time stability of the k-band catalog sources · using the allan variance to determine noise floor...
TRANSCRIPT
Time stability of the K-band catalog sources
K.LeBail(1),A.deWi1(2),C.S.Jacobs(3),D.Gordon(1)(1)NVI,Inc.,NASA/GSFC(code61A),Greenbelt,MD,U.-S.
(2)SARAO/HartRAO,Krugersdorp,SouthAfrica(3)JetPropulsionLaboratory,CaliforniaInst.Technology/NASA,Pasadena,CA,U.-S.
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Acknowledgements: Copyright ©2019. All Rights Reserved. U.S. Government sponsorship acknowledged for work done at JPL-Caltech under a contract with NASA. The VLBA is managed by NRAO, funded by the National Science Foundation, and operated under cooperative agreement by Associated Universities. The authors gratefully acknowledge use of the VLBA under the USNO’s time allocation. This work supports USNO’s ongoing research into the celestial reference frame and geodesy. HartRAO is a facility of the National Research Foundation (NRF) of South Africa. The Hobart telescope is operated by the University of Tasmania and this research has been supported by AuScope Ltd., funded under the National Collaborative Research Infrastructure Strategy (NCRIS).
Outline
• K-bandinICRF3• BriefreviewonhowtousetheAllanvariancetodeterminenoisefloorofsourceUmeseries
• NoisefloorofthelatestGSFCK-bandUmeseriessoluUonandcomparisonwiththelatestGSFCS/XUmeseriessoluUonon3differentsets
2/1624thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
K-band
K-bandinICRF3
3/16
Ksolu'on S/Xsolu'on
Source# 906 4775
Session# 65 6271
ObservaUonperiod
05/2002–11/2018
08/1979–01/2019
Source#(≥10sessions)
354 788
SeeposterP306:A.deWi1etal.,“TheK-band(24GHz)CelesUalReferenceFrame”.
Thispaper:StudyofthelatestGSFCUmeseriessoluUonsforKandS/X.
−80 −60 −40 −20 0 20 40 60 800
20
40
60
80
100
Declination (deg)
Sour
ce n
oise
(µas
)
ICRF3 decimation test − Right Ascension
S/X noise floorK noise floor
−80 −60 −40 −20 0 20 40 60 800
20
40
60
80
100
Declination (deg)
Sour
ce n
oise
(µas
)
ICRF3 decimation test − Declination
S/X noise floorK noise floor
310commonsources
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
0
20
40
60
80
100
-90 -80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90
S/Xnoisefloor Knoisefloor
0
20
40
60
80
100
-90 -80 -70 -60 -50 -40 -30 -20 -10 0 10 20 30 40 50 60 70 80 90
S/Xnoisefloor Knoisefloor
K-band and S/X-band Position time series examples
DifferentwaystolookattheseUmeseries:
• StandarddeviaUon=>staUcquanUty;
• NoisefloordeterminedwiththeAllanvariance=>takesintoaccounttheUmevariable.
4/16
1980 1985 1990 1995 2000 2005 2010 2015 2020−1
−0.5
0
0.5
1
RAcosDEC (mas) 0552+398
S/X Standard dev: 1.512 K Standard dev: 0.139
S/XK
1980 1985 1990 1995 2000 2005 2010 2015 2020−1
−0.5
0
0.5
1
DEC (mas) 0552+398
S/X Standard dev: 1.864 K Standard dev: 0.165
S/XK
1980 1985 1990 1995 2000 2005 2010 2015 2020−1
−0.5
0
0.5
1
RAcosDEC (mas) 3C120
S/X Standard dev: 4.686 K Standard dev: 0.166
S/XK
1980 1985 1990 1995 2000 2005 2010 2015 2020−1
−0.5
0
0.5
1
DEC (mas) 3C120
S/X Standard dev: 4.770 K Standard dev: 0.217
S/XK
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Using the Allan variance to determine noise floor (1/2)
-1 Whitenoise
0 Flickernoise
+1 Randomwalk
5/16
• TheAllanvarianceisastaUsUcaltoolthatgivesthelevelandtypeofnoiseofUmeseries.
• IfarethemeasurementsandτthesamplingUme,theAllanvarianceis:
• Typeofnoisedeterminedbytheslopeofthecurve:€
xi( )i=1,n
€
σ2 τ( ) =12
xi+1 − xi( )2
€
log10 σ2( ) = f log10 τ( )( )
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Whitenoise Flickernoise Randomwalk
Realdata:sourcesnotobservedregularly=>difficulUesinstaUsUcaldeterminaUonduetogapsinbetweenobservaUons,numberofobservaUons,…PreprocessingoftheUmeseries.• Step1:Keepsourceswith10ormoreobservaUons.• Step2:Averaging(yearlyandmonthly)andinterpolaUon.Thresholdcut-offwheninterpolaUng.
• Step3:Allanvarianceprocessingforeachsource,eachcoordinate,eachaveragedUmeseries.
• Step4:NoisefloordeterminaUonforeachsourceandeachcoordinate.WelookatthenoisetypedeterminedbytheslopeoftheAllanvariancecurve:
• Whitenoiseorflickernoise:thenoiseflooristhelowestAllanvariancevalue.• Randomwalk:sourcerejected.
6/16
Using the Allan variance to determine noise floor (2/2)
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Comparison 1/3 310 common sources – Period 1979-now
TheKnoisefloorstendtobesmallerthantheS/Xnoisefloors.
7/16
StandarddeviaUonNoisefloordeterminedby
theAllanvariance
500 1000 1500 20000
20
40
60
80
100
120
140
Source standard deviation (µas)
Sour
ce n
umbe
r
RAcos(DEC) − K−band
500 1000 1500 20000
20
40
60
80
100
120
140DEC − K−band
Source standard deviation (µas)
Sour
ce n
umbe
r
500 1000 1500 20000
20
40
60
80
100
120
140
Source standard deviation (µas)
Sour
ce n
umbe
r
RAcos(DEC) − S/X−band
500 1000 1500 20000
20
40
60
80
100
120
140DEC − S/X−band
Source standard deviation (µas)
Sour
ce n
umbe
r
100 200 300 400 5000
10
20
30
40
50
60RAcos(DEC) − K−band
Source noise floor (µas)
Sour
ce n
umbe
r
100 200 300 400 5000
10
20
30
40
50
60DEC − K−band
Source noise floor (µas)
Sour
ce n
umbe
r
100 200 300 400 5000
10
20
30
40
50
60RAcos(DEC) − S/X−band
Source noise floor (µas)
Sour
ce n
umbe
r
100 200 300 400 5000
10
20
30
40
50
60DEC − S/X−band
Source noise floor (µas)
Sour
ce n
umbe
r
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Comparison 1/3 310 common sources – Period 1979-now
Noisefloorcomparisonin
10odeclinaUonbands
8/16
−80 −60 −40 −20 0 20 40 60 800
100
200
300
400
500
Declination (deg)So
urce
noi
se fl
oor (µ
as) RAcos(DEC)
S/X noise floorK noise floor
−80 −60 −40 −20 0 20 40 60 800
100
200
300
400
500
Declination (deg)
Sour
ce n
oise
floo
r (µ
as) DEC
S/X noise floorK noise floor
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Comparison 2/3 87 common sources – Period 11/2016-11/2018
FocusonsameperiodofobservaUon:
November2016toNovember2018.
9/16
1980 1985 1990 1995 2000 2005 2010 2015
S/X sessionsK sessions
Ksolu'on S/Xsolu'on
Source# 901 4728
Session# 44 391
Source#(≥10sessions) 254 431
87commonsources
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Comparison 2/3 87 common sources – Period 11/2016-11/2018
10/16
2016.5 2017 2017.5 2018 2018.5 2019 2019.5−1
−0.5
0
0.5
1
RAcosDEC (mas) 0552+398
S/X Standard dev: 0.347 K Standard dev: 0.158
S/XK
2016.5 2017 2017.5 2018 2018.5 2019 2019.5−1
−0.5
0
0.5
1
DEC (mas) 0552+398
S/X Standard dev: 0.693 K Standard dev: 0.205
S/XK
2016.5 2017 2017.5 2018 2018.5 2019 2019.5−1
−0.5
0
0.5
1
RAcosDEC (mas) 3C120
S/X Standard dev: 0.319 K Standard dev: 0.183
S/XK
2016.5 2017 2017.5 2018 2018.5 2019 2019.5−1
−0.5
0
0.5
1
DEC (mas) 3C120
S/X Standard dev: 0.689 K Standard dev: 0.220
S/XK
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Comparison 2/3 87 common sources – Period 11/2016-11/2018
TheS/XnoisefloorstendtobesmallerthantheKnoisefloors.
11/16
500 1000 1500 20000
5
10
15
20
25
30
35
40
Source standard deviation (µas)
Sour
ce n
umbe
r
RAcos(DEC) − K−band
500 1000 1500 20000
5
10
15
20
25
30
35
40DEC − K−band
Source standard deviation (µas)
Sour
ce n
umbe
r
500 1000 1500 20000
5
10
15
20
25
30
35
40
Source standard deviation (µas)So
urce
num
ber
RAcos(DEC) − S/X−band
500 1000 1500 20000
5
10
15
20
25
30
35
40DEC − S/X−band
Source standard deviation (µas)
Sour
ce n
umbe
r
100 200 300 400 5000
5
10
15
20RAcos(DEC) − K−band
Source noise floor (µas)
Sour
ce n
umbe
r
100 200 300 400 5000
5
10
15
20DEC − K−band
Source noise floor (µas)
Sour
ce n
umbe
r
100 200 300 400 5000
5
10
15
20RAcos(DEC) − S/X−band
Source noise floor (µas)
Sour
ce n
umbe
r
100 200 300 400 5000
5
10
15
20DEC − S/X−band
Source noise floor (µas)
Sour
ce n
umbe
r
StandarddeviaUonNoisefloordeterminedby
theAllanvariance
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Comparison 2/3 87 common sources – Period 11/2016-11/2018
12/16
−80 −60 −40 −20 0 20 40 60 800
100
200
300
400
500
Declination (deg)So
urce
noi
se fl
oor (µ
as) RAcos(DEC)
S/X noise floorK noise floor
−80 −60 −40 −20 0 20 40 60 800
100
200
300
400
500
Declination (deg)
Sour
ce n
oise
floo
r (µ
as) DEC
S/X noise floorK noise floor
Noisefloorcomparisonin
10odeclinaUonbands
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Comparison 3/3 31 common sources - VLBA sessions
• UDsessions:24-hourVLBAsessionsatK-band.• UF001andUG002sessions:24-hourVLBAsessionsatS/Xband.Goals:improvingtheprecisionofICRF3,ICRF3maintenance,andfutureupdatesoftheICRFatradiofrequencies.Approximately3300oftheweakestICRF3sourceswillbere-observedduringthesesessions.
13/16
Ksolu'on S/Xsolu'on
Source# 819 4145
Session# 27 40
Source#(≥10sessions)
149 132
2016.5 2017 2017.5 2018 2018.5 2019 2019.5−1
−0.5
0
0.5
1
RAcosDEC (mas) 0552+398
S/X Standard dev: 0.214 K Standard dev: 0.150
S/XK
2016.5 2017 2017.5 2018 2018.5 2019 2019.5−1
−0.5
0
0.5
1
DEC (mas) 0552+398
S/X Standard dev: 0.209 K Standard dev: 0.209
S/XK
31commonsources
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Comparison 3/3 31 common sources - VLBA sessions
TheKnoisefloorsandtheS/Xnoisefloorsseemtobeequivalent.
14/16
500 1000 1500 20000
5
10
15
Source standard deviation (µas)
Sour
ce n
umbe
r
RAcos(DEC) − K
500 1000 1500 20000
5
10
15DEC − K−band
Source standard deviation (µas)
Sour
ce n
umbe
r
500 1000 1500 20000
5
10
15
Source standard deviation (µas)
Sour
ce n
umbe
r
RAcos(DEC) − S/X−band
500 1000 1500 20000
5
10
15DEC − S/X−band
Source standard deviation (µas)
Sour
ce n
umbe
r
100 200 300 400 5000
5
10
15RAcos(DEC) − K−band
Source noise floor (µas)
Sour
ce n
umbe
r
100 200 300 400 5000
5
10
15DEC − K−band
Source noise floor (µas)
Sour
ce n
umbe
r
100 200 300 400 5000
5
10
15RAcos(DEC) − S/X−band
Source noise floor (µas)
Sour
ce n
umbe
r
100 200 300 400 5000
5
10
15DEC − S/X−band
Source noise floor (µas)
Sour
ce n
umbe
r
StandarddeviaUonNoisefloordeterminedby
theAllanvariance
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Comparison 3/3 31 common sources - VLBA sessions
15/16
−80 −60 −40 −20 0 20 40 60 800
100
200
300
400
500
Declination (deg)So
urce
noi
se fl
oor (µ
as) RAcos(DEC)
S/X noise floorK noise floor
−80 −60 −40 −20 0 20 40 60 800
100
200
300
400
500
Declination (deg)
Sour
ce n
oise
floo
r (µ
as) DEC
S/X noise floorK noise floor
Noisefloorcomparisonin
10odeclinaUonbands
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Conclusions
• K-bandUmestability• TheK-bandobservaUonshavereachedalevelofstabilityequivalenttothelevelofcurrentS/XobservaUons.
• ThestrengthoftheS/Xdatasetisinitsbroaddiversityofbaselinesandsessions.
• WeneedtoconUnuemonitoringtheK-bandobservaUonsandcomparingthestabilityoftheframerealizedbytheK-bandobservaUonswiththeS/Xframe.
16/16
• ThankstotheVLBA,K-bandobservaUonshaveincreasedgreatlyinthepasttwoyears,prompUngmanystudies.Atthe2019EVGA:
• BenediktSoja:“IonosphericcalibraUonforK-bandcelesUalreferenceframes”.• HanaKrásná:“EarthorientaUonparametersesUmatedfromK-bandVLBA
measurements”.• AlethadeWi1:“TheK-band(24GHz)CelesUalReferenceFrame”.
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Thank you
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
And more…
Structure,propermoUon?
1980 1985 1990 1995 2000 2005 2010 2015 2020−1
−0.5
0
0.5
1
RAcosDEC (mas) 3C418
S/X Standard dev: 0.732 K Standard dev: 0.191
S/XK
1980 1985 1990 1995 2000 2005 2010 2015 2020−1
−0.5
0
0.5
1
DEC (mas) 3C418
S/X Standard dev: 0.853 K Standard dev: 0.227
S/XK
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain
Noise floor comparison Individual sources
StandarddeviaUon
0 500 1000 1500 20000
500
1000
1500
2000
RAcos(DEC)
S/X source standard deviation (µas)
K so
urce
sta
ndar
d de
viat
ion
(µas
)
0 500 1000 1500 20000
500
1000
1500
2000
DEC
S/X source standard deviation (µas)
K so
urce
sta
ndar
d de
viat
ion
(µas
)
0 100 200 300 400 5000
100
200
300
400
500
RAcos(DEC)
S/X source noise floor (µas)
K so
urce
noi
se fl
oor (µ
as)
0 100 200 300 400 5000
100
200
300
400
500
DEC
S/X source noise floor (µas)
K so
urce
noi
se fl
oor (µ
as)
0 100 200 300 400 5000
100
200
300
400
500
RAcos(DEC)
S/X source noise floor (µas)
K so
urce
noi
se fl
oor (µ
as)
0 100 200 300 400 5000
100
200
300
400
500
DEC
S/X source noise floor (µas)
K so
urce
noi
se fl
oor (µ
as)
0 500 1000 1500 20000
500
1000
1500
2000
RAcos(DEC)
S/X source standard deviation (µas)
K so
urce
sta
ndar
d de
viat
ion
(µas
)
0 500 1000 1500 20000
500
1000
1500
2000
DEC
S/X source standard deviation (µas)
K so
urce
sta
ndar
d de
viat
ion
(µas
)
0 500 1000 1500 20000
500
1000
1500
2000
RAcos(DEC)
S/X source standard deviation (µas)
K so
urce
sta
ndar
d de
viat
ion
(µas
)
0 500 1000 1500 20000
500
1000
1500
2000
DEC
S/X source standard deviation (µas)
K so
urce
sta
ndar
d de
viat
ion
(µas
)
NoisefloordeterminedbytheAllanvariance
0 100 200 300 400 5000
100
200
300
400
500
RAcos(DEC)
S/X source noise floor (µas)
K so
urce
noi
se fl
oor (µ
as)
0 100 200 300 400 5000
100
200
300
400
500
DEC
S/X source noise floor (µas)
K so
urce
noi
se fl
oor (µ
as)
(157
/142
sou
rces)
En'reperiod
(310
sou
rces)
(74sources)
2-yrpe
riod
(87sources)
(24/28
sou
rces)
VLBAsession
s(3
1sources)
24thMeeUngoftheEuropeanVLBIGroupforGeodesyandAstrometry(EVGA)March17-192019,LasPalmas,GranCanaria,Spain