seems unlikely.

Chuck Holst


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From: James <jimtibensky_at_fastmail.fm>
subject: RE: [Paddlewise] Effect of Barometric Pressure on Tide Height: Debunking the Myth
Date: Fri, 27 Dec 2002 12:32:43 -0500
Chuck Holst said:
> I once experienced a storm surge on Lake Superior. I was camped with friends on a low beach in a bay in Pukaskwa National Park when a rainstorm passed by the mouth of the bay. Suddenly the water rose several inches and swirled onto the beach, putting out the fire in the Coleman double-burner stove I was cooking dinner on. The water remained high several minutes, then slowly drained away. 

Chuck - You may have experienced a seiche.  These happen when the air
pressure is lower in one part of great lake than other.  It sets up
something that is usually described as being similar to water sloshing in
a bowl: it goes up on one side and down on the other, then switches. 
These are not all that rare on the Great Lakes.  I once almost got fired
from my lifeguard job at a beach in Chicago because the water had seiched
out and my boat was high and dry with about fifty yards of sand between
me and the water.  The captain's attitude was that I should have pushed
the thing out rather than tell the swimmers to stay out of the water.

Jim Tibensky
> 
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From: Richard Culpeper <culpeper_at_tbaytel.net>
subject: Re: [Paddlewise] Effect of Barometric Pressure on Tide Height: Debunking the Myth
Date: Thu, 26 Dec 2002 12:16:30 -0500
[Moderator's Note: Content unaltered. Excessive quoting (i.e.  headers/footers/sig lines/extraneous comments from previous posts, etc.) have been removed. Please edit quoted material in addition to removing header/trailers when replying to posts.]

Or water accumulation needing a few minutes to equalize.

Or wind blowing water toward shore delaying equalization.

Or combination thereof.

Check out the shallow beach in Terrace Bay for this sort of thing.

Chuck Holst wrote:

>I once experienced a storm surge on Lake Superior. I was camped with 
>friends on a low beach in a bay in Pukaskwa National Park when a rainstorm 
>passed by the mouth of the bay. Suddenly the water rose several inches and 
>swirled onto the beach, putting out the fire in the Coleman double-burner 
>stove I was cooking dinner on. The water remained high several minutes, 
>then slowly drained away. I always assumed that low pressure associated 
>with the rainstorm caused the surge. An alternate explanation would be the 
>wake from an ore or grain ship that was over the horizon. However, Pukaskwa 
>is far from the shipping lanes, so that explanation seems unlikely.
>
>Chuck Holst
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From: Chuck Holst <cholst_at_bitstream.net>
subject: RE: [Paddlewise] Effect of Barometric Pressure on Tide Height: Debunking the Myth
Date: Fri, 27 Dec 2002 22:36:36 -0600
>>
Chuck - You may have experienced a seiche.  These happen when the air
pressure is lower in one part of great lake than other.  It sets up
something that is usually described as being similar to water sloshing in
a bowl: it goes up on one side and down on the other, then switches.
These are not all that rare on the Great Lakes.
>>

I have experienced seiches on Lake Superior, but they were periodic and 
much slower. This was a one-time event, and very rapid compared to the 
seiches.

But this was not the only strange thing I have seen in Pukaskwa. On 
another, very still, day on the same trip we were paddling along the shore 
north of Michipicoten Island when I noticed tall clouds developing over 
Michipicoten and the mainland to the north. Gradually these clouds grew 
higher and higher, forming tall pillars. Finally they reached a thin layer 
of mackerel clouds, where the cloud pillars began to spread out fpr miles 
in all directions, a band of clear blue sky always separating them from the 
pre-existing layer of clouds. Ihad never seen this phenomenon before, and 
have never seen it since.

Chuck Holst


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From: Richard Culpeper <culpeper_at_tbaytel.net>
subject: Re: [Paddlewise] Effect of Barometric Pressure on Tide Height: Debunking the Myth
Date: Sat, 28 Dec 2002 11:46:46 -0500
Chuck Holst wrote:

>I noticed tall clouds developing over 
>Michipicoten and the mainland to the north. Gradually these clouds grew 
>higher and higher, forming tall pillars. Finally they reached a thin layer 
>of mackerel clouds, where the cloud pillars began to spread out fpr miles 
>in all directions, a band of clear blue sky always separating them from the 
>pre-existing layer of clouds.
>
Probably the result of poutine based flatulence by people having eaten 
at the White River chip stand.

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