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DORIS Zenith Tropospheric Delays available from the IGN Analysis Center Pascal Willis, Olivier Bock, Yoaz BarSever, Kamil Teke

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DORIS  Zenith  Tropospheric  Delays  available  from  the  IGN  Analysis  

Center  

Pascal  Willis,  Olivier  Bock,    Yoaz  Bar-­‐Sever,  Kamil  Teke  

SUMMARY  

•  Overview  of  DORIS  tropospheric  results  •  SpaKal/temporal  interpolaKon  issues  

•  Some  results  

•  Conclusions  

Recent  studies  at  IGN  Reference   sta+ons   period   comparisons   results  

Snajdrova  et  al.,  J  Geod.,  2006  

VLBI  /  CONT  3  

CONT05  2  weeks  

VLBI  GPS  ECMWV  WVR  

ZTD  

Bock  et  al.,  Adv.  Space  Res.,  2010  

GPS  30  

1  year  (2007)  

GPS   ZTD  

Teke  et  al.,  J.  Geod.,  2011  

VLBI  /  CONT  3  

CONT08  2  weeks  

VLBI  GPS  ECMWV  WVR  

ZTD  gradients  

Willis  et  al.,  IAG  Symp.,  2012  

GPS  30  

1  year  (2007)  

GPS   gradients  

Willis  et  al.,  IAG  Symp.,  in  press  

GPS  30  

1  year  (2010  

GPS   ZTD  gradients  

Willis  et  al.,  Adv.  Space  Res.,  submi_ed  

GAVB  1  

3  years   GPS  ECMWF  

ZTD  gradients  

SpaKal/temporal  interpolaKon  

•  Temporal  :  need  to  interpolate  GPS  (or  other)  and  to  compare  at  DORIS  data  points  (related  to  satellite  passes)  

•  SpaKal  :  need  to  correct  for  dry  and  wet  delays  (from  antenna  reference  point  to  antenna  reference  point)  

NB:  especially  important  for  VLBI  (2-­‐3  km  away)  

CorrecKng  with  tropospheric  Ke  

258 260 262 264 266 268 270 2720.42

0.4

0.38

0.36

0.34

0.32

0.3KOKEE (VLBI) KOLB (DORIS)

DOY 2011

Trop

osph

ere

ties

in m

m

Hydrostatic ties Total (hyd.+wet) ties

258 260 262 264 266 268 270 27231

32

33

34

35

36

37

38

39

40

41HARTRAO (VLBI) HBMB (DORIS)

DOY 2011Tr

opos

pher

e tie

s in

mm

Hydrostatic tiesTotal (hyd.+wet) ties

Kokee  Park   Hartebeestoech  

From  Teke  et  al.,  in  prep.  

 Need  to  correct  as  reference  points  are  different  for  hydrostaKc  +  wet  

Examples  of  CONT11  results  

15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30

2120

2130

2140

2150

2160

2170

2180

2190

September 2011

zeni

th to

tal d

elay

s in

mm

BADARY BADB

VLBI VieVSNWM ECMWFDORIS IGN

15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30

2300

2310

2320

2330

2340

2350

2360

2370

2380

September 2011

zeni

th to

tal d

elay

s in

mm

NYALES20 NYA1 SPJB

VLBI VieVSGPS CODENWM ECMWFDORIS IGN

15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30

2060

2080

2100

2120

2140

2160

2180

2200

September 2011

zeni

th to

tal d

elay

s in

mm

KOKEE KOKB KOLB

VLBI VieVSGPS CODENWM ECMWFDORIS IGN

15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 301980

2000

2020

2040

2060

2080

2100

2120

September 2011

zeni

th to

tal d

elay

s in

mm

HARTRAO HRAO HBMB

VLBI VieVSGPS CODENWM ECMWFDORIS IGN

FromTeke  et  al.,  in  prep.  

CONT11  results  

0 1 2 3 4 5 615

10

5

0

5

10

15

20

Har

tebe

etsh

oek

HBM

B

Koke

eKO

LB

Bada

ryBA

DB

Ny

Ales

und

SPJB

MEA

N(E

CM

WF

DO

RIS

)

mm

0 1 2 3 4 54

2

0

2

4

6

8

10

12

HRAO

HBM

B

KOKB

KOLB

NYA

1SP

JB

MEA

N(GPS

DORIS)

mm

0 1 2 3 4 5 66

4

2

0

2

4

6

8

10

12

14

HAR

TRAO

HBM

B

KOKE

EKO

LB

BADAR

YBA

DB NYA

LES20SP

JB

MEA

N(VLBIDORIS)

mm

DORIS  vs.  ECMWF   DORIS  vs.  VLBI   DORIS  vs.  GPS  

NB:  light  grey  =  standard  deviaKon  of  differences,  dark  grey  =  mean  bias  

ZTD  vs.  number  of  DORIS  satellites  

Bock  et  al.,  in  prep  

Comparisons  at  GAVB  (ECMWF)  

ZTD  comparisons  at  GAVD  (with  GPS)  

Zoom  

From  Willis  et  al.,  submi_ed  

Horizontal  gradients  

LaKtude  dependency  

GPS/DORIS  correlaKon  

From  Willis  et  al.,  2012  

Tropospheric  North  gradients  /  CONT11  

15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30

2

1.5

1

0.5

0

0.5

1

1.5

2

2.5

September 2011

tropo

sphe

re n

orth

gra

dien

ts in

mm

KOKEE KOKB KOLB

VLBI VieVSGPS CODENWM ECMWFDORIS IGN

From  Teke  et  al.,  in  prep.  

15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30

1.5

1

0.5

0

0.5

September 2011

tropo

sphe

re n

orth

gra

dien

ts in

mm

NYALES20 NYA1 SPJB

VLBI VieVSGPS CODENWM ECMWFDORIS IGN

Conclusions  

•  ZTD  :  mulKple  comparisons  were  done  –  VLBI,  GPS,  ECMWF  –  Short  Kme  periods  (CONT-­‐type  comparisons)  –  Long  Kme  periods  (staKon-­‐specific)  

•  Horizontal  gradients  – GPS  intercomparisons  +  recent  CONT  results  

Possible  use  for  climatological  studies  (long-­‐term,  post-­‐processing  mode)