Mechanisms and impacts of Earth system tipping elements
Tipping elements are components of the Earth system which may respond nonlinearly to
anthropogenic climate change by transitioning toward substantially different long‐term …
anthropogenic climate change by transitioning toward substantially different long‐term …
All‐Recyclable Triboelectric Nanogenerator for Sustainable Ocean Monitoring Systems
The growing severity of environmental problems such as plastic waste and climate change
has inspired active research into solutions based on recyclable and renewable energy …
has inspired active research into solutions based on recyclable and renewable energy …
The impact of 3-D Earth structure on far-field sea level following interglacial West Antarctic Ice Sheet collapse
Prior to inferring ice sheet stability from past interglacial sea-level records, these records
must first be corrected for the contaminating effects of glacial isostatic adjustment (GIA) …
must first be corrected for the contaminating effects of glacial isostatic adjustment (GIA) …
Synchronous retreat of Thwaites and Pine Island glaciers in response to external forcings in the presatellite era
RW Clark, JS Wellner, CD Hillenbrand… - Proceedings of the …, 2024 - National Acad Sciences
Today, relatively warm Circumpolar Deep Water is melting Thwaites Glacier at the base of its
ice shelf and at the grounding zone, contributing to significant ice retreat. Accelerating ice …
ice shelf and at the grounding zone, contributing to significant ice retreat. Accelerating ice …
The influence of realistic 3D mantle viscosity on Antarctica's contribution to future global sea levels
N Gomez, M Yousefi, D Pollard, RM DeConto… - Science …, 2024 - science.org
The response of the Antarctic Ice Sheet (AIS) to climate change is the largest uncertainty in
projecting future sea level. The impact of three-dimensional (3D) Earth structure on the AIS …
projecting future sea level. The impact of three-dimensional (3D) Earth structure on the AIS …
Constraining the contribution of the Antarctic Ice Sheet to Last Interglacial sea level
Polar temperatures during the Last Interglacial [LIG;~ 129 to 116 thousand years (ka)] were
warmer than today, making this time period an important testing ground to better understand …
warmer than today, making this time period an important testing ground to better understand …
Dislocation theory of steady and transient creep of crystalline solids: Predictions for olivine
In applications critical to the geological, materials, and engineering sciences, deformation
occurs at strain rates too small to be accessible experimentally. Instead, extrapolations of …
occurs at strain rates too small to be accessible experimentally. Instead, extrapolations of …
[HTML][HTML] DiluviumDEM: Enhanced accuracy in global coastal digital elevation models
D Dusseau, Z Zobel, CR Schwalm - Remote Sensing of Environment, 2023 - Elsevier
Accurate representation of global coastal topography is essential for numerous scientific
disciplines, coastal management, and disaster risk assessment. Even with recent …
disciplines, coastal management, and disaster risk assessment. Even with recent …
Evolution of the Antarctic Ice Sheet over the next three centuries from an ISMIP6 model ensemble
Abstract The Ice Sheet Model Intercomparison Project for CMIP6 (ISMIP6) is the primary
effort of CMIP6 (Coupled Model Intercomparison Project–Phase 6) focusing on ice sheets …
effort of CMIP6 (Coupled Model Intercomparison Project–Phase 6) focusing on ice sheets …
A high‐end estimate of sea level rise for practitioners
RSW van de Wal, RJ Nicholls, D Behar… - Earth's …, 2022 - Wiley Online Library
Sea level rise (SLR) is a long‐lasting consequence of climate change because global
anthropogenic warming takes centuries to millennia to equilibrate for the deep ocean and …
anthropogenic warming takes centuries to millennia to equilibrate for the deep ocean and …