Results 121 to 130 of about 757,045 (352)
Gravimetric estimation of the Eötv¨ös matrix components
Contributions to Geophysics and Geodesy, 2017 The components of the Eötvös matrix are useful for various geodetic applications, such as interpolation of the elements of the deflection of the vertical, determination of gravity anomalies and determination of geoid heights. A torsion balance instrument
Gerassimos MANOUSSAKIS +2 more
doaj +1 more source
Geophysical Research Letters, Volume 53, Issue 2, 28 January 2026.Abstract Alaska's tectonic complexity makes it ideal for probing upper mantle deformation. We present a 3D shear‐wave anisotropy model obtained by inverting 7,985 SKS splitting intensity measurements from 261 broadband stations using 941 events from 2000 to 2023.
Yi Lin, Manuele Faccenda, Li Zhao
wiley +1 more source
Marine geodesy a multipurpose approach to solve oceanic problems [PDF]
Various current and future problem areas of marine geodesy are identified. These oceanic problem areas are highly diversified and include submersible navigation under ice seas, demarcation and determination of boundaries in deep ocean, tsunamis, ecology,
Saxena, N.
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Geophysical Research Letters, Volume 53, Issue 2, 28 January 2026.Abstract The Northeastern (NE) Tibet, as the front of plateau growth, widely absorbs northeastward extrusion, leading to significant uplift and forming a basin‐mountain tectonic framework. However, it remains unclear how the crust of NE Tibet deformed in response to the far‐field effects of the India‐Eurasia collision.
Ruo‐Jie Li +4 more
wiley +1 more source
A numerical test of the topographic bias
Journal of Geodetic Science, 2018 In 1962 A. Bjerhammar introduced the method of analytical continuation in physical geodesy, implying that surface gravity anomalies are downward continued into the topographic masses down to an internal sphere (the Bjerhammar sphere).
Sjöberg L.E., Joud M.S.S.
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Investigation of a geodesy coexperiment to the Gravity Probe B relativity gyroscope program [PDF]
Geodesy is the science of measuring the gravitational field of and positions on the Earth. Estimation of the gravitational field via gravitation gradiometry, the measurement of variations in the direction and magnitude of gravitation with respect to ...
Everitt, C. W. F. +2 more
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AVIRIS‐3 Rapid Response to January 2025 Los Angeles Wildfires
Geophysical Research Letters, Volume 53, Issue 2, 28 January 2026.Abstract Wildfires in wildland‐urban interfaces (WUIs) are a growing concern due to their devastating impact on human communities and ecosystems. Low‐latency impact assessment is critical for wildfire response, yet immediate access to fire‐affected communities can be limited.
Megan Ward‐Baranyay +15 more
wiley +1 more source
Open Geosciences, 2015 Most of the inland lakes do not have up-to-datebathymetry. However, a significant progress in surveyingtechnologies creates a possibility to quickly and accuratelydescribe the underwater environment.
Popielarczyk Dariusz +2 more
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The Uganda Gravimetric Geoid Model 2014 Computed by The KTH Method
Journal of Geodetic Science, 2015 For many developing countries such as Uganda, precise gravimetric geoid determination is hindered by the low quantity and quality of the terrestrial gravity data.
Sjöberg L. E., Gidudu A., Ssengendo R.
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The Zonal Wave‐3 Mode Impacts Antarctic Dense Water Formation
Geophysical Research Letters, Volume 53, Issue 2, 28 January 2026.Abstract At the Antarctic margins, dense water masses form as sea ice develops, driving the Antarctic branch of the global meridional overturning circulation. Previous studies found that large‐scale climate modes such as the Southern Annular Mode and El Niño Southern do not fully account for the interannual variability of dense water formation.
M. Auger, P. Spence, A. K. Morrison
wiley +1 more source