Results 241 to 250 of about 38,278 (336)
Abstract Glacier flow is typically modeled using a power‐law rheology known as the Glen–Nye flow law, with the power n $n$ assumed to be 3. However, recent research and past observations suggest that n=4 $n=4$ may better represent ice flow in some locations.
Benjamin Getraer, Mathieu Morlighem
wiley +1 more source
Ultraslow spreading ridges: slowest but locally thickest. [PDF]
Liu CZ, Zhu RX.
europepmc +1 more source
Summer Dynamics of Microbial Diversity on a Mountain Glacier. [PDF]
Hotaling S, Price TL, Hamilton TL.
europepmc +1 more source
Climate policy implications of nonlinear decline of Arctic land permafrost and other cryosphere elements [PDF]
Dmitry Yumashev+9 more
openalex +1 more source
Can Biogeochemical Tracer Observations Constrain Southern Ocean Diapycnal Mixing Rates?
Abstract Direct observations of background diapycnal mixing rates in the Southern Ocean (SO) are limited spatially and temporally, making the choice of an appropriate value to parameterize this mixing in Earth system models a challenge. However, the deployment of Argo floats throughout the SO has provided an extensive range of observations of both ...
Elizabeth Ellison+2 more
wiley +1 more source
A digital-twin platform for cryospheric disaster warning. [PDF]
Cui Y+7 more
europepmc +1 more source
Lower viral evolutionary pressure under stable versus fluctuating conditions in subzero Arctic brines. [PDF]
Zhong ZP+7 more
europepmc +1 more source
Abstract We used very high‐resolution satellite images to map the development of retrogressive thaw slumps (RTS) at six sites in the Russian High Arctic for the period 2011 to 2020. The 3,466 mapped RTS revealed an overall high activity, with site‐specific increases of RTS‐affected area up to +2,700% and RTS numbers up to +1,294%.
S. Barth+4 more
wiley +1 more source
Artificial intelligence for geoscience: Progress, challenges, and perspectives. [PDF]
Zhao T+50 more
europepmc +1 more source
Assessing the Duration of the Paleocene‐Eocene Thermal Maximum
Abstract The Paleocene‐Eocene Thermal Maximum (PETM) was a climate/carbon cycle perturbation recognized in stable carbon isotope (δ13C) records with a negative carbon isotope excursion (CIE). The PETM CIE termination has been associated with a δ13C inflection with pre‐PETM‐like values referred to as the G point.
Victor A. Piedrahita+6 more
wiley +1 more source