Results 241 to 250 of about 131,619 (292)

Assessing Co‐Located NISAR and Sentinel‐1 Observations for Atmospheric Characterization

open access: yesJournal of Geophysical Research: Atmospheres, Volume 131, Issue 19, 16 October 2026.
Abstract Tropospheric delay remains one of the largest sources of uncertainty in repeat‐pass Interferometric Synthetic Aperture Radar (InSAR) measurements, while accurate three‐dimensional deformation retrieval continues to be limited by the geometry of current spaceborne SAR systems.
Shadi Oveisgharan   +3 more
wiley   +1 more source

A digital-twin platform for cryospheric disaster warning. [PDF]

open access: yesNatl Sci Rev
Cui Y   +7 more
europepmc   +1 more source

Application of Distributed Acoustic Sensing for Active Near-Surface Seismic Monitoring. [PDF]

open access: yesSensors (Basel)
Roshdy E   +4 more
europepmc   +1 more source

North American ice sheet persistence into past interglacials should inform future projections. [PDF]

open access: yesNat Commun
Creel RC   +6 more
europepmc   +1 more source

Totten Glacier Subglacial Hydrology Determined From Geophysics and Modeling

Earth and Planetary Science Letters, 2020
Aurora Subglacial Basin (ASB), which feeds Totten Glacier, is a marine basin lying below sea level and contains up to 3.5m of global sea level equivalent. Rates of future sea level rise from this area are primarily dependent on the stability of Totten Ice Shelf and the controls on ice flow dynamics upstream of the grounding line, both of which may be ...
Christine F Dow, D D Blankenship
exaly   +2 more sources

Geophysical Characterization of the Furggwanghorn Rock Glacier, Switzerland

Proceedings, 2012
Degradation of alpine permafrost due to changing mean annual air temperatures can act as trigger for landslides and other ground instabilities. For a better understanding of the underlying thermo-hydromechanical processes an interdisciplinary research project has been set up.
Kaspar Merz   +3 more
openaire   +1 more source

Home - About - Disclaimer - Privacy