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Determining the accurate positions of Japan The earth’s shapes, latitudes and longitudes have been defined in accordance with the International Terrestrial Reference Frame (ITRF) which is constructed and maintained through global geodetic observations and international cooperation and coordination. In accordance with the ITRF, GSI determines the positions of the Japanese archipelago through VLBI *1 observations and the locations of GNSS *2 CORSs and triangulation stations on the land through GNSS observations. Results of these activities are compiled and publicized for utilization as basic information which is indispensable for identification, management and security of the nation’s territories. *1 VLBI (Very Long Baseline Interferometry): A technique to measure the distance between two or more parabolic antennas over thousands of km with a-few-mm accuracy, by calculating the arrival time difference of received signals radiated from celestial bodies far away in the universe. *2 GNSS (Global Navigation Satellite System): A collective term for satellite navigation systems that determine the position on the globe by using satellites, including the U.S. Global Positioning System (GPS), the Japanese Quasi-Zenith Satellite System (QZSS; known as “MICHIBIKI”), the Russian Global Navigation Satellite System (GLONASS), and EUʼs Galileo. *Declination: deviation of the indicated north (magnetic north) on a compass from the geographic north (true north). GGOS is an initiative for international collaboration for prompting the geodetic observations (VLBI, GNSS, SLR, DORIS and gravimetry) and integrating them in a global scale. The GGOS is contributing to enhancing collaboration for realizing and sustaining the ITRF. GSI has taken over the presidency of the GGOS, actively leading the lines. GGOS (Global Geodetic Observing System) Determining the accurate positions of Japan Survey VLBI Observing Facility (Ishioka Geodetic Observing Station, Ibaraki) The GNSS Continuously Operating Reference Station (GNSS CORS) is an observation facility that receives signals from such as GPS and QZSS. About 1,300 GNSS CORSs are operating in the whole area of the country. Received data are sent to the Central Analysis Center at GSI in real time to calculate precise positions of these stations. GNSS CORSs constitute an important infrastructure widely used for precise positioning in ICT construction and smart agriculture as well as land surveying and crust monitoring. Leveling GNSS CORS Leveling is a surveying technique for determining elevations. Two leveling rods are vertically placed, one at a point of known elevation and the other at an unknown point. By adding the difference in scale reading between these rods to the elevation of the known point, the elevation of the unknown point is obtained. This process is successively applied to determine elevations at arbitrary points. The elevations of benchmarks, used as references for determin- ing the elevations in each area of Japan, are determined through leveling starting from the Origin of the Japanese Verti- cal Control Network, whose elevation is defined in reference to the mean sea surface (elevation 0 m) of Tokyo Bay. Repeated leveling allows us to know the accurate temporal changes in elevations, and its results are also used as basic data for disaster miti- gation. Geomagnetic surveys It is known that the geomagnetic bearing and scale depends on the location and vary with time. Geomagnetic surveys are conducted to identify the geographic distribution and chronological variation of geomagnetic fields. Data obtained at the Geodetic Observatory on Mt. Kanozan show that the rate of change in declination* started to increase after 2010. Results of geomagnetic surveys are precious data for com- pass users (climbers and smartphone users). They are also used for monitoring volcanic activities and choosing aircraft routes. Maintaining of control points on remote islands Japan has many remote islands. GSI has constructed control points (tri- angulation points) on such islands and determined their latitudes, longitudes and elevations to identify and secure the Japan’ s territo- ries. Gravity surveys GSI conducts gravity surveys at domestic gravity points and adapts and publicizes the results to the international standards. Values of gravity are required for deter- mining accurate ele- vations and are widely used for exploration of underground active faults and resources and calibration of measuring instru- ments. 04 03 ITRF, Geodetic Stations and Control Points in Japan 7.6 7.0 6.4 1990 2000 2020 2010 Declination Magnetic north on westside [deg] (westside: +; eastside: -) Variation of declination at the Geodetic Observatory on Mt. Kanozan ITRF GNSS CORS Surveys VLBI SLR GNSS DORIS GRACE Source: nasa.gov Photo:ESA Source: csr.utexas.edu Source: geod.jpn.org T. North M. North Triangulation station Central Analysis Center in Tsukuba, Ibaraki Absolute gravimeter FG5 GNSS CORS General installations for Leveling a b Origin of the Japanese Vertical Control Network Tide station Tokyo Bay mean sea level (Tokyo Peil) Elevation reference (0m) Elevation Rod Rod Level Benchmark Benchmark Elevation 24.3900 m Reconstruction of 1st order triangu- lation point on Nishinoshima Island [Year] VLBI

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Determining the accurate positions of JapanThe earth’s shapes, latitudes and longitudes have been defined in accordance with the International Terrestrial Reference Frame (ITRF) which is constructed and maintained through global geodetic observations and international cooperation and coordination. In accordance with the ITRF, GSI determines the positions of the Japanese archipelago through VLBI*1 observations and the locations of GNSS*2 CORSs and triangulation stations on the land through GNSS observations. Results of these activities are compiled and publicized for utilization as basic information which is indispensable for identification, management and security of the nation’s territories.*1 VLBI (Very Long Baseline Interferometry): A technique to measure the distance

between two or more parabolic antennas over thousands of km with a-few-mm accuracy, by calculating the arrival time difference of received signals radiated from celestial bodies far away in the universe.

*2 GNSS (Global Navigation Satellite System): A collective term for satellite navigation systems that determine the position on the globe by using satellites, including the U.S. Global Positioning System (GPS), the Japanese Quasi-Zenith Satellite System (QZSS; known as “MICHIBIKI”), the Russian Global Navigation Satellite System (GLONASS), and EUʼs Galileo.

*Declination: deviation of the indicated north (magnetic north) on a compass from the geographic north (true north).

GGOS is an initiative for international collaboration for prompting the geodetic observations (VLBI, GNSS, SLR, DORIS and gravimetry) and integrating them in a global scale. The GGOS is contributing to enhancing collaboration for realizing and sustaining the ITRF. GSI has taken over the presidency of the GGOS, actively leading the lines.

GGOS (Global Geodetic Observing System)

Determining the accuratepositions of JapanSurvey

VLBI Observing Facility (Ishioka Geodetic Observing Station, Ibaraki)

The GNSS Continuously Operating Reference Station (GNSS CORS) is an observation facility that receives signals from such as GPS and QZSS. About 1,300 GNSS CORSs are operating in the whole area of the country.Received data are sent to the Central Analysis Center at GSI in real time to calculate precise positions of these stations. GNSS CORSs constitute an important infrastructure widely used for precise positioning in ICT construction and smart agriculture as well as land surveying and crust monitoring.

● Leveling

● GNSS CORS

Leveling is a surveying technique for determining elevations. Two leveling rods are vertically placed, one at a point of known elevation and the other at an unknown point.By adding the difference in scale reading between these rods to the elevation of the known point, the elevation of the unknown point is obtained. This process is successively applied to determine elevations at arbitrary points.The elevations of benchmarks, used as references for determin-ing the elevations in each area of Japan, are determined through leveling starting from the Origin of the Japanese Verti-cal Control Network, whose elevation is defined in reference to the mean sea surface (elevation 0 m) of Tokyo Bay. Repeated leveling allows us to know the accurate temporal changes in elevations, and its results are also used as basic data for disaster miti-gation.

● Geomagnetic surveysIt is known that the geomagnetic bearing and scale depends on the location and vary with time. Geomagnetic surveys are conducted to identify the geographic distribution and chronological variation of geomagnetic fields. Data obtained at the Geodetic Observatory on Mt. Kanozan show that the rate of change in declination* started to increase after 2010. Results of geomagnetic surveys are precious data for com-pass users (climbers and smartphone users). They are also used for monitoring volcanic activities and choosing aircraft routes.

● Maintaining of control points on remote islandsJapan has many remote islands. GSI has constructed control points (tri-angulation points) on such islands and determined their latitudes, longitudes and elevations to identify and secure the Japan’ s territo-ries.

● Gravity surveysGSI conducts gravity surveys at domestic gravity points and adapts and publicizes the results to the international standards. Values of gravity are required for deter-mining accurate ele-vations and are widely used for exploration of underground active faults and resources and ca l ib ra t ion of measu r ing in s t ru -ments.

0403

ITRF, Geodetic Stations and Control Points in Japan

7.6

7.0

6.41990 2000 20202010

Declination Magnetic northon westside

[deg] (westside: +; eastside: -)

Variation of declination at the GeodeticObservatory on Mt. Kanozan

ITRF

GNSS CORS

Surveys

VLBI SLRGNSS DORISGRACESource: nasa.gov

Photo:ESASource: csr.utexas.edu

Source: geod.jpn.org T. North

M. North

Triangulation station

Central Analysis Center in Tsukuba, Ibaraki

Absolute gravimeter FG5

GNSS CORS

General installations for Leveling

a b

Origin of the JapaneseVertical Control Network

Tide station

Tokyo Baymean sea

level(Tokyo Peil) Elevation reference (0m)

Elevation

RodRod

Level

BenchmarkBenchmark

Elevation24.3900 m

Reconstruction of 1st order triangu-lation point on Nishinoshima Island

[Year]

VLBI

Efforts for Supporting “High-precision Positioning Society”*

Water flows from high to low, but more sci-entifically, it follows gravity. Accurate values of elevations, associated with water flows cannot be known without gravity. However, the effect of gravity is not reflect-ed in the values of height obtained by GNSS. GSI has been conducting very precise nationwide surveys of gravity using aircraft and plans to complete the operation of drawing the reference of elevation (0 m), a virtual line extending from the mean sea surface to land areas by March 2024. After that, GNSS will allow everyone to know the accurate elevation immediately, any-where and anytime.

Toward a society utilizing elevation with GNSS

The QZSS "MICHIBIKI," operated since November 2018 and called "Japanese GPS," offers Centimeter Level Augmentation Service (CLAS) as one of the partic-ular features to enable precise positioning in real time.Observation data obtained at GNSS CORSs are used for CLAS, and thus GNSS CORSs become more important than ever for their role to support MICHIBIKI‘s services expected to be essential in various fields in future.

The GNSS CORS network supports precisepositioning with MICHIBIKI.

Maps are created based on the positions at a certain reference time in the past. The earth’s ground, on the other hand, is constantly moving because of crustal activities. This is why the positions on a map tend to deviate from the current positions measured by GNSS, and the deviations accumulate and increase with time. Thus, GSI has created the Crustal Deforma-tion Correction System (POS2JGD) so that everyone can utilize location information without being aware of such differences.

Aligning maps with ever-moving crusts

A society supported byprecise positioning

A society supported byprecise positioning

QZSS “MICHIBIKI”Source: qzss.go.jp

The controlstation compilesand sendsaugmentationinformation.

Location-basedservice providerscompile and deliveraugmentationinformation.

Delivery ofaugmentationinformation. 

GSI compiles andprovides crustaldeformation correctioninformation.

Privateobservationstation

Mean sealevel

Aircraft nationwidemeasures gravity.

Elevation

GNSS

The density of the underground matter is not uniform and depends on locations. Thus, “the elevationreference does not always follow the mean sea level.

CrustalDeformationCorrection

System

A highly dense GNSS CORS network is required for providing more precise location based services. To realize it, GSI has started to integrate private observation stations into theexisting GNSS CORS network to provide more accurate positioning services. In addition, GSI is enhancing the functions of the GNSS CORS network so that their observation data can be stably provided even in case of power failure or submergence during a disaster.

Toward a society where more reliable positioningis realized

Crustal Deformation Correction

current positionposition on a map

Crustal Deformation Correction System

Source: Document distributedat the first business modelexamination meeting onautomatized driving aroundroad stations in hilly andmountainous areas

Source: Brochure of the GeospatialProject, Secretariat of the NationalSpatial Data Infrastructure (NSDI)Committee 

0605

CentralAnalysisCenter

Provides data onGNSS CORSs

Provision of correction information・Correction parameter files・Correction at the website・WebAPI for correction

The accurate elevation is shown immediately.

Elevation reference

(0m)

PhysicalDistribution Using

UAV

ICT Construction

Automatized DrivingSmart Agricultures

Crustal Deformation Correction System (POS2JGD)https://positions.gsi.go.jp/cdcs/*High-precision Positioning Society: a society in which a highly precise positioning environment exists through establishment of a

quasi-zenith satellite operation system, progress of indoor/outdoor positioning environment and technologies and popularizationand sophistication of mobile information terminals.

*High-precision Positioning Society: a society in which a highly precise positioning environment exists through establishment of a quasi-zenith satellite operation system, progress of indoor/outdoor positioning environment and technologies and popularizationand sophistication of mobile information terminals.

High-densitymatter