Re: [time-nuts] OT: NZ Christchurch member

2011-02-25 Thread Brooke Clarke

Hi:

The Richter method of analyzing earthquakes is based on what can be 
learned from a simple seismometer.  For example by looking at the time 
difference between the P wave and the main shaking you can determine how 
far away the epicenter is located.  The Richter number depends on the 
peak of the main shaking.  But the energy depends on the integral of the 
magnitude of the shaking over the time it lasts.  The damage is 
proportional to the total energy not it's peak.  The public is used to 
hearing the Richter number even though it does not really describe the 
damage level.


For example I had just left work when the Loma Prieta quake happened and 
was standing in front of the building watching the wall sized windows 
oil canning.  With each cycle the window displacement was getting 
larger.  If the quake had lasted about 30 second longer all the windows 
would have exploded, either with glass going into the building or coming 
at those of us standing in in front.  We started to get on the ground to 
get some protection, but then the quake stopped.


http://www.prc68.com/I/Seismometer.shtml

Have Fun,

Brooke Clarke
http://www.PRC68.com


William H. Fite wrote:

For meteorologists and geologists, the Richter scale has a carefully defined
meaning and is used only for purposes where that definition fits.

This per a friend of mine who does seismic stuff for NOAA:
Him:  The Richter number means something very specific to us and something
quite different to the media.  Actually, the Richter doesn't have a great
deal of analytical value to us.  You can say, this is a Category Four
hurricane but that really tells you very little about what is going on in
the storm.  Richter is like that.
Me:  You're saying that the Richter is a poor predictor of surface
disruption?
Him:  Well, obviously a 9 will be expected to do much more damage than a 6
but it is at best a very rough indicator.  The location of the epicenter and
a dozen other factors play into it.
Me:  So how do you assess the damage potential?
Him:  Lots of people think we still rely mainly on the old
pendulum-and-stylus seismographs from the 1930s.  Actually, we take a great
many measurements in addition to seismometry.  But when it comes to
assessing the damage, we go outside and look, just like the TV stations do.

And his final comment:  By the way, did you know that when the shuttle
launches we capture that on virtually every strain guage seismometer in the
country?

I found that interesting.



On Thu, Feb 24, 2011 at 10:56 PM, jimlux  wrote:

   

On 2/24/11 5:23 PM, Bob Bownes wrote:

 

What is the conversion factor for Richter to dBm? :)

Bob
As a guy with degrees in geology and EE. I really should know this...:)



   

Especially since both are log scales..

The problem is that Richter is log magnitude displacement on a particular
kind of seismometer (which is sort of a low pass filter) and dBm is log
power.  However, there should be some sort of scale factor that converts it.

I think it's energy goes as amplitude^1.5.  there's also a scale factor for
how far the seismograph is from the epicenter.


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Re: [time-nuts] OT: NZ Christchurch member

2011-02-25 Thread Bob Bownes
The last 'modern' seismometers I worked with  (as an undergrad in the
early 80's) were all three axis laser interferometry based. I'm sure
they've gotten a bit better since then.

Not only could we pick up a shuttle launch from 1,400 miles away, we
could pick up frat parties from across town on the old strain gauge
monster at the top of the hill. :)

It was one of my first exposures to filtering actually.

As your friend said, 'Richter' is not actually used by seismologists
anymore, they use the moment magnitude scale for larger quakes, which,
while similar, is different. It's more about energy released than
about motion.

Back to your regularly scheduled discussion.

Bob


On Fri, Feb 25, 2011 at 11:09 AM, jimlux  wrote:
> On 2/25/11 7:55 AM, Poul-Henning Kamp wrote:
>>
>> In message,
>> "Wil
>> liam H. Fite" writes:
>>
>>> Me:  You're saying that the Richter is a poor predictor of surface
>>> disruption?
>>
>> For damage assement you really need a vector-version of richter,
>> vertical does a lot more damage than horizontal on average.
>>
>
>
> Yes.. I doubt anyone still uses the torsion seismometer Richter used,
> although more modern scales (moment magnitude, etc.) still relate back (e.g.
> they set the calibration to match for some notional set of events)..
>
> That way, people have an idea... A Magnitude 3 earthquake within a few tens
> of km of me will be noticeable, if it's quiet. A magnitude 4 will be very
> noticeable, and a 5 will be exciting. A 6 will wake you up in the middle of
> the night.  I'd compare it to something like Mohs hardness, except actually
> with a quantitative basis.  (People who work with material properties like
> hardness use other scales anyway)
>
> It's a "roughly quantitative" measure of energy release, in the same sense
> that kilotons are for explosions. It's like that whole "cup of gasoline:
> dynamite" comparison.. it's the rate of energy (e.g. power) that creates the
> qualitative difference between running my camping stove and blasting.
>
> We do the same thing in time-nuttery.. we use log scales to talk about
> performance.. dBc/Hz for phase noise, and really, just the exponent to talk
> about ADEV.  (nobody gets excited about the difference between 1.1E-13 and
> 1.5E-13... but the difference between 1E-11 and 1E-15 is worth talking
> about)
>
> Maybe we should start promulgating dBallan?
>
> And maybe get an SI unit... The "Allan", although since the fractional
> frequency error is dimensionless
>
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Re: [time-nuts] OT: NZ Christchurch member

2011-02-25 Thread jimlux

On 2/25/11 7:55 AM, Poul-Henning Kamp wrote:

In message, "Wil
liam H. Fite" writes:


Me:  You're saying that the Richter is a poor predictor of surface
disruption?


For damage assement you really need a vector-version of richter,
vertical does a lot more damage than horizontal on average.




Yes.. I doubt anyone still uses the torsion seismometer Richter used, 
although more modern scales (moment magnitude, etc.) still relate back 
(e.g. they set the calibration to match for some notional set of events)..


That way, people have an idea... A Magnitude 3 earthquake within a few 
tens of km of me will be noticeable, if it's quiet. A magnitude 4 will 
be very noticeable, and a 5 will be exciting. A 6 will wake you up in 
the middle of the night.  I'd compare it to something like Mohs 
hardness, except actually with a quantitative basis.  (People who work 
with material properties like hardness use other scales anyway)


It's a "roughly quantitative" measure of energy release, in the same 
sense that kilotons are for explosions. It's like that whole "cup of 
gasoline: dynamite" comparison.. it's the rate of energy (e.g. power) 
that creates the qualitative difference between running my camping stove 
and blasting.


We do the same thing in time-nuttery.. we use log scales to talk about 
performance.. dBc/Hz for phase noise, and really, just the exponent to 
talk about ADEV.  (nobody gets excited about the difference between 
1.1E-13 and 1.5E-13... but the difference between 1E-11 and 1E-15 is 
worth talking about)


Maybe we should start promulgating dBallan?

And maybe get an SI unit... The "Allan", although since the fractional 
frequency error is dimensionless


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Re: [time-nuts] OT: NZ Christchurch member

2011-02-25 Thread Poul-Henning Kamp
In message , "Wil
liam H. Fite" writes:

>Me:  You're saying that the Richter is a poor predictor of surface
>disruption?

For damage assement you really need a vector-version of richter,
vertical does a lot more damage than horizontal on average.

-- 
Poul-Henning Kamp   | UNIX since Zilog Zeus 3.20
p...@freebsd.org | TCP/IP since RFC 956
FreeBSD committer   | BSD since 4.3-tahoe
Never attribute to malice what can adequately be explained by incompetence.

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Re: [time-nuts] OT: NZ Christchurch member

2011-02-25 Thread William H. Fite
For meteorologists and geologists, the Richter scale has a carefully defined
meaning and is used only for purposes where that definition fits.

This per a friend of mine who does seismic stuff for NOAA:
Him:  The Richter number means something very specific to us and something
quite different to the media.  Actually, the Richter doesn't have a great
deal of analytical value to us.  You can say, this is a Category Four
hurricane but that really tells you very little about what is going on in
the storm.  Richter is like that.
Me:  You're saying that the Richter is a poor predictor of surface
disruption?
Him:  Well, obviously a 9 will be expected to do much more damage than a 6
but it is at best a very rough indicator.  The location of the epicenter and
a dozen other factors play into it.
Me:  So how do you assess the damage potential?
Him:  Lots of people think we still rely mainly on the old
pendulum-and-stylus seismographs from the 1930s.  Actually, we take a great
many measurements in addition to seismometry.  But when it comes to
assessing the damage, we go outside and look, just like the TV stations do.

And his final comment:  By the way, did you know that when the shuttle
launches we capture that on virtually every strain guage seismometer in the
country?

I found that interesting.



On Thu, Feb 24, 2011 at 10:56 PM, jimlux  wrote:

> On 2/24/11 5:23 PM, Bob Bownes wrote:
>
>> What is the conversion factor for Richter to dBm? :)
>>
>> Bob
>> As a guy with degrees in geology and EE. I really should know this...:)
>>
>>
>>
> Especially since both are log scales..
>
> The problem is that Richter is log magnitude displacement on a particular
> kind of seismometer (which is sort of a low pass filter) and dBm is log
> power.  However, there should be some sort of scale factor that converts it.
>
> I think it's energy goes as amplitude^1.5.  there's also a scale factor for
> how far the seismograph is from the epicenter.
>
>
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Re: [time-nuts] OT: NZ Christchurch member

2011-02-24 Thread jimlux

On 2/24/11 5:23 PM, Bob Bownes wrote:

What is the conversion factor for Richter to dBm? :)

Bob
As a guy with degrees in geology and EE. I really should know this...:)




Especially since both are log scales..

The problem is that Richter is log magnitude displacement on a 
particular kind of seismometer (which is sort of a low pass filter) and 
dBm is log power.  However, there should be some sort of scale factor 
that converts it.


I think it's energy goes as amplitude^1.5.  there's also a scale factor 
for how far the seismograph is from the epicenter.


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Re: [time-nuts] OT: NZ Christchurch member

2011-02-24 Thread Bob Bownes
What is the conversion factor for Richter to dBm? :)

Bob
As a guy with degrees in geology and EE. I really should know this...:)


On Thu, Feb 24, 2011 at 8:11 PM, Magnus Danielson
 wrote:
> On 24/02/11 10:38, Steve Rooke wrote:
>>
>> I heard he was still shaking :)
>
> Did he get any amazing waveforms out of mother earths shaker-table?
>
> PS. Happy to hear you are alright and still has a sense of humor intact.
>
> Cheers,
> Magnus
>
>> Cheers, Steve
>>
>> On 24/02/2011, Raj  wrote:
>>>
>>> Anyone hear from Time-Nut Steve Rooke from Christchurch ?
>>>
>>> Cheers
>>>
>>> --
>>> Raj, VU2ZAP
>>> Bangalore, India.
>>>
>>>
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>>
>>
>
>
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Re: [time-nuts] OT: NZ Christchurch member

2011-02-24 Thread Magnus Danielson

On 24/02/11 10:38, Steve Rooke wrote:

I heard he was still shaking :)


Did he get any amazing waveforms out of mother earths shaker-table?

PS. Happy to hear you are alright and still has a sense of humor intact.

Cheers,
Magnus


Cheers, Steve

On 24/02/2011, Raj  wrote:

Anyone hear from Time-Nut Steve Rooke from Christchurch ?

Cheers

--
Raj, VU2ZAP
Bangalore, India.


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Re: [time-nuts] OT: NZ Christchurch member

2011-02-24 Thread WB6BNQ
Steve,

Isn't Bruce Griffiths in your area ?  I am wondering how he is doing ?

BillWB6BNQ



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Re: [time-nuts] OT: NZ Christchurch member

2011-02-24 Thread Steve Rooke
I heard he was still shaking :)

Cheers, Steve

On 24/02/2011, Raj  wrote:
> Anyone hear from Time-Nut Steve Rooke from Christchurch ?
>
> Cheers
>
> --
> Raj, VU2ZAP
> Bangalore, India.
>
>
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-- 
Steve Rooke - ZL3TUV & G8KVD
The only reason for time is so that everything doesn't happen at once.
- Einstein

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[time-nuts] OT: NZ Christchurch member

2011-02-23 Thread Raj
Anyone hear from Time-Nut Steve Rooke from Christchurch ?

Cheers

-- 
Raj, VU2ZAP
Bangalore, India. 


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