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From: Chris Luginbuhl (cbl_at_hidden_email_address.net)
Date: 06/21/1995



Dear Brian et al.,

It seems reasonable that the built urban environment would have an enhanced
interaction with the low-frequency component of thunder. Taking the speed of sound to be about 350 m/s, the approximate wavelength of various sound frequencies is:

            400 Hz     1  m
             40        9  m
             20       17  m
             10       35  m

It seems clear that these lower frequencies (below 50 Hz or so) begin to have wavelengths comparable to building sizes and separations. In some cases, for some locations and some restricted frequencies this might lead to resonant enhancement (through constructive interference), but I would guess that more often these low frequencies would be largely damped by the surrounding structures and spaces.

In any case, though I am unable to give a rigorous discussion in this regard, at least from this argument we should not be surprised that there is
something special going on at these lower frequencies in urban environments.
Perhaps someone else can give a more rigorous discussion and better insight.

Thunder with a french accent? Perhaps if the barrels were made of wood...

  • Thunder effects on precipitation -----------------

I note Brian's comment regarding the sudden change in precipitation intensity associated with nearby strikes/thunder claps. I also have noticed
this, I think, and am curious to know 1) if anyone has ever tried to verify this phenomenon (i.e. show that it is a real effect, not just the effect of "selective memory" where we note and remember the cases where the
rain increases just after a strike, but do not note or forget the cases where it doesn't), and 2) if anyone has found a reason for the effect, or has
themselves an idea about it. Can an intense sonic field passing though rain-filled air cause water drops to coalesce? Is is possible for the pressure fluctuations to condense more water drops out of the saturated air
and grow the droplets large enough to perceptibly affect the precipitation in a fwe seconds?

Certainly, if real, the effect must be quite local and very fast - there is
no time for drops formed high in the air to change the precipitation intensity near the observer in such close temporal proximity to the thunder...

To begin with, of course, and to reiterate, it would be smart and it would seem fairly simple to verify the effect by measurement. There is not much point in fantasizing explanations for hypothetical phenomena...

Chris Luginbuhl
U.S. Naval Observatory Flagstaff Station Flagstaff AZ
cluginbuhl_at_nofs.navy.mil