UNAVCO

Last updated
UNAVCO, Inc.
Founded1984 (1984)
Focus Geodesy, Data acquisition, Scientific data archiving
Location
Coordinates 40°03′40″N105°12′21″W / 40.06114°N 105.20586°W / 40.06114; -105.20586
Website www.unavco.org
Formerly called
University NAVSTAR Consortium

UNAVCO was a non-profit university-governed consortium that facilitated geology research and education using geodesy.

Contents

Background

UNAVCO was funded by the National Science Foundation (NSF) and the National Aeronautics and Space Administration (NASA) to support geology research worldwide. It operated the Geodetic Facility for the Advancement of Geoscience (GAGE Facility) on behalf of the NSF and NASA. As a university-governed consortium, UNAVCO supported the goals of the academic scientific community. UNAVCO had 120 US academic members and supported over 110 organizations globally as associate members.

On January 1, 2023, UNAVCO merged with the Incorporated Research Institutions for Seismology (IRIS) into EarthScope Consortium. [1]

Tools and Services

Data

The UNAVCO GAGE Facility, as a World Data Center, provided access to scientific data for quantifying the motions of rock, ice, and water at or near the Earth's surface. Geodetic Imaging Data] is collected by various sensors deployed on satellites, aircraft, and on the ground to provide high-resolution terrain models and deformation measurements. These can be taken over areas ranging in size from a dozen meters to hundreds of square kilometers. Data collected from strain and seismic borehole instruments is used to measure deformation on or near to the surface of the Earth as well as to measure the physical properties of rock within the vicinity of the installations. At many of the geodetic measurement sites, meteorological data are also collected to aid with processing of the geodetic data. In the large EarthScope Plate Boundary Observatory, now known as the "Network of the Americas" (NOTA), UNAVCO acquired, archived, and distributed multiple community datasets; including data from GNSS/GPS, strain meters, borehole seismometers, tilt meters, and geodetic imaging taken with radar and lidar.

The datasets could be found online via http file servers and search interfaces.

GPS/GNSS Systems

The UNAVCO GAGE Facility managed a community pool of high accuracy portable GPS/GNSS receiver systems used for a range of applications. These systems – which include: receivers, antennas, mounts, power and optionally, communications – can be deployed for days in shorter jobs or for many months in long-term investigations. Systems are also available for precision mapping applications.

Terrestrial Laser Scanning

The GAGE Facility at UNAVCO maintained a pool of Terrestrial Laser Scanning (TLS) instruments and associated peripherals; digital photography equipment, software and ancillary equipment to support Earth science investigators. TLS technology is based on lidar (Light Detection And Ranging) and is sometimes referred to as ground-based lidar or tripod lidar. It is an active imaging system whereby laser pulses are emitted by the scanner and the time and intensity of the returning pulses, reflected by the surface or object being scanned, are recorded. The round-trip time for pulses enables the taking of millions/billions of points, from which a 3D "point cloud" is generated to accurately map the scanned surface/object.

The primary capability of TLS is the generation of high resolution 3D maps and images of surfaces and objects over scales of meters to kilometers with centimeter to sub-centimeter precision. Repeat TLS measurements allow the imaging and measurement of changes through time and in unprecedented detail, making TLS even more valuable for transformative science investigations.

TLS is a powerful geodetic imaging tool which may support a wide range of user applications in many different environments. Geology applications to date include detailed mapping of; fault scarps, geologic outcrops, fault-surface roughness, frost polygons, lava lakes, dikes, fissures, glaciers, columnar joints and hillside drainages. Carrying out additional TLS surveys can be useful in the imaging and measurement of surface changes over time due to, for example; surface processes, volcanic deformation, ice flow, beach morphology transitions, or post-seismic slip. The incorporation of GNSS/GPS measurements provides accurate georeferencing of TLS data in an absolute reference frame. The addition of digital photography can be used to create photorealistic 3D images.

Engineering Expertise

The UNAVCO GAGE Facility provided engineering expertise and equipment resources to investigators in support of their geophysical research projects. This included proposal planning, project logistics, project support letters, field engineering support, modern GNSS equipment loans, permanent GNSS/GPS station installations, operation, and maintenance, and/or data acquisition, quality control, transfer, management, and archiving.

GAGE Facility engineers provided both classroom and in-field training; as well as project design and implementation, field engineering, TLS or GNSS/GPS network operations, and technology development for GNSS/GPS, TLS and other applications.

Polar services

The UNAVCO GAGE Facility provided geodetic support to NSF-OPP (National Science Foundation Office of Polar Programs) funded researchers working in the Arctic and Antarctic. Survey-grade GPS receivers, Terrestrial Laser Scanners, and supporting power and communications systems for continuous data collection and campaign surveying could be provided. Operation and maintenance services were also provided for long term data collection, with on-line data distribution from the UNAVCO community archive.

GGN, GNSS, IGS Support

The UNAVCO GAGE Facility provided global infrastructure support to NASA/JPL in operating a collection of high capability, globally distributed, permanent GNSS/GPS stations called the NASA Global GNSS Network (GGN). Data from these stations are used to produce highly accurate products for GNSS/GPS Earth science research, multidisciplinary applications, and education. UNAVCO also provided support for the International GNSS Service (IGS).

Short Courses, Workshops, Internships

The UNAVCO GAGE Facility's Education and Community Engagement (ECE) program offered short courses and workshops. They focused on professional development, research, and education, strategic support for scientific investigators in developing broader impacts, in-residence programs for geodesy science community members and educators, professional development in geosciences for K-12 faculty, and for undergraduate students through RESESS (Research Experiences in Solid Earth Science for Students), student internships to encourage broader participation in geosciences.

Plate Boundary Observatory (PBO)

UNAVCO operated the Plate Boundary Observatory (PBO), the geodetic component of the EarthScope program, funded by the National Science Foundation. The PBO consisted of several major observatory components: a network of 1100+ permanent, continuously operating Global Positioning System (GPS) stations many of which provided data at high-rate and in real-time, 78 borehole seismometers, 74 borehole strain meters, 28 shallow borehole tilt meters, and six long baseline laser strain meters. These instruments are complemented by INSAR (interferometric synthetic aperture radar) and lidar imagery and geochronology.

Continuously Operating Caribbean GPS Observational Network (COCONet)

UNAVCO operated the Continuously Operating Caribbean GNSS/GPS Observational Network (COCONet), which consisted of 50 planned continuously operating GPS/weather stations integrated with 65 existing GPS stations operated by partner organizations, 15 of which will be upgraded with new equipment. COCONet provides free, high-quality, open-format GPS and meteorological data for these stations via the internet for use by scientists, government agencies, educators, students, and the private sector. These data are used by local and foreign researchers to study solid earth processes such as tectonic plate motions, tectonic plate boundary interaction and deformation, including earthquake cycle processes and risks. They also serve atmospheric scientists and weather forecasting groups by providing more precise estimates of tropospheric water vapor and enabling better forecasting of the dynamics of airborne moisture associated with the yearly Caribbean hurricane cycle.

Organization

UNAVCO was organized into three programs. The three programs focused on: (1) data collection, including installation and maintenance of large-scale geodetic instrument networks (Geodetic Infrastructure); (2) network data operations, community data products, and cyber infrastructure (Geodetic Data Services); and (3) education and outreach strategies (Education and Community Engagement).

Geodetic Infrastructure

The Geodetic Infrastructure (GI) program integrated all geodetic infrastructure and data acquisition capabilities for continuously operating observational networks and shorter-term deployments. Supported activities included development and testing, advanced systems engineering, the construction, operation, and maintenance of permanent geodetic instrument networks around the globe, and engineering services tailored to PI project requirements. Major projects supported by the GI program included the 1,112 station Plate Boundary Observatory (PBO), Polar networks in Greenland and Antarctica (GNET and ANET, together known as POLENET), COCONet spanning the Caribbean plate boundary, the multi-disciplinary AfricaArray, and several other smaller continuously observing geodetic networks.

Geodetic Data Services

Geodetic Data Services (GDS) program provided services for the long-term stewardship of unique data sets. These services organized, managed, and archived data, and developed tools for data access and interpretation. GDS provided a comprehensive suite of services including sensor network data operations, data products and services, data management and archiving, and advanced cyber-infrastructure. Services were provided for GNSS/GPS data, Imaging data, Strain and Seismic data, and Meteorological data. GNSS/GPS data enable millimeter-scale surface motions at discrete points. Data from geodetic imaging instruments can be used to map topography and delineate deformation with high spatial resolution. INSAR and Terrestrial LIDAR imaging data services are provided. Strain and seismic data from borehole strain meters, seismometers, thermometers, pore pressure transducers, tilt meters, and rock samples from drilling, as well as surface-based tilt meters and laser strain meters were available. In addition, temperature, relative humidity, and atmospheric pressure data are available from surface measurements of atmospheric conditions from stations. Tropospheric parameters are generated during daily GNSS/GPS post-processing managed by UNAVCO and were accessed through data access services. The program was optimized to enable access to high-precision geodetic data. The UNAVCO Data Archive included more than 2,300 continuous GNSS/GPS stations.

Education and Community Engagement

The Education and Community Engagement program provided services to communicate the scientific results of the geodetic community, foster education across a broad range of learners, and grow workforce development and international partnerships. Particular focus was given to providing training, developing educational materials, and facilitating technical short courses to scientists studying geodesy. The program also supported formal education (K-12) and informal public outreach through workshops, educational materials for secondary students and undergraduate level courses, museum displays, and social media interactions. UNAVCO provided an annual series of short courses and workshops aimed at current researchers who wanted to update their skills or branch into new areas of geodetic research. UNAVCO Short Courses were offered to increase the capacity of the scientific community to process, analyze, and interpret various types of geodetic data. Educational Workshops promoted a broader understanding of Earth science for college and secondary education faculty.

UNAVCO supported geo-workforce development through undergraduate internship programs, graduate student mentoring, and online resources. The premier internship program for upper division undergraduate students was Research Experience in the Solid Earth Science for Students (RESESS). RESESS is funded by the National Science Foundation (NSF) and ExxonMobil. It was a multi-year geoscience research internship as well as a community support and professional development program designed to increase the diversity of students entering the geosciences. Upper-division undergraduate students from underrepresented groups spent 11 weeks in Boulder, Colorado during the summer, conducting an independent geoscience-focused research project. RESESS was a summer internship program dedicated to increasing the diversity of students entering the geosciences. Interns worked under the guidance of a research mentor and were mentored and supported throughout the academic year by RESESS program staff from UNAVCO. The alumni of RESESS are 55% Latino/Hispanic, 27% African American/Black, 11% Native American, and 7% Asian American. Of the 30 interns who went on to earn a bachelor's degree, 13 were enrolled in a master's degree program and 8 were enrolled in a doctoral program. Nine RESESS alumni were in private industry, five of which were working in geosciences. [2]

Membership and Governance

UNAVCO Members were educational or nonprofit institutions chartered in the United States (US) or its Territories with a commitment to scholarly research involving the application of high precision geodesy to Earth science or related fields. Members must also be willing to make a clear and continuing commitment to active participation in governance and science activities. Associate Membership was available to organizations other than U.S. educational institutions, when those organizations shared UNAVCO's mission and otherwise met the qualifications for membership.

A board of directors was charged with UNAVCO oversight and governance, and was elected by designated representatives of UNAVCO member institutions. The Board worked with the science community to create a broad interdisciplinary research agenda based on applications of geodetic technology, to identify investigator needs for infrastructure support, to develop proposals to appropriate sponsors to maintain that infrastructure capability, and to ensure that UNAVCO and its activities provide high quality, cost-effective, and responsive support. Advisory committees for each of the three programs guided the focus of the programs and helped shape their initiatives.

Science

For more than two decades, space-based geodetic observations have enabled measurement of the motions of the Earth's surface and crust at many different scales, with unprecedented spatial and temporal detail and increased precision, leading to fundamental discoveries in continental deformation, plate boundary processes, the earthquake cycle, the geometry and dynamics of mathematical systems, continental groundwater storage, and hydrologic loading.

Space geodesy furthers research on earthquake and tsunami hazards, volcanic eruptions, hurricanes, coastal subsidence, wetlands health, soil moisture, groundwater distribution, and space weather. [3]

Solid Earth

Earth and the tools to study it are constantly changing. The tectonic plates are continuously in motion, though so slowly that even with the highest precision instruments, months or years of observations are necessary to measure it. Over the last several decades, the advent of space-based geodetic techniques have improved the ability to measure tectonic plate motion by several orders of magnitude in spatial and temporal resolution as well as accuracy, and to establish stable terrestrial and celestial reference frames required to achieve these improvements. The research with these systems has led to revolutionary progress in our understanding of plate boundaries and plate interiors. [4]

Cryosphere

Ice covers approximately 10% of Earth's land surface at the present, with most of the ice mass being contained in the Greenland and Antarctic continental ice sheets. Designing and undertaking geodetic experiments that enable researchers to improve the understanding of ice dynamics allows stronger predictions (through numerical models) of the response of the glaciers to changing climates. [5] [6] [7]

Environmental and Hydrogeodesy

Through its sensitivity to mass redistribution and accurate distance measurements, geodesy is uniquely posed to answer fundamental questions about issues relating to water and the environment. Geodetic observations are enabling researchers, for the first time, to follow the motion of water within Earth's system at global scales and to characterize changes in terrestrial groundwater storage at a variety of scales, ranging from continental-scale changes in water storage using gravity space missions, to regional and local changes using INSAR, GNSS, leveling, and relative gravity measurements of surface deformation accompanying aquifer-system compaction. [8] [9] [10]

Ocean

Seventy-five percent of Earth's crust is unobservable using solely electromagnetic energy-based geodetic techniques. Seafloor geodesy can now expand geodetic positioning to off-shore environments. [11] Researchers can see the effects of changes in Earth's crust far beyond what we can measure with instruments placed solely on dry land. [12]

Atmosphere

Space geodesy utilizes electromagnetic signals propagating through the atmosphere of Earth, providing information on tropospheric temperature and water vapor and on ionospheric electron density. Thus, in the early twenty-first century, the goal of geodesy has evolved to include study of the kinematics and dynamics of both Earth's atmosphere and the solid Earth. [13] [14] [15]

Human Dimensions

Geodetic research associated with earthquakes and volcanoes have goals of providing early warnings and mitigating future hazard events on a global scale. As the population density increases and more people live in proximity to seismically active faults, understanding the nature of earthquakes remains a goal of the Earth sciences. [16] [17]

Technology

High-resolution images and 3D/4D topography maps facilitate field-based tests of a new generation of quantitative models of mass transport mechanisms. Open access to data, tools and facilities for processing, analysis, and visualization, and new algorithms and workflows are changing the landscape of geodetic scientific collaboration. [18]

Related Research Articles

<span class="mw-page-title-main">Geodesy</span> Science of measuring the shape, orientation, and gravity of the Earth and other astronomical bodies

Geodesy is the science of measuring and representing the geometry, gravity, and spatial orientation of the Earth in temporally varying 3D. It is called planetary geodesy when studying other astronomical bodies, such as planets or circumplanetary systems.

<span class="mw-page-title-main">Geophysics</span> Physics of the Earth and its vicinity

Geophysics is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis. Geophysicists, who usually study geophysics, physics, or one of the Earth sciences at the graduate level, complete investigations across a wide range of scientific disciplines. The term geophysics classically refers to solid earth applications: Earth's shape; its gravitational, magnetic fields, and electromagnetic fields ; its internal structure and composition; its dynamics and their surface expression in plate tectonics, the generation of magmas, volcanism and rock formation. However, modern geophysics organizations and pure scientists use a broader definition that includes the water cycle including snow and ice; fluid dynamics of the oceans and the atmosphere; electricity and magnetism in the ionosphere and magnetosphere and solar-terrestrial physics; and analogous problems associated with the Moon and other planets.

<span class="mw-page-title-main">Digital elevation model</span> 3D computer-generated imagery and measurements of terrain

A digital elevation model (DEM) or digital surface model (DSM) is a 3D computer graphics representation of elevation data to represent terrain or overlaying objects, commonly of a planet, moon, or asteroid. A "global DEM" refers to a discrete global grid. DEMs are used often in geographic information systems (GIS), and are the most common basis for digitally produced relief maps. A digital terrain model (DTM) represents specifically the ground surface while DEM and DSM may represent tree top canopy or building roofs.

<span class="mw-page-title-main">World Geodetic System</span> Geodetic reference system

The World Geodetic System (WGS) is a standard used in cartography, geodesy, and satellite navigation including GPS. The current version, WGS 84, defines an Earth-centered, Earth-fixed coordinate system and a geodetic datum, and also describes the associated Earth Gravitational Model (EGM) and World Magnetic Model (WMM). The standard is published and maintained by the United States National Geospatial-Intelligence Agency.

<span class="mw-page-title-main">Figure of the Earth</span> Size and shape used to model the Earth for geodesy

In geodesy, the figure of the Earth is the size and shape used to model planet Earth. The kind of figure depends on application, including the precision needed for the model. A spherical Earth is a well-known historical approximation that is satisfactory for geography, astronomy and many other purposes. Several models with greater accuracy have been developed so that coordinate systems can serve the precise needs of navigation, surveying, cadastre, land use, and various other concerns.

<span class="mw-page-title-main">Satellite laser ranging</span>

In satellite laser ranging (SLR) a global network of observation stations measures the round trip time of flight of ultrashort pulses of light to satellites equipped with retroreflectors. This provides instantaneous range measurements of millimeter level precision which can be accumulated to provide accurate measurement of orbits and a host of important scientific data. The laser pulse can also be reflected by the surface of a satellite without a retroreflector, which is used for tracking space debris.

<span class="mw-page-title-main">U.S. National Geodetic Survey</span> U.S. federal surveying and mapping agency

The National Geodetic Survey (NGS) is a United States federal agency based in Washington, D.C. that defines and manages a national coordinate system, providing the foundation for transportation and communication, mapping and charting, and a large number of science and engineering applications. Since its founding in 1970, it has been part of the National Oceanic and Atmospheric Administration (NOAA), a division within the United States Department of Commerce.

<span class="mw-page-title-main">International Terrestrial Reference System and Frame</span> World spatial reference system co-rotating with the Earth in its diurnal motion in space

The International Terrestrial Reference System (ITRS) describes procedures for creating reference frames suitable for use with measurements on or near the Earth's surface. This is done in much the same way that a physical standard might be described as a set of procedures for creating a realization of that standard. The ITRS defines a geocentric system of coordinates using the SI system of measurement.

<span class="mw-page-title-main">Satellite geodesy</span> Measurement of the Earth using satellites

Satellite geodesy is geodesy by means of artificial satellites—the measurement of the form and dimensions of Earth, the location of objects on its surface and the figure of the Earth's gravity field by means of artificial satellite techniques. It belongs to the broader field of space geodesy. Traditional astronomical geodesy is not commonly considered a part of satellite geodesy, although there is considerable overlap between the techniques.

<span class="mw-page-title-main">Aseismic creep</span> Surface displacement along a geological fault without earthquakes occurring

In geology, aseismic creep or fault creep is measurable surface displacement along a fault in the absence of notable earthquakes. Aseismic creep may also occur as "after-slip" days to years after an earthquake. Notable examples of aseismic slip include faults in California.

<span class="mw-page-title-main">Earthscope</span> Earth science program exploring the structure of the North American continent

The EarthScope project was an National Science Foundation (NSF) funded earth science program that, from 2003-2018, used geological and geophysical techniques to explore the structure and evolution of the North American continent and to understand the processes controlling earthquakes and volcanoes. The project had three components: USArray, the Plate Boundary Observatory, and the San Andreas Fault Observatory at Depth. Organizations associated with the project included UNAVCO, the Incorporated Research Institutions for Seismology (IRIS), Stanford University, the United States Geological Survey (USGS) and National Aeronautics and Space Administration (NASA). Several international organizations also contributed to the initiative. EarthScope data are publicly accessible.

<span class="mw-page-title-main">Plate Boundary Observatory</span>

The Plate Boundary Observatory (PBO) was the geodetic component of the EarthScope Facility. EarthScope was an earth science program that explored the 4-dimensional structure of the North American Continent. EarthScope was a 15-year project (2003-2018) funded by the National Science Foundation (NSF) in conjunction with NASA. PBO construction took place from October 2003 through September 2008. Phase 1 of operations and maintenance concluded in September 2013. Phase 2 of operations ended in September 2018, along with the end of the EarthScope project. In October 2018, PBO was assimilated into a broader Network of the Americas (NOTA), along with networks in Mexico (TLALOCNet) and the Caribbean (COCONet), as part of the NSF's Geodetic Facility for the Advancement of Geosciences (GAGE). GAGE is operated by EarthScope Consortium.

<span class="mw-page-title-main">North American Datum</span> Reference frame for geodesy on the continent

The North American Datum (NAD) is the horizontal datum now used to define the geodetic network in North America. A datum is a formal description of the shape of the Earth along with an "anchor" point for the coordinate system. In surveying, cartography, and land-use planning, two North American Datums are in use for making lateral or "horizontal" measurements: the North American Datum of 1927 (NAD 27) and the North American Datum of 1983 (NAD 83). Both are geodetic reference systems based on slightly different assumptions and measurements.

<span class="mw-page-title-main">Geodynamics</span> Study of dynamics of the Earth

Geodynamics is a subfield of geophysics dealing with dynamics of the Earth. It applies physics, chemistry and mathematics to the understanding of how mantle convection leads to plate tectonics and geologic phenomena such as seafloor spreading, mountain building, volcanoes, earthquakes, faulting. It also attempts to probe the internal activity by measuring magnetic fields, gravity, and seismic waves, as well as the mineralogy of rocks and their isotopic composition. Methods of geodynamics are also applied to exploration of other planets.

<span class="mw-page-title-main">UNSW School of Surveying and Geospatial Engineering</span>

The UNSW School of Surveying and Geospatial Engineering (SAGE), part of the UNSW Faculty of Engineering, was founded in 1970 and disestablished in 2013.

<span class="mw-page-title-main">Geodetic Observatory Wettzell</span>

The Geodetic Observatory Wettzell is located atop the 616 meter-high mountain Wagnerberg, west of the village Wettzell in the German district Cham in the Bavarian Forest.

<span class="mw-page-title-main">Kristine M. Larson</span> American geophysicist

Kristine Marie Larson is an American academic. She is Emeritus Professor of Aerospace Engineering at the University of Colorado Boulder. Her research considers the development of algorithms for high-precision Global Positioning System (GPS) data analysis. She was the first to demonstrate that GPS could be used to detect seismic waves. She was awarded the 2015 European Geosciences Union Christiaan Huygens Medal.

Éric Calais is a French geologist-geophysicist, born in 1964, internationally recognized practitioner of high-precision space geodesy and a pioneer in its applications to measure seismic deformations at the boundaries of tectonic plates and in their interiors. He has been a member of the French Academy of Sciences since 2017.

Thomas A. Herring is a geophysicist, known for developing and applying systems of space geodesy to high-precision geophysical measurements and geodynamic research.

Tonie Marie van Dam is an American geophysicist and geodesist, known for her pioneering research on solid Earth deformations due to loads from atmospheric and hydrologic pressures. She and her collaborators used space geodetic observations and modeling for increased precision in measuring and understanding such loads.

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