Re: Spherical Bouguer correction

Lester Anderson <[email protected]> Fri, 22 Aug 2014 09:56:50 +0100
Newsgroups gmane.comp.gis.gmt.user
Message-ID <[email protected]>
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Thanks for the clarification Walter

> Date: Thu=2C 21 Aug 2014 16:59:19 -0400
> From: [email protected]
> Subject: Re: [GMT-HELP] Spherical Bouguer correction
> To: [email protected]
>=20
> Lester=2C
>=20
> The difference is a factor of 2=2C so obviously one of these has to be wr=
ong.
>=20
> If you derive both you find that you can be outside an entire sphere=2C a=
nd so get the factor of 4=2C but you cannot be =93outside=94 an infinite sl=
ab=2C you can only be on one side of it=2C hence the factor of 2.
>=20
> However=2C in the course of the flat slab derivation you end up with some=
thing involving an argument (to a logarithm?) like H/R=2C and taking the li=
mit as R goes to infinity. Here=2C H is your slab thickness and R is the di=
stance between a point in the slab and the point you are trying to correct.
>=20
> Thus if your slab thickness=2C H=2C is short compared to the size of the =
earth=2C then use the slab formula. The curvature of the Earth is negligibl=
e if H is of order of the thickness of the crust=2C because H/R rapidly van=
ishes before R gets big enough for you to sense the curvature.
>=20
> Only if H is as thick as of the order of the radius of the earth do you n=
eed the formula with the 4=2C but by that point the Bouguer correction is a=
bsurd anyway and you should instead be calculating attractions directly.
>=20
> In other words=2C the Bouguer correction only makes sense in the case tha=
t H << R.
>=20
> Walter
>=20
>=20
>=20
> Walter H F Smith
> Geophysicist=2C Laboratory for Satellite Altimetry
> NOAA NCWCP code E/RA-31
> 5830 University Research Court=2C room 3752
> College Park MD 20740-3818
> 301-683-3377 (voice=2C my desk)
> 301-683-3300 (voice=2C reception)
> 301-683-3301 (fax=2C reception)
> [email protected]
> http://www.star.nesdis.noaa.gov/star/Smith_WHF.php
>=20
>=20
> On Aug 18=2C 2014=2C at 5:50 AM=2C Lester Anderson <lester_anderson1963@H=
OTMAIL.COM> wrote:
>=20
> > Hi all=2C
> >=20
> > Quick question (off topic)=2C but should one strictly be using the simp=
le spherical correction (4piG(rho)H) as opposed to the "infinite" slab (2pi=
G(rho)H) for the Bouguer calculation?
> >=20
> > Trying to think at what point this would become a significant considera=
tion in terms of a geographic area?
> >=20
> > Cheers
> > Lester
> > Mailing list for GMT discussions of all kinds. If you are not sure you =
have found a bug=2C discuss it here first. To formally report bugs or reque=
st features=2C please register and add New Issue on gmt.soest.hawaii.edu To=
 unsubscribe=2C send the message "signoff gmt-help" [email protected]=
.edu Note: gmt-help will become obsolete on Sept 1=2C 2014 - please use for=
um on gmt.soest.hawaii.edu instead.
>=20
> Mailing list for GMT discussions of all kinds.  If you are not sure you h=
ave found a bug=2C discuss it here first.
> To formally report bugs or request features=2C please register and add Ne=
w Issue on gmt.soest.hawaii.edu
> To unsubscribe=2C send the message "signoff gmt-help" to [email protected]=
awaii.edu
> Note: gmt-help will become obsolete on Sept 1=2C 2014 - please use forum =
on gmt.soest.hawaii.edu instead.
 		 	   		  =

Mailing list for GMT discussions of all kinds.  If you are not sure you have found a bug, discuss it here first.
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<body class=3D'hmmessage'><div dir=3D'ltr'>Thanks for the clarification Wal=
ter<br><br><div>&gt=3B Date: Thu=2C 21 Aug 2014 16:59:19 -0400<br>&gt=3B Fr=
om: [email protected]<br>&gt=3B Subject: Re: [GMT-HELP] Spherical Bo=
uguer correction<br>&gt=3B To: [email protected]<br>&gt=3B <br>&gt=
=3B Lester=2C<br>&gt=3B <br>&gt=3B The difference is a factor of 2=2C so ob=
viously one of these has to be wrong.<br>&gt=3B <br>&gt=3B If you derive bo=
th you find that you can be outside an entire sphere=2C and so get the fact=
or of 4=2C but you cannot be =93outside=94 an infinite slab=2C you can only=
 be on one side of it=2C hence the factor of 2.<br>&gt=3B <br>&gt=3B Howeve=
r=2C in the course of the flat slab derivation you end up with something in=
volving an argument (to a logarithm?) like H/R=2C and taking the limit as R=
 goes to infinity. Here=2C H is your slab thickness and R is the distance b=
etween a point in the slab and the point you are trying to correct.<br>&gt=
=3B <br>&gt=3B Thus if your slab thickness=2C H=2C is short compared to the=
 size of the earth=2C then use the slab formula. The curvature of the Earth=
 is negligible if H is of order of the thickness of the crust=2C because H/=
R rapidly vanishes before R gets big enough for you to sense the curvature.=
<br>&gt=3B <br>&gt=3B Only if H is as thick as of the order of the radius o=
f the earth do you need the formula with the 4=2C but by that point the Bou=
guer correction is absurd anyway and you should instead be calculating attr=
actions directly.<br>&gt=3B <br>&gt=3B In other words=2C the Bouguer correc=
tion only makes sense in the case that H &lt=3B&lt=3B R.<br>&gt=3B <br>&gt=
=3B Walter<br>&gt=3B <br>&gt=3B <br>&gt=3B <br>&gt=3B Walter H F Smith<br>&=
gt=3B Geophysicist=2C Laboratory for Satellite Altimetry<br>&gt=3B NOAA NCW=
CP code E/RA-31<br>&gt=3B 5830 University Research Court=2C room 3752<br>&g=
t=3B College Park MD 20740-3818<br>&gt=3B 301-683-3377 (voice=2C my desk)<b=
r>&gt=3B 301-683-3300 (voice=2C reception)<br>&gt=3B 301-683-3301 (fax=2C r=
eception)<br>&gt=3B [email protected]<br>&gt=3B http://www.star.nesd=
is.noaa.gov/star/Smith_WHF.php<br>&gt=3B <br>&gt=3B <br>&gt=3B On Aug 18=2C=
 2014=2C at 5:50 AM=2C Lester Anderson &[email protected]=
M&gt=3B wrote:<br>&gt=3B <br>&gt=3B &gt=3B Hi all=2C<br>&gt=3B &gt=3B <br>&=
gt=3B &gt=3B Quick question (off topic)=2C but should one strictly be using=
 the simple spherical correction (4piG(rho)H) as opposed to the "infinite" =
slab (2piG(rho)H) for the Bouguer calculation?<br>&gt=3B &gt=3B <br>&gt=3B =
&gt=3B Trying to think at what point this would become a significant consid=
eration in terms of a geographic area?<br>&gt=3B &gt=3B <br>&gt=3B &gt=3B C=
heers<br>&gt=3B &gt=3B Lester<br>&gt=3B &gt=3B Mailing list for GMT discuss=
ions of all kinds. If you are not sure you have found a bug=2C discuss it h=
ere first. To formally report bugs or request features=2C please register a=
nd add New Issue on gmt.soest.hawaii.edu To unsubscribe=2C send the message=
 "signoff gmt-help" [email protected] Note: gmt-help will become =
obsolete on Sept 1=2C 2014 - please use forum on gmt.soest.hawaii.edu inste=
ad.<br>&gt=3B <br>&gt=3B Mailing list for GMT discussions of all kinds.  If=
 you are not sure you have found a bug=2C discuss it here first.<br>&gt=3B =
To formally report bugs or request features=2C please register and add New =
Issue on gmt.soest.hawaii.edu<br>&gt=3B To unsubscribe=2C send the message =
"signoff gmt-help" to [email protected]<br>&gt=3B Note: gmt-help wi=
ll become obsolete on Sept 1=2C 2014 - please use forum on gmt.soest.hawaii=
.edu instead.<br></div> 		 	   		  </div></body>
</html>=
Mailing list for GMT discussions of all kinds.  If you are not sure you have found a bug, discuss it here first.
To formally report bugs or request features, please register and add New Issue on gmt.soest.hawaii.edu
To unsubscribe, send the message &quot;signoff gmt-help&quot; to <a href=3D"mailto:[email protected]">[email protected]</a>
Note: gmt-help will become obsolete on Sept 1, 2014 - please use forum on gmt.soest.hawaii.edu instead.

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