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National Report of Sweden to the NKG General ... - Lantmäteriet

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17comparison and evaluation <strong>of</strong>frequency transfer with VLBI andGNSS. Our results show that geodeticVLBI can reach frequency transferstability <strong>of</strong> 1e-15 during one day, andthat this is in good agreement withGNSS-based techniques.We use <strong>the</strong> global geodetic VLBI dataset <strong>to</strong> derive long time series <strong>of</strong>tropospheric zenith wet delay (ZWD)and atmospheric gradient values. ForOnsala, <strong>the</strong>se time series cover morethan 25 years. The ZWD can beconverted in<strong>to</strong> information on <strong>the</strong>integrated water vapour content(IPWV) and compared <strong>to</strong>independently derived IPWV resultsfrom a ground based microwaveradiometer operated at Onsala andradiosonde observations from <strong>the</strong>Landvetter-Go<strong>the</strong>nburg airport. Figure3.2 shows <strong>the</strong> corresponding timeseries.Figure 3.2: Time series <strong>of</strong> integratedprecipitable water vapor (IPWV) asdetermined from geodetic VLBI dataobserved at Onsala (VLBI, <strong>to</strong>p) microwaveradiometry at Onsala (WVR, middle) andradiosondes at Go<strong>the</strong>nburg-Landvetter (RS,bot<strong>to</strong>m).<strong>the</strong> order <strong>of</strong> 0.4 <strong>to</strong> 0.6 kg/m2 perdecade. However, <strong>the</strong> agreement is notperfect. A major problem in <strong>the</strong>comparison is <strong>the</strong> different sampling <strong>of</strong><strong>the</strong> three data sets and <strong>the</strong> individualdata gaps. Synchronization <strong>of</strong> <strong>the</strong> datasets results in small biases on <strong>the</strong> order<strong>of</strong> 1 kg/m2 and root-mean-square(RMS) differences <strong>of</strong> less than 2 kg/m2,but does not improve <strong>the</strong> agreement <strong>of</strong><strong>the</strong> trends.3.3 Super-conducting gravimetryOn June 10 2009, a super-conductinggravimeter (SCG, series number GWR-054) was taken in<strong>to</strong> operation at <strong>the</strong>Onsala Space Observa<strong>to</strong>ry. The mainuse <strong>of</strong> <strong>the</strong> new facility is providing acalibrated gravity station for visitinggroups within absolute gravity projectsaiming e.g. at determining gravitychanges in <strong>the</strong> Nordic countries inconnection with GIA. The newgravimeter station provides us with <strong>the</strong>"third pillar" <strong>of</strong> geodesy, i.e. gravityand geopotential measurement,complementing our contributions <strong>the</strong>o<strong>the</strong>r two pillars, earth rotation andearth deformation. This developmenthas now raised Onsala <strong>to</strong> <strong>the</strong> status <strong>of</strong> aFundamental Geodetic Station, a corestations for <strong>the</strong> maintenance <strong>of</strong> <strong>the</strong>International Reference System. Figure3.3. presents <strong>the</strong> gravimeter record forslightly more than one year. Severalexternal research groups with absolutegravimeters have been visiting Onsalasince mid 2009 <strong>to</strong> do parallelmeasurements with <strong>the</strong> newinstrument.The IPWV data derived from <strong>the</strong>individual techniques show highcorrelation with correlation coefficients<strong>of</strong> 0.95 and better. All three techniquesshow positive trends for <strong>the</strong> IPWV on

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