ANNAPOLIS

Station summaryLOYF

Showing all stations within 1000 km of the observed station Active station No data for 30 days Decommissioned No observations in SONEL (Survey) Not co-located with observed station
Showing all stations within 1000 km of the observed station Available data / Station OK Available data / Problem(s) detected Does not work No longer exists Foreign partner management Not co-located with observed station
Showing all stations within 1000 km of the observed station Co-located with observed station Not co-located with observed station
  • More informations on each symbol.
  • GPS
    Tide Gauge
    DORIS
IGS-type acronym : LOYF
Latitude : 38.97447200
Longitude : -76.52219400
Installed date : 2006-03-16
Decommissioned date :
Country : U.S.A.
City : ANNAPOLIS
Station status : active (green)
Distance to Tide Gauge (m) : 3790
Domes Nr.: 49261M001
Station operator: (SMRTNT) - SmartNet North America
IGS-like station form :

GPS position times seriesLOYF



Position
(Reference epoch: )




Offsets (mm)
MMaterial change or malfunction
EEarthquake
RFReference Frame change
UUnknown
NANot available
Position discontinuity
Velocity discontinuity
     
   
Vertical component
   
East component
   
North Component


Data available at SONELLOYF



Quality plots on RINEX filesLOYF

Quality plots on RINEX files of LOYF Quality plots on RINEX files of LOYF Royal Observatory of Belgium

Plots generated using software developed with the EPN team at ROB
Observations & tracking performance Satellite tracking

informations (this operation may take 20 to 45s)

The satellite tracking graph has been calculated for all stations for the first day of each month. If you wish to have a graph for another date, choose the 'Calculate a specific date' option.

Comparison with satellite altimetry data

Co-located instrumentsLOYF

Photo albumLOYF

BibliographyLOYF

If you have a relevant reference to suggest, please send-us an e-mail : sonel@sonel.org
  • puce Ezer, Corlett, 2012. Is sea level rise accelerating in the Chesapeake Bay? A demonstration of a novel new approach for analyzing sea level data. Geophysical Research Letters. Get this reference
  • puce Ezer, 2013. Sea level rise, spatially uneven and temporally unsteady: Why the U.S. East Coast, the global tide gauge record, and the global altimeter data show different trends. Geophysical Research Letters. Get this reference