Hi Jim, Thanks for this information. I have one Lehman N/S and one =
E/W, and their performance agrees with your findings. There may be =
differences due to orientation, but I do not see them.
Ted
----- Original Message -----=20
From: Connie & Jim Lehman=20
To: psn-l@.................
Sent: Friday, May 30, 2008 11:25 AM
Subject: Directional characteristics of a "lehman type" sensor-
PSN friends--I have noted several references to directional =
performance on a typical 15-20 sec "Lehman" design. It was our =
observation that very few quakes were blocked out due to orientation. =
One summer when mictoseisms are lowest (here in Virginia) we ran two =
systems with booms at right angles, N-S & E-W. We copied 66 events in =
two months. There were signatures in both orientations--(excepting for =
a half-dozen small events) and we noted the predictable comparisons with =
incoming P,S, & L wave fronts. P waves show strong coming in broadside. =
S waves show strongest coming in off the end. Likewise the Surface =
waves -S show a distinctive difference whether they be Love waves or =
Raleigh. You simply cannot hide from a readable event due to =
orientation.
This test was made with systems having no filtering excepting to =
remove mechanical room noise typical in a building, and 60 hz AC. We =
were satisfied the generalizations above were verified, as we copied =
several events (Alaskan or thereabouts--coming into our booms at 45 =
degrees) which appeared identical on our n-s,e-w readouts. Running two =
long period systems is a luxury now, but in earlier days of the big =
bulky worldwide sensors, dual copy was standard--with few stations to =
get a tag on direction of event.
Here in VA. we usually ran our system broadside a few degrees off =
E-W to accent the events of South Pacific, but any South American events =
of size would boom right in with lower P waves and heavy S wave =
signatures.
Another side effect of noting amplitude of S or surface wave =
arrivals--one can tell whether the event has a shallow focus--less than =
30 km, or a deep focus of several hundred km--even before you are told!!
I hope this is informative. Jim Lehman
Hi Jim, Thanks for this=20
information. I have one Lehman N/S and one E/W, and their=20
performance agrees with your findings. There may be =
differences due=20
to orientation, but I do not see them.
Ted
----- Original Message -----
From:=20
Connie &=20
Jim Lehman
Sent: Friday, May 30, 2008 =
11:25 AM
Subject: Directional =
characteristics of a=20
"lehman type" sensor-
PSN friends--I have noted several =
references to=20
directional performance on a typical 15-20 sec "Lehman" design. =
It was=20
our observation that very few quakes were blocked out due to=20
orientation. One summer when mictoseisms are lowest (here in =
Virginia)=20
we ran two systems with booms at right angles, N-S & E-W. We =
copied=20
66 events in two months. There were signatures in both=20
orientations--(excepting for a half-dozen small events) and we =
noted the=20
predictable comparisons with incoming P,S, & L wave fronts. =
P=20
waves show strong coming in broadside. S waves show =
strongest=20
coming in off the end. Likewise the Surface waves -S show=20
a distinctive difference whether they be Love waves or =
Raleigh. You=20
simply cannot hide from a readable event due to =
orientation.
This test was made with =
systems=20
having no filtering excepting to remove mechanical room noise =
typical in=20
a building, and 60 hz AC. We were satisfied the generalizations =
above=20
were verified, as we copied several events (Alaskan or =
thereabouts--coming=20
into our booms at 45 degrees) which appeared identical on our n-s,e-w=20
readouts. Running two long period systems is a luxury now, but =
in=20
earlier days of the big bulky worldwide sensors, dual copy was=20
standard--with few stations to get a tag on direction of =
event.
Here in VA. we usually ran our =
system=20
broadside a few degrees off E-W to accent the events of South Pacific, =
but any=20
South American events of size would boom right in with lower P waves =
and heavy=20
S wave signatures.
Another side effect of =
noting=20
amplitude of S or surface wave arrivals--one can tell whether the =
event has a=20
shallow focus--less than 30 km, or a deep focus of several hundred =
km--even=20
before you are told!!
I hope this is =
informative. =20
Jim Lehman
=20