Results 131 to 140 of about 35,280 (229)
Mesoscale Eddy Currents Reshape the Spatial Distribution of Wave Height in the Southern Ocean
Abstract Mesoscale eddy currents influence ocean surface waves, but their imprints on wave height remain poorly described by observations. Here, we examine significant wave height (SWH) variations associated with more than 42,000 mesoscale eddies in the Southern Ocean using along‐track Jason‐3 altimeter measurements.
Tianyi Cheng +3 more
wiley +1 more source
High‐Resolution Observations Unveil (Sub)Mesoscale Heat Fluxes Shaping Upper‐Ocean Heat Content
Abstract Upper‐ocean heat content (UOHC) modulates air–sea exchange in tropical regions; however, its variability at (sub)mesoscale remains insufficiently resolved. Here we combine Surface Water and Ocean Topography (SWOT) observations with high‐resolution glider sections in the northeastern tropical Pacific, where mesoscale eddies and sharp frontal ...
Mathieu Gentil +5 more
wiley +1 more source
Hydraulic or Seepage Erosion: What Drives Bank Collapse in Tidal Environments?
Abstract The collapse of channel banks in tidal environments has typically been interpreted using fluvial concepts that prioritize hydraulic (flow‐driven) erosion. Yet daily tidal fluctuations trap pore water in channel banks, potentially producing sustained seepage flows capable of triggering collapse even without strong currents.
Kun Zhao +5 more
wiley +1 more source
Exploring the Interior Structure and Mode of Tidal Heating in Enceladus
Enceladus is among the most intriguing bodies in the solar system due to its astrobiological potential. Determining the extent and duration of habitability (i.e., sustained habitability ) requires characterizing the interior properties and the level and ...
Amirhossein Bagheri +6 more
doaj +1 more source
Parametrized tidal dissipation numbers of nonrotating black holes
40 pages, Matches PRD ...
Hajime Kobayashi +4 more
openaire +2 more sources
Turbulent Mixing and Dissipation Around Rough Seamounts
Abstract Seamounts are critical components of the global ocean energy budget, contributing significantly to turbulent dissipation through their interaction with large‐scale flows. However, most previous numerical investigations used smoothed bathymetry that omits small‐scale topographic variability. We use turbulence‐resolving large‐eddy simulations to
Tomas Chor +2 more
wiley +1 more source
A Method for Quantifying Paleoenvironmental Impacts on Lunar Recession and the Moon’s Age
Geological evidence indicates that the Moon formed at least 4.46 billion years ago. Models of Earth–Moon evolution generally describe tidal friction as the primary driver of lunar recession—the gradual increase in the lunar orbital semimajor axis—and the
M. Kiani Shahvandi
doaj +1 more source
The coupled tidal evolution of the moons and spins of warm exoplanets
Context. The Solar System giant planets harbor a wide variety of moons. Among them, the largest moons have moon-to-planet mass ratios of the order of 10−4.
Su Yubo, Saillenfest Melaine
doaj +1 more source
Impact of Non‐Classical Gravity‐Wave Dynamics on Middle‐Atmosphere Mean Flow and Solar Tides
Abstract Conventional gravity‐wave (GW) parameterizations neglect three aspects of GW dynamics. Instead of momentum and entropy fluxes they use Eliassen‐Palm fluxes, thereby neglecting the possibility that resolved flow are not in geostrophic and hydrostatic balance.
T. Kühner, G. S. Völker, U. Achatz
wiley +1 more source
Abstract Hovmöller plots of upper‐tropospheric local (Rossby) wave activity (LWA) show that the subtropics of the North Pacific/Atlantic basins are relatively wave‐free in the upstream and wavier in the downstream of quasi‐stationary atmospheric rivers (QSARs).
Hung‐I. Lee, Noboru Nakamura
wiley +1 more source

