|
|
|
|
St. John's Magnetic Observatory
Metadata from the NOAA Metadata Manager's Repository (NMMR)
- Identification_Information:
-
- Citation:
-
- Citation_Information:
-
- Originator:Geological Survey of Canada
- Publication_Date:1968
- Title:
- St. John's Magnetic Observatory
- Online_Linkage:http://www.geolab.nrcan.gc.ca
- Description:
-
- Abstract:
The St. John's Geomagnetic Observatory began operation on 1 August, 1968. A location in southeastern Newfoundland was chosen
to reduce one of the largest gaps in the geographical distribution of magnetic observatories in North America. In addition
to contributing data for studies of worldwide geomagnetic variations and secular change, the St. John's Observatory provides
control for the marine and airborne geomagnetic surveys conducted over the broad continental shelf east of Canada.
The initial St. John's Observatory occupied a site 3 km northeast of the centre of the city, in the White Hills area, and
was approximately 1.5 km from the sea. The area is magnetically flat and the total intensity varied by less than 15 nT within
the initial site. A preliminary survey of geomagnetic time variations throughout Newfoundland revealed no gross electromagnetic
induction anomalies in the St. John's region but some coastal induction effect must be expected and has in fact been found.
1968 Observatory:
There were two non-magnetic buildings 100 m apart. The site was enclosed by an aluminum fence, segmented to avoid the disruption
of the natural earth currents.
One building was used both for the variometers and for absolute observations. It was 13 m long and 6.5 m wide, with the long
axis magnetic north-south (1968), and was supported by concrete resting on the bedrock. It was of wooden construction, well
insulated and covered with enamelled aluminum siding. Two reinforced and insulated concrete slabs, isolated from the walls
of the building and from each other, provided support for the absolute instrument piers and the fluxgate magnetometer sensor,
and for the photographic variometer tables respectively. Two insulated light-tight rooms enclosed the photographic instruments.
The second building, about 8 m square, was of similar non- magnetic construction. It included an office, darkroom and laboratory
in which the magnetic field was sufficiently undisturbed to have permitted the operation of many types of magnetometers.
The buildings were connected by underground ducts carrying electrical power, signal and communication cables.
The initial recording instrumentation consisted of a set of standard run RUSKA photographic variometers, a portable ASKANIA
photographic variometer and a three component fluxgate magnetometer registering on an analogue paper chart recorder. St.
John's was the first Canadian observatory to have a production run AMOS Mk I installed. Routine operation of the AMOS Mk I
began in December, 1969
1975 Observatory:
Following a decision of the Department of the Environment to construct a new office and laboratory complex, the New foundland
Environment Institute, on Crown Land previously reserved for the Observatory, an agreement was reached whereby DOE would relocate
the recording building 100 to 125 m to the northeast. This would ensure that the recordings of the magnetic variations would
not be subject to interference from traffic on the access road leading to the new Institute. A total force survey in August,
1974 revealed no significant field gradients or anomalies within the proposed observatory site. Tenders for a new magnetic
observatory building were called in April, 1975. The new building, having the same specifications as the 1968 13 m by 6.5
m building, was completed in December, 1975.
The aging AMOS Mk I was replaced by the AMOS Mk III in mid- March, 1981.
1990 Observatory:
Official notification by Public Works Canada (Atlantic Region) to the Earth Physics Branch indicated that the St. John's Observatory
site was under considerable pressure for it to be developed for other Federal Government departments. As a result of discussions
with Public Works during the summer of 1985, preliminary plans were formulated in order to move St. John's Observatory elsewhere
in Newfoundland. A number of prospective sites were examined in the following 3 years but were found to be unsuitable for
various reasons. In early 1988 the decision was made to move the Observatory an additional 500+ m back towards the northeast
into the undeveloped White Hills Crown Land reserve. Site preparation and building construction were completed by the summer
of 1989.
The Observatory presently consists of a scattering of sensor huts and instrument buildings, all separated from each other
by at least 30 m. Two 3 m by 5 m buildings of non-magnetic construction house the electronics racks and the absolute observation
pier respectively. Five other prefabricated shelters house the various sensors and also serve as additional storage.
Contrary to the usual detrimental effect of new construction on the local avifauna, a biological impact analysis by LeDrew
Environmental Management Lt. showed a probable enhanced environment for the migratory snowy owls. Snowy owls nest in the
White Hills area from fall to spring. Although the decrease in surface vegetation is probably appreciated by the snowy owls,
it is most likely not looked upon with such enthusiasm by the local mice and shrew population. The third St. John's Observatory
was placed in service in January, 1990 with the installation of the Geological Survey of Canada's prototype CANMOS. A fully
INTERMAGNET compliant CANMOS was installed in March, 1991.
- Purpose:
To provide ground-based, calibrated values of the Earth's magnetic field at a specific location for scientific research and
practical applications.
- Supplemental_Information:
Elevation: 100 meters
- Time_Period_of_Content:
-
- Time_Period_Information:
-
- Range_of_Dates/Times:
-
- Beginning_Date:1968
- Ending_Date:Present
- Currentness_Reference:
ground condition
- Status:
-
- Progress:In work
- Maintenance_and_Update_Frequency:Irregular
- Spatial_Domain:
-
- Bounding_Coordinates:
-
- West_Bounding_Coordinate:-64.27
- East_Bounding_Coordinate:-64.27
- North_Bounding_Coordinate:52.68
- South_Bounding_Coordinate:52.68
- Keywords:
-
- Theme:
-
- Theme_Keyword_Thesaurus:NASA/GCMD Earth Science Keywords
- Theme_Keyword:Earth Science > Solid Earth > Geomagnetism
- Theme_Keyword:Earth Science > Solid Earth > Geomagnetism > Geomagnetic Indices
- Theme_Keyword:Earth Science > Solid Earth > Geomagnetism > Magnetic Declination
- Theme_Keyword:Earth Science > Solid Earth > Geomagnetism > Magnetic Field
- Theme_Keyword:Earth Science > Solid Earth > Geomagnetism > Magnetic Inclination
- Theme_Keyword:Earth Science > Solid Earth > Geomagnetism > Magnetic Intensity
- Theme:
-
- Theme_Keyword_Thesaurus:ISO 19115 Topic Category
- Theme_Keyword:geoscientificInformation
- Theme_Keyword:intelligenceMilitary
- Theme_Keyword:utilitiesCommunication
- Theme_Keyword:climatologyMeteorologyAtmosphere
- Theme:
-
- Theme_Keyword_Thesaurus:INTERMAGNET
- Theme_Keyword:Magnetic Observatory Definitive Data
- Access_Constraints:None
- Point_of_Contact:
-
- Contact_Information:
-
- Contact_Organization_Primary:
-
- Contact_Organization:Geological Survey of Canada
- Contact_Person:L. McKee
- Contact_Address:
-
- Address_Type:mailing
- Address:
7-Observatory Crescent
- Address:
Contact institute
- City:Newfoundland
- State_or_Province:Ottawa
- Postal_Code:K1A 0Y3
- Country:Canada
- Contact_Voice_Telephone:613-837-9158
- Contact_Facsimile_Telephone:613-824-9803
- Contact_Electronic_Mail_Address:Lmckee@NRCan.ca
Back to Top
- Data_Quality_Information:
-
- Attribute_Accuracy:
-
- Attribute_Accuracy_Report:
Data from the St. John's Magnetic Observatory Magnetic Observatory met the requirements for being an INTERMAGNET Magnetic
Observatory (IMO), and as such met the specifications listed in the INTERMAGNET Technical Manual (http://www.intermagnet.org//im_manual.pdf)
- Quantitative_Attribute_Accuracy_Assessment:
-
- Attribute_Accuracy_Value:Full field
- Attribute_Accuracy_Explanation:
Dynamic Range
- Quantitative_Attribute_Accuracy_Assessment:
-
- Attribute_Accuracy_Value:0.025 nT
- Attribute_Accuracy_Explanation:
Resolution
- Quantitative_Attribute_Accuracy_Assessment:
-
- Attribute_Accuracy_Value:8 Hz reduced by a boxcar filter to 1second data; 1 second data reduced to 5 second data
- Attribute_Accuracy_Explanation:
Sampling Rate
- Quantitative_Attribute_Accuracy_Assessment:
-
- Attribute_Accuracy_Value:19 point Gaussian filter for the production of 1 minute data from 5 second data
- Attribute_Accuracy_Explanation:
Numeric Filter
- Logical_Consistency_Report:
Contact institution
- Completeness_Report:
These data represent the complete record set for this station and this time period.
- Lineage:
-
- Process_Step:
-
- Process_Description:
Contact institute
- Source_Used_Citation_Abbreviation:
- Unknown
- Process_Date:Unknown
Back to Top
- Entity_and_Attribute_Information:
-
- Detailed_Description:
-
- Entity_Type:
-
- Entity_Type_Label:Magnetometer
- Entity_Type_Definition:
- A scientific instrument for measuring the strength of magnetic fields.
- Entity_Type_Definition_Source:
- http://en.wikipedia.org/wiki/Magnetometer
- Attribute:
-
- Attribute_Label:fluxgate magnetometer
- Attribute_Definition:
A kind of magnetometer that detects second harmonic signals from a secondary coil surrounding an iron core that is driven
into saturation by a primary coil using radio frequency signals. The second harmonic signal is proportional to the strength
of the ambient magnetic field.
- Attribute_Definition_Source:
http://www.earthsci.unimelb.edu.au/ES304/MODULES/MAG/NOTES/fluxgate.html
- Attribute_Domain_Values:
-
- Unrepresentable_Domain:
- This is a type of magnetometer instrument used for measuring the Magnetic Field
- Attribute:
-
- Attribute_Label:proton precession magnetometer
- Attribute_Definition:
A kind of scalar magnetometer that measures only the strength of the total magnetic field vector and not its direction or
components. A hydrogen-rich fluid is polarized using a strong electric current. When the current is turned off, the protons
in the fluid precess around the ambient magnetic field at a frequency given by the gyromagnetic ratio and proportional to
the strength of the surrounding magnetic field.
- Attribute_Definition_Source:
http://en.wikipedia.org/wiki/Magnetometer#Scalar_magnetometers
- Attribute_Domain_Values:
-
- Unrepresentable_Domain:
- This is a type of magnetometer instrument used for measuring the Magnetic Field
- Attribute:
-
- Attribute_Label:Overhauser magnetometer
- Attribute_Definition:
A type of scalar magnetometer that employs the precession of free unpaired electrons rather than protons in a fluid.
- Attribute_Definition_Source:
http://en.wikipedia.org/wiki/Magnetometer#Scalar_magnetometers
- Attribute_Domain_Values:
-
- Unrepresentable_Domain:
- This is a type of magnetometer instrument used for measuring the Magnetic Field
- Detailed_Description:
-
- Entity_Type:
-
- Entity_Type_Label:Earth's Magnetic Field Components
- Entity_Type_Definition:
- The Earth's magnetic field is characterized by a direction and intensity which can be determined by various combinations of
three of seven possible magnetic field components.
- Entity_Type_Definition_Source:
- Wienert, K.A., Notes on geomagnetic observatory and survey practice, UNESCO Earth Sciences 5, 1970.
- Attribute:
-
- Attribute_Label:Inclination (I)
- Attribute_Definition:
The angle which the line of force at a point of observation makes with the horizontal plane, positive when directed downward
- Attribute_Definition_Source:
Wienert, K.A., Notes on geomagnetic observatory and survey practice, UNESCO Earth Sciences 5, 1971
- Attribute_Domain_Values:
-
- Range_Domain:
-
- Range_Domain_Minimum:-90.0
- Range_Domain_Maximum:90.0
- Attribute_Units_of_Measure:Decimal Degrees or Degrees and Decimal Minutes
- Attribute:
-
- Attribute_Label:Declination (D)
- Attribute_Definition:
The angle made by the magnetic meridian and the true north meridian, considered positive east of north and negative west of
north
- Attribute_Definition_Source:
Wienert, K.A., Notes on geomagnetic observatory and survey practice, UNESCO Earth Sciences 5, 1971
- Attribute_Domain_Values:
-
- Range_Domain:
-
- Range_Domain_Minimum:-180.0
- Range_Domain_Maximum:180.0
- Attribute_Units_of_Measure:Decimal Degrees or Degrees and Decimal Minutes
- Attribute:
-
- Attribute_Label:Horizontal Intensity (H)
- Attribute_Definition:
The projection of the geomagnetic field vector on the horizontal plane, always positive
- Attribute_Definition_Source:
Wienert, K.A., Notes on geomagnetic observatory and survey practice, UNESCO Earth Sciences 5, 1971
- Attribute_Domain_Values:
-
- Range_Domain:
-
- Range_Domain_Minimum:0
- Range_Domain_Maximum:40000.0
- Attribute_Units_of_Measure:nanotesla
- Attribute:
-
- Attribute_Label:Vertical Intensity (Z)
- Attribute_Definition:
The projection of the geomagnetic field vector on the vertical plane, positive when directed down
- Attribute_Definition_Source:
Wienert, K.A., Notes on geomagnetic observatory and survey practice, UNESCO Earth Sciences 5, 1971
- Attribute_Domain_Values:
-
- Range_Domain:
-
- Range_Domain_Minimum:-70000.0
- Range_Domain_Maximum:60000.0
- Attribute_Units_of_Measure:nanotesla
- Attribute:
-
- Attribute_Label:Total Intensity (F)
- Attribute_Definition:
The scalar magnitude of the geomagnetic field vector, always positive
- Attribute_Definition_Source:
Wienert, K.A., Notes on geomagnetic observatory and survey practice, UNESCO Earth Sciences 5, 1971
- Attribute_Domain_Values:
-
- Range_Domain:
-
- Range_Domain_Minimum:25000.0
- Range_Domain_Maximum:80000.0
- Attribute_Units_of_Measure:nanotesla
- Attribute:
-
- Attribute_Label:North Component (X)
- Attribute_Definition:
The projection of the horizontal component (H) in the true meridian
- Attribute_Definition_Source:
Wienert, K.A., Notes on geomagnetic observatory and survey practice, UNESCO Earth Sciences 5, 1971
- Attribute_Domain_Values:
-
- Range_Domain:
-
- Range_Domain_Minimum:-10000.0
- Range_Domain_Maximum:45000.0
- Attribute_Units_of_Measure:nanotesla
- Attribute:
-
- Attribute_Label:East Component (Y)
- Attribute_Definition:
The projection of the horizontal component on the true east direction, positive when directed eastward
- Attribute_Definition_Source:
Wienert, K.A., Notes on geomagnetic observatory and survey practice, UNESCO Earth Sciences 5, 1971
- Attribute_Domain_Values:
-
- Range_Domain:
-
- Range_Domain_Minimum:-20000.0
- Range_Domain_Maximum:20000.0
- Attribute_Units_of_Measure:nanotesla
- Detailed_Description:
-
- Entity_Type:
-
- Entity_Type_Label:Geographic Location
- Entity_Type_Definition:
- A coordinate system that provides a means for expressing every location on the Earth using three coordinates of a spherical
coordinate system which is aligned with the spin axis of the Earth.
- Entity_Type_Definition_Source:
- http://en.wikipedia.org/wiki/Geographic_location
- Attribute:
-
- Attribute_Label:Latitude
- Attribute_Definition:
Latitude is an angular measurement in degrees that gives the location of a place on the Earth above (toward the North pole)
or below (toward the South pole) of the equator.
- Attribute_Definition_Source:
http://en.wikipedia.org/wiki/Latitude
- Attribute_Domain_Values:
-
- Range_Domain:
-
- Range_Domain_Minimum:-90
- Range_Domain_Maximum:+90
- Attribute_Units_of_Measure:angular degrees
- Attribute:
-
- Attribute_Label:Longitude
- Attribute_Definition:
Longitude is an angluar measurement in degrees that describes the location of a place on the Earth east or west of a north-south
line called the Prime Meridian.
- Attribute_Definition_Source:
http://en.wikipedia.org/wiki/Longitude
- Attribute_Domain_Values:
-
- Range_Domain:
-
- Range_Domain_Minimum:-180
- Range_Domain_Maximum:+180
- Attribute_Units_of_Measure:angular degrees
- Attribute:
-
- Attribute_Label:Elevation
- Attribute_Definition:
Elevation is the vertical position of a location relative to some height above the Earth's surface, generally taken as the
mean sea level or geoid.
- Attribute_Definition_Source:
http://en.wikipedia.org/wiki/Geoid
- Attribute_Domain_Values:
-
- Range_Domain:
-
- Range_Domain_Minimum:0
- Range_Domain_Maximum:unlimited
- Attribute_Units_of_Measure:meters
Back to Top
- Distribution_Information:
-
- Distributor:
-
- Contact_Information:
-
- Contact_Organization_Primary:
-
- Contact_Organization:DOC/NOAA/NESDIS/NGDC > National Geophysical Data Center, NESDIS, NOAA, U.S. Department of Commerce
- Contact_Person:David Fischman
- Contact_Position:Data Manager
- Contact_Address:
-
- Address_Type:mailing and physical
- City:Boulder
- State_or_Province:CO
- Postal_Code:80303
- Country:USA
- Contact_Voice_Telephone:303 497-4654
- Contact_Facsimile_Telephone:303-497-6513
- Contact_Electronic_Mail_Address:david.fischman@noaa.gov
- Hours_of_Service:8:00 - 5:00 Mountain
- Distribution_Liability:
While every effort has been made to ensure that these data are accurate and reliable within the limits of the current state
of the art, NOAA cannot assume liability for any damages caused by any errors or omissions in the data, nor as a result of
the failure of the data to function on a particular system. NOAA makes no warranty, expressed or implied, nor does the fact
of distribution constitute such a warranty.
- Standard_Order_Process:
-
- Digital_Form:
-
- Digital_Transfer_Information:
-
- Format_Name:IAGA2002
- Format_Version_Date:2001
- Format_Specification:
http://www.ngdc.noaa.gov/IAGA/vdat/iagaformat.html
- Format_Information_Content:
Columnar ASCII values including date, time, and magnetic field values, including header information pertinate to the individual
observatory.
- File_Decompression_Technique:generally ZIP
- Digital_Transfer_Option:
-
- Online_Option:
-
- Computer_Contact_Information:
-
- Network_Address:
-
- Network_Resource_Name:http://www.ngdc.noaa.gov/IAGA/vdat/iagaformat.html
- Digital_Form:
-
- Digital_Transfer_Information:
-
- Format_Name:WDC-A
- Digital_Transfer_Option:
-
- Online_Option:
-
- Computer_Contact_Information:
-
- Network_Address:
-
- Network_Resource_Name:www.wdcb.ru/stp/data/geo_min.val/AIA-Argentine%20Islands/DIGITAL%20WDC%20FORMATS.doc
- Access_Instructions:
- This is an outdated ASCII format.
- Fees:None
- Ordering_Instructions:
Contact NGDC for instructions.
Back to Top
- Metadata_Reference_Information:
-
- Metadata_Date:
- Metadata_Contact:
-
- Contact_Information:
-
- Contact_Organization_Primary:
-
- Contact_Organization:DOC/NOAA/NESDIS/NGDC > National Geophysical Data Center, NESDIS, NOAA, U.S. Department of Commerce
- Contact_Person:David Fischman
- Contact_Position:Data Manager
- Contact_Address:
-
- Address_Type:mailing and physical
- City:Boulder
- State_or_Province:CO
- Postal_Code:80303
- Country:USA
- Contact_Voice_Telephone:303 497-4654
- Contact_Facsimile_Telephone:303-497-6513
- Contact_Electronic_Mail_Address:david.fischman@noaa.gov
- Hours_of_Service:8:00 - 5:00 Mountain
- Metadata_Standard_Name:Content Standard for Digital Geospatial Metadata: Extensions for Remote Sensing Metadata
- Metadata_Standard_Version:FGDC-STD-012-2002
- Metadata_Extensions:
-
- Online_Linkage:http://www.ngdc.noaa.gov/metadata/extensions/local_extensions.html
- Profile_Name:NGDC Extensions to FGDC Metadata
Back to Top
Metadata stylesheets are provided courtesy of ESRI. Copyright (c) 2000-2002, Environmental Systems Research Institute, Inc.
All rights reserved.
|
|
|
Discussion Comment on, report a problem with, or make a suggestion about this item. An administrator will see what you have written and a reply will appear here (if appropriate) and a you will be i-mailed
|
|
|
Publication Info
|
Usage Statistics
|
|
|
| This page has been edited: | 0 time(s)
|
| This page was viewed: | 383 time(s)
|
| This page is bookmarked by: | 0 user(s)
|
|
|
|
|