Results 141 to 150 of about 2,067 (261)
Abstract The oceanic component of the Transpolar Drift (TPD) is a key component of Arctic Ocean surface circulation. However, our understanding of its spatial extent and influence on the underlying water column remains limited. This study leverages a unique high spatial resolution oceanographic transect from August 2022 (late summer), first to identify
Zoé Koenig +8 more
wiley +1 more source
Population Size and Habitat Use by <i>Tachypleus tridentatus</i> in the Taiwan Straits. [PDF]
Shih YJ +10 more
europepmc +1 more source
Abstract The Penultimate Deglaciation (PDG) saw warming from the Penultimate Glacial Maximum to the Last Interglacial (LIG). We present 18‐kyr transient simulations through the PDG into the LIG using a fully‐coupled three‐dimensional ocean‐atmosphere model forced with Paleoclimate Modeling Intercomparison Project Phase 4 transient boundary conditions ...
Tim D. Cutler +3 more
wiley +1 more source
Ocean driven retreat of the Northeast Greenland Ice Stream following the Last Glacial Maximum. [PDF]
Callard SL +6 more
europepmc +1 more source
Nearshore Depth Estimation Using Fine-Resolution Remote Sensing of Ocean Surface Waves. [PDF]
Liu M, Zhu S, Cheng S, Zhang W, Cao G.
europepmc +1 more source
Abstract Paleomagnetic and rock magnetic analyses were conducted on sediment cores from the northeastern Greenland Shelf and Young Sound along the western edge of Fram Strait. The paleomagnetic signal in all three sediment cores is characterized by a strong and stable single component magnetization carried by low coercivity ferrimagnetic single domain ...
Juliette Girard +7 more
wiley +1 more source
Intraspecific and spatial variation in habitat use by sperm whales (<i>Physeter macrocephalus</i>) along the west coast of Martinique. [PDF]
Laurent S +4 more
europepmc +1 more source
Abstract Earth's long period background seismic wavefield is dominated by two distinct processes that couple ocean wave energy to a global microseism wavefield. We assess global microseism intensity in the secondary (4–10 s) and primary (14–20 s) bands, and across eight 2 s‐wide period bands between 4 and 20 s.
Richard C. Aster +4 more
wiley +1 more source
Spatial Dynamics of Harbour Porpoise <i>Phocoena phocoena</i> Relative to Local Hydrodynamics and Environmental Conditions. [PDF]
Runya RM +4 more
europepmc +1 more source
Fault Friction, Plate Rheology, and Mantle Torques From a Global Dynamic Model of Neotectonics
Abstract Improvements in software, parallel computing, global data sets, and laboratory flow‐laws help to develop the global Earth5 thin‐shell finite‐element model of Bird et al. (2008, https://doi.org/10.1029/2007jb005460) into a benchmark study. All experiments confirm that modeled faults (other than megathrusts) have low effective friction of 0.085 ±
Peter Bird +2 more
wiley +1 more source

