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ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
The
Spec
ial R
ole
of S
LR fo
rIn
ter-
Tech
niqu
eC
ombi
natio
ns
Mar
kus
Rot
hach
erFo
rsch
ungs
einr
icht
ung
Sat
ellit
enge
odäs
ie, T
U M
ünch
en(F
ES
G)
ILR
S W
orks
hop
2003
Oct
ober
28-3
1, 2
003
Koe
tztin
g, G
erm
any
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
•In
trodu
ctio
n
•S
&S
:So
lutio
ns a
nd S
tatis
tics
•W
&W
:W
avel
engt
h an
d W
ater
Vap
or
•C
&C
:C
lock
s an
d C
orre
latio
ns
•A
&A
:A
nten
nas
and
Abs
olut
e S
cale
•G
&G
:G
eom
etry
and
Gra
vity
•O
&O
:O
rbits
and
“O-C
”
•C
oncl
usio
ns
Con
tent
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Intr
oduc
tion:
Vis
ion
of a
Rig
orou
s C
ombi
natio
n
•M
ake
use
of th
e st
reng
ths
of th
e in
divi
dual
ob
serv
atio
n te
chni
ques
•P
rofit
from
co-
loca
tion
of in
stru
men
ts
(site
s an
d sa
telli
tes)
•E
nsur
e co
nsis
tenc
ybe
twee
n al
l te
chni
ques
•D
iffer
bet
wee
n te
chni
que-
spec
ific
syst
emat
ic b
iase
san
d ge
nuin
e ge
odet
ic/g
eoph
ysic
al s
igna
ls
•Fi
nal g
oal:
All
com
mon
par
amet
ers
of a
ll ob
serv
ing
tech
niqu
es a
re ri
goro
usly
co
mbi
ned
as c
onsi
sten
t inp
ut to
the
IGG
OS
pr
ojec
t
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Para
met
er S
pace
forC
ombi
natio
n
Para
met
er T
ype
VL
BI
GPS
/G
LO
N.
DO
RIS
/PR
AR
ESL
RL
LR
Alti
-m
etry
Qua
sar C
oord
. (IC
RF)
XN
utat
ion
X(X
)X
Pola
r Mot
ion
XX
XX
XU
T1X
Leng
thof
Day
(LO
D)
XX
XX
Sub-
Dai
lyER
PsX
XER
P O
cean
Tid
eA
mpl
itude
sX
XX
X
Coo
rd.+
Vel
oc.(I
TRF)
XX
XX
X(X
)G
eoce
nter
X
XX
XG
ravi
tyFi
eld
XX
X(X
)X
Orb
itsX
XX
XX
LEO
Orb
itsX
XX
XIo
nosp
here
XX
XX
Trop
osph
ere
XX
XX
Tim
e/Fr
eq. T
rans
fer
(X)
X(X
)
Major SLR Contributions
(X)
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Solu
tions
and
Stat
istic
s(S
&S)
CO
NT‘
02SL
R
VLB
I G
PS
# O
bs.
5’19
546
’682
5’93
5’76
0 #
Coo
rd.
8124
459
# E
OP
75
7575
#
Trop
os.
01’
554
26’7
26
# O
rbits
30
03’
770
# A
mbi
g.
00
43’2
38
# C
lock
s 0
1’16
4--
- #
Par
am.
186
2’81
774
’268
CO
NT‘
02 V
LBI C
ampa
ign
•D
GFI
: VLB
Isol
utio
ns•
TUM
: G
PSso
lutio
ns•
TUM
: SL
Rso
lutio
ns(L
1+L2
)
Oct
ober
17-3
0, 2
003,
con
tinuo
usV
LBI
SLR
: few
obse
rvat
ions
buta
lso
few
para
met
ers
(no
cloc
ks, n
o tro
posp
here
, no
ambi
guiti
es,…
)
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Wav
elen
gth
and
Wat
erVa
por(
W&
W)
SLR
is th
e on
ly te
chni
que
obse
rvin
g at
opt
ical
wav
elen
gths
:
•S
LR is
in a
uni
que
situ
atio
nco
ncer
ning
atm
osph
eric
refra
ctio
n•
Trop
osph
ere
disp
ersi
vefo
r SLR
, but
not
for m
icro
wav
es•
Two-
frequ
ency
lase
r ran
ging
(mai
nly
valid
atio
n to
ol ?
)•
Dry
del
ay c
an b
e m
odel
ed w
ith p
ress
ure
data
at t
he s
ite•
Wet
del
ay is
qui
te s
mal
l
All
othe
r tec
hniq
ues
(GPS
, VLB
I, D
OR
IS, a
ltim
etry
, InS
AR
, …):
•S
uffe
r fro
m th
e sa
me
trop
osph
eric
refr
actio
n ef
fect
s•
Suf
fer f
rom
sim
ilar i
onos
pher
icre
frac
tion
effe
cts
•H
ave
tropo
sphe
ricre
fract
ion
as th
e or
a m
ajor
err
or s
ourc
e
Onl
y SL
R c
an h
elp
to d
etec
t bia
ses
(e.g
. due
to a
tmos
pher
e m
ism
odel
ing)
com
mon
to a
ll ot
her t
echn
ique
s
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Wav
elen
gth
and
Wat
erVa
por(
W&
W)
Influ
ence
of
wat
er v
apor
eon
SLR
/LLR
(Mar
ini-M
urra
y):
ez
SLR wet
trp
⋅≈
=00
0141
.0)0
(,
δρIn
fluen
ce o
f w
ater
vap
or o
n G
PS/V
LBI/D
OR
IS (S
aast
amoi
nen)
:
Rat
io o
f Mic
row
ave/
SLR
:
ee
Tz
Micro wet
trp
⋅≈
⋅
+⋅
≈=
0096
.005.0
1225
0022
77.0
)0(
,δρ Wet
del
ay: G
PS/V
LBI/D
OR
IS u
p to
40
cm; S
LR u
p to
6 m
m
Trop
osph
ere
zeni
th d
elay
par
amet
ers ―
wea
keni
ng th
e so
lutio
ns ―
have
to b
e es
timat
ed fo
r mic
row
ave
tech
niqu
es, b
ut n
ot fo
r SLR
68)0
()0
(
,,≈
==zz
SLR wet
trpMicro wet
trp
δρδρ
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Clo
cks
and
Cor
rela
tions
(C&
C)
Estim
atio
n of
clo
ck p
aram
eter
s:
•SL
R: t
he o
nly
tech
niqu
e, w
here
in g
ener
al n
o cl
ock
corr
ectio
nsha
ve
to b
e es
timat
ed•
GPS
: rec
eive
r and
sat
ellit
e cl
ock
para
met
ers
for e
very
epo
ch•
VLB
I: re
ceiv
er c
lock
cor
rect
ions
abo
ut e
very
hou
r (be
twee
n st
atio
ns)
•D
OR
IS: c
lock
bia
ses
have
to b
e es
timat
ed to
o
Estim
atio
n of
clo
ck p
aram
eter
s de
grad
es th
e he
ight
qua
lity
Exce
ptio
ns fo
r SLR
:•
Estim
atio
n of
a ra
nge
bias
for a
n S
LR s
tatio
n: c
orre
spon
ds to
a
rece
iver
clo
ck c
orre
ctio
nin
GP
S/V
LBI/D
OR
IS
•Es
timat
ion
of a
tim
e bi
ases
for a
n S
LR s
tatio
n
Estim
atio
n of
rang
e bi
ases
sho
uld
be a
void
ed to
the
exte
nt p
ossi
ble
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Para
met
er Z
enith
-Dep
ende
nce
z
z
.
..
.
z
Sta
tion
Hei
ght
Zeni
th T
ropo
sphe
reD
elay
Clo
ckC
orre
ctio
n()
()
() 0
cos
hh
zz
δρδρ
⋅=
()
()
() 0
cos1
trp
trp
zz
δρδρ
⋅=
()
()
Rclk
clk
tc
zδ
δρδρ
⋅=
=0
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Cor
rela
tion:
Hei
ght,
Clo
cks,
Tro
posp
here
•In
fluen
ce o
f clo
ck a
nd
tropo
sphe
re e
stim
atio
n on
st
atio
n he
ight
(San
terr
e)
•Ex
trem
e co
rrel
atio
ns
betw
een
heig
ht, c
lock
, and
tro
posp
here
zen
ith d
elay
•N
o pr
oble
m fo
r SLR
: he
ight
s sh
ould
be
perfe
ct
Coo
rd. +
Clo
ckC
oord
. onl
yC
oord
.+Tr
opo.
z max
σ1 h
/σ0 h
Co
r(h
,trp
)70
13.7
8-0
.964
759.
23-0
.943
806.
13-0
.907
853.
94-0
.830
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Obs
erva
tion
Geo
met
ry
Nic
eob
serv
atio
nge
omet
ryfo
rgoo
d st
atio
ns(1
4 da
ys)
Wel
l-sui
ted
for
heig
htde
term
inat
ion
SLR
ver
y im
port
ant f
or
abso
lute
hei
ght
estim
atio
n Es
timat
ion
of
rang
e bi
ases
sh
ould
be
avoi
ded
to th
e ex
tent
po
ssib
le
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Ant
enna
san
d A
bsol
ute
Scal
e(A
&A
)C
hara
cter
istic
s of
GPS
rece
iver
and
sat
ellit
e an
tenn
as:
•N
ot a
ccur
atel
y kn
own,
cha
ngin
g w
ith e
leva
tion
and
azim
uth
•G
PS
resu
lts d
epen
dent
on
elev
atio
n cu
t-off
•La
rge
syst
emat
ic e
ffect
s du
e to
ant
enna
pha
se c
ente
rcor
rect
ions
(r
ecei
ver a
nd s
atel
lite
ante
nnas
)•
Man
y ch
ange
s of
GP
S re
ceiv
er/a
nten
na e
quip
men
t (ju
mps
in h
eigh
t)•
GP
S is
too
muc
h af
fect
ed b
y sy
stem
atic
effe
cts
to a
llow
acc
urat
eab
solu
te h
eigh
tand
abs
olut
e sc
ale
dete
rmin
atio
n in
the
glob
al
netw
ork
and
for I
TRF.
VLB
I tel
esco
pes:
•V
LBI t
eles
cope
s ar
e hu
ge a
nd h
eavy
stru
ctur
es•
VLB
I tel
esco
pe d
efor
mat
ion
may
bia
s re
sults
(ele
vatio
n de
pend
ence
?)
SLR
: no
such
ant
enna
pro
blem
s (d
efor
mat
ion
shou
ld b
e sm
all,
no
phas
e ce
nter
var
iatio
ns):
wel
l-sui
ted
to d
efin
e sc
ale
of IT
RF;
but
ca
libra
tion
has
to b
e ve
ry a
ccur
ate
and
relia
ble.
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Ant
enna
Phas
e C
ente
r Cor
rect
ions
Ant
enna
phas
ece
nter
varia
tions
:
•G
PS
rece
iver
ante
nna
•G
PS
sat
ellit
ean
tenn
a
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
GPS
: Ele
vatio
n C
ut-O
ff Ef
fect
•C
hang
e of
sta
tion
coor
dina
tes
due
to a
ch
ange
in e
leva
tion
cut-o
ff an
gle
•M
ost u
p-to
-dat
e ab
solu
te p
hase
cen
ter
varia
tions
used
for
rece
iver
s (r
obot
m
easu
rem
ents
) and
sa
telli
tes
(glo
bal
estim
atio
n)
•A
nten
nas
are
a cr
itica
l er
ror s
ourc
e !
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
GPS
: Abs
olut
e-R
elat
ive
Ant
enna
Patte
rns
•C
hang
e fro
m re
lativ
e (n
ow in
use
) to
abso
lute
ant
enna
in
form
atio
n (to
be
used
by
IGS
in
futu
re)
•A
bsol
ute
phas
e ce
nter
var
iatio
ns o
nly
deriv
able
with
fixe
d IT
RF
scal
e.
•Sy
stem
atic
cha
nge
in
scal
e to
ITR
F (s
ever
al m
m)
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Com
paris
onof
GPS
& V
LBI T
ropo
sphe
re
•C
ON
T’02
Cam
paig
n (1
4 da
ys)
•V
ery
nice
agr
eem
ent i
n te
mpo
ral v
aria
tions
, but
larg
e sy
stem
atic
bi
ases
betw
een
VLB
I and
GP
S, i
ndic
atin
g so
me
unm
odel
edef
fect
s
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Com
paris
onof
GPS
& V
LBI T
ropo
sphe
re
Diff
eren
ce b
etw
een
GPS
and
VLB
I
0510152025
ALGO
FAIR
HRAO
KOKB
NYA1
ONSA
WES2
WTZR
Zenith Trop. Delay [mm]
Theo
ryEs
timat
es
4.5
0.9
3.10
WTZ
R
11.7
0.5
1.75
WE
S2
5.1
4.1
13.7
1O
NS
A
1.7
0.9
3.07
NY
A1
14.2
2.8
9.24
KO
KB
7.8
0.5
1.54
HR
AO
6.8
3.9
13.0
8FA
IR
14.0
6.9
23.1
1A
LGO
∆ZT
DE
stim
.[m
m]
∆ZT
DTh
eory
[mm
]
∆H
eigh
t(lo
calt
ie)
[m]
Sta
tion
∆H
eigh
t= 1
0m →
∆ZD
≈3m
m
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Rot
atio
n an
d R
otat
ion
Rat
es (R
&R
)O
ne-to
-one
rela
tion
betw
een
chan
ges
in U
T1-U
TC, ∆
ε, ∆ψ
and
chan
ges
in th
eor
bita
l ele
men
tsΩ
, i, u
0 (ρ
=1.0
0273
79):
→U
T1-U
TC a
nd n
utat
ion
offs
ets
cann
otbe
estim
ated
toge
ther
with
orbi
tal e
lem
ents
→LO
D a
nd n
utat
ion
rate
sca
nbe
estim
ated
bysa
telli
tete
chni
ques
; qu
ality
of o
rbit
mod
elis
cruc
ial(
chan
ges
of e
lem
ents
with
time)
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
UT1
-UTC
and
Nut
atio
nfr
omSL
R
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
LOD
and
Nut
atio
nR
ates
from
SLR
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Nut
atio
nfr
omSL
R, G
PS, a
nd V
LBI
•C
ompa
rison
of n
utat
ion
durin
gth
eC
ON
T’02
Cam
paig
n(1
4 da
ys)
•S
LR re
sults
sim
ilart
o th
ose
of G
PS
(at l
east
in o
bliq
uity
)
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
LOD
from
SLR
, GPS
, and
VLB
I •C
ON
T’02
C
ampa
ign
(1
4 da
ys)
•S
ubda
ilyLO
D
from
GP
S a
nd
VLB
I
•D
aily
val
ues
from
SLR
(L
ageo
s1
+ 2)
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
X-an
d Y-
Pole
from
SLR
CO
NT’
02 C
ampa
ign
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Geo
met
ryan
d G
ravi
ty(G
&G
)
SLR
is o
ne o
f the
maj
or te
chni
ques
to e
stab
lish
a lin
k be
twee
n ge
omet
ry, E
arth
rota
tion,
and
gra
vity
(thr
ee p
illar
s of
geo
desy
):
•G
eoce
nter
: rel
atio
n be
twee
n or
igin
of I
TRF
and
low
ord
er h
arm
onic
s co
effic
ient
C01
, C11
, S11
of th
e E
arth
’s g
ravi
ty fi
eld
•P
rinci
ple
axes
of i
nerti
a te
nsor
: rel
atio
n be
twee
n E
arth
rota
tion,
or
ient
atio
n of
the
grav
ity fi
eld
(C21
, S21
, S22
), an
d IT
RF
orie
ntat
ion
•H
elp
to d
istin
guis
h be
twee
n “m
atte
r ter
ms”
and
“mot
ion
term
s”
(gra
vity
“fee
ls” o
nly
“mat
ter”
, Ear
th ro
tatio
n “m
atte
r” a
nd “m
otio
n”)
SLR
as
a lin
k be
twee
n 3
pilla
rs: v
ery
impo
rtant
for t
he IG
GO
S in
tegr
atio
n co
ncep
t and
for I
ER
S re
fere
nce
fram
e de
finiti
ons
Gra
vity
fiel
d va
riatio
ns d
ue to
exa
ctly
the
sam
e Ea
rth
proc
esse
s(e
.g.,
from
geo
phys
ical
flui
ds) a
s E
arth
rota
tion
and
defo
rmat
ion
(geo
met
ry)
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Thre
eLa
yers
of O
bjec
ts
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Orb
its a
nd „
Obs
erve
d-C
ompu
ted“
(O&
O)
Valid
atio
n of
GN
SS o
rbits
(GPS
, Glo
nass
, Gal
ileo,
…):
•S
LR m
easu
rem
ents
are
suc
cess
fully
use
d to
val
idat
e G
NS
S o
rbits
•Sy
stem
atic
bia
sof
abo
ut 4
-5 c
m(!)
bet
wee
n G
PS
orb
its fr
om
mic
row
ave
and
SLR
obs
erva
tions
―re
ason
stil
l unc
lear
•M
ay b
ecom
e im
porta
nt fo
r Gal
ileo
sate
llites
, too
Valid
atio
n of
Low
Ear
th O
rbite
r (LE
O) o
rbits
:•
Muc
h pr
ogre
ss in
pre
cise
orb
it de
term
inat
ion
(PO
D) o
f LEO
sth
anks
to v
alid
atio
n w
ith S
LR “o
bser
ved-
com
pute
d” (O
-C)
•Ev
alua
tion
of d
iffer
ent s
trat
egie
s(k
inem
atic
, red
uced
-dyn
amic
, …)
and
softw
are
pack
ages
and
para
met
eriz
atio
ns•
SLR
“O-C
” val
ues
allo
w d
etec
tion
of s
yste
mat
ic o
rbit
erro
rs
SLR
obs
erva
tions
are
ext
rem
ely
valu
able
for P
OD
stu
dies
; PO
D
beco
mes
eve
r mor
e cr
ucia
l for
new
sat
ellit
e m
issi
ons
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
SLR
Val
idat
ion
of C
HA
MP
GPS
Orb
its
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
CH
AM
P O
rbits
: Obs
erve
d-C
ompu
ted
•S
LR “O
-C” v
alue
s (o
r res
idua
ls) s
till
show
sig
nific
ant s
yste
mat
ic
tren
dsfo
r ind
ivid
ual p
asse
s
•Si
mila
r beh
avio
r of k
inem
atic
and
redu
ced-
dyna
mic
orbi
t res
idua
ls
•D
etai
led
anal
ysis
of t
he re
sidu
als
may
giv
e in
form
atio
n on
mod
el
defic
ienc
es, e
.g.:
–G
PS
pol
ariz
atio
n ef
fect
–R
elat
ivis
tic c
orre
ctio
ns–
Hig
her o
rder
iono
sphe
ricco
rrec
tions
–
Orb
it pa
ram
eter
izat
ion
…
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Futu
re C
ombi
natio
n: "
Wee
kly"
SIN
EX S
olut
ions
IVS
AC
1IV
S A
C 2
IVS
AC
n
Site
Coo
rd.,
EO
Ps,
Qua
sar
Coo
rd.
IGS
AC
1IG
S A
C 2
IGS
AC
n
Site
Coo
rdin
ates
, EO
Ps
ILR
S A
C 1
ILR
S A
C 2
ILR
S A
C n
Site
Coo
rdin
ates
, EO
Ps
IDS
AC
1ID
S A
C 2
IDS
AC
n
Site
Coo
rdin
taes
, EO
Ps
IVS
Com
bina
tion
Site
Coo
rd.,
EO
Ps,
Qua
sar C
oord
.
IGS
Com
bina
tion
Site
Coo
rdin
ates
, EO
Ps
ILR
S C
ombi
natio
n
Site
Coo
rdin
ates
, EO
Ps
IDS
Com
bina
tion
Site
Coo
rdin
ates
, EO
Ps
Com
bine
d"w
eekl
y"
Inte
r-te
chni
que
Solu
tions
Site
Coo
rdin
ates
, EO
Ps,
Qua
sar C
oord
inat
es
IER
S C
ombi
natio
n C
ente
rs
Loca
l Tie
Info
rmat
ion
Rem
ove
Bia
ses
Bet
wee
n Te
chni
ques
VLB
IG
PSSL
R/L
LRD
OR
IS
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Futu
re C
ombi
natio
n: M
ulti-
Year
Sol
utio
ns(F
ully
Con
sist
ent S
et o
f ITR
F/EO
Ps/IC
RF)
Wee
k 1
Wee
k 2
Wee
k n
Com
bine
dS
olut
ions
:S
ite C
oord
., E
OP
s,Q
uasa
r Coo
rdin
ates
Tim
e Se
ries
of S
ite C
oord
inat
es
ITR
F
Site
Coo
rdin
ates
+S
ite V
eloc
ities
EOP
Com
bine
d S
erie
sX
p, Y
p, U
T1,
∆ε,
∆ψ
ICR
F
Qua
sar C
oord
.+
Qua
sar M
otio
n
Tim
e Se
ries
of E
OPs
Tim
e Se
ries
of Q
uasa
r Coo
rdin
ates
Pre
-elim
inat
ion
of E
OP
sR
esub
stitu
tion
(Hel
mer
tBlo
ckin
g)
Han
dlin
g of
Site
Cha
nges
, N
on-li
near
Mot
ion
Ann
ual S
igna
ls
Sam
e flo
wch
art a
lso
valid
for
indi
vidu
al te
chni
ques
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Mea
surin
gan
d M
odel
ing
the
Eart
h Sy
stem
Mea
surin
g In
form
atio
n ab
out E
arth
Sys
tem
Influ
ence
/ M
odel
ling
Obs
erva
tion
Mod
ellin
g
Spac
e G
eode
tic
Tech
niqu
es
VLB
I
SLR
LLR
GP
S
DO
RIS
Alti
met
ry
InS
AR
Rin
glas
er
Geo
met
ry
Sta
tion
Pos
ition
/Mot
ion,
Sea
Leve
l Cha
nge,
Def
orm
atio
n
Eart
h R
otat
ion
Pre
cess
ion/
Nut
atio
n,P
olar
Mot
ion,
U
T1, L
OD
Gra
vity
Geo
cent
erG
ravi
ty fi
eld,
Te
mpo
ral v
aria
tions
Eart
h Sy
stem
(incl
. GG
F)
Sun
/Moo
n
(Pla
nets
)
Atm
osph
ere
Oce
an
Hyd
rosp
here
Cry
osph
ere
Cor
e
Man
tle
Cru
st
C O M B I N A T I O N
I N T E R A C T I O N S
ILR
S W
orks
hop
2003
, Oct
ober
28-3
1, 2
003,
Köt
ztin
g, G
erm
any
Con
clus
ions
•S
LR h
as fe
w o
bser
vatio
ns, b
ut a
lso
few
par
amet
ers
to e
stim
ate
•S
LR is
the
only
opt
ical
tech
niqu
e (u
niqu
e to
ass
ess
atm
osph
ere
bias
es)
•N
o tro
posp
here
est
imat
ion
nece
ssar
y fo
r SLR
(cor
rela
tions
, bia
ses)
•N
o cl
ock
corr
ectio
n es
timat
ion
nece
ssar
y fo
r SLR
(cor
rela
tions
, bi
ases
) →
good
hei
ghts
•N
o bi
g an
tenn
a pr
oble
ms
→ab
solu
te s
cale
, hei
ghts
•Im
porta
nt li
nk b
etw
een
grav
ity, E
arth
rota
tion,
and
geo
met
ry•
SLR
O-C
cru
cial
for p
rogr
ess
in P
OD
SLR
is a
uni
que
part
ner i
n th
e go
al o
f a ri
goro
us c
ombi
natio
n of
the
spac
e ge
odet
ic te
chni
ques
(IER
S an
d IG
GO
S)Th
e in
divi
dual
tech
niqu
es s
houl
d fe
el a
s a
part
of a
larg
er w
hole
w
ith a
com
mon
goa
l rat
her t
han
wor
king
in c
ompe
titio
nIn
terli
nked
, the
tech
niqu
es a
re m
uch
stro
nger
and
it is
mor
e di
fficu
lt to
isol
ate
and
cut i
ndiv
idua
l tec
hniq
ues