Scientists and engineers have observed for some time that tidal amplitudes at many
locations are shifting considerably due to nonastronomical factors. Here we review …

Until recently, high-resolution global modeling of tides has been done separately from high-
resolution global modeling of the atmospherically-forced oceanic general circulation. Here …

We present results from an ensemble of eight climate models, each of which has carried out
simulations of the early Eocene climate optimum (EECO,∼ 50 million years ago). These …

Astronomically calibrated cyclostratigraphy relies on correct matching of observed
sedimentary cycles to predicted astronomical drivers such as eccentricity, obliquity, and …

Ocean tides are the main source of high‐frequency variability in the vertical and horizontal
motion of ice sheets near their marine margins. Floating ice shelves, which occupy about …

Abstract Tides and Earth‐Moon system evolution are coupled over geological time. Tidal
energy dissipation on Earth slows rotation rate, increases obliquity, lunar orbit semi‐major …

The climate during the Cenozoic era changed in several steps from ice‐free poles and warm
conditions to ice‐covered poles and cold conditions. Since the 1950s, a body of information …

After more than a century of doubt and equivocation, cyclostratigraphy–the stratigraphic
record of astronomically forced paleoclimatic change–has come to be widely accepted in the …

Dissipation of tidal energy causes the Moon to recede from the Earth. The currently
measured rate of recession implies that the age of the Lunar orbit is 1500 My old, but the …

Here, we compare the ocean overturning circulation of the early Eocene (47–56 Ma) in eight
coupled climate model simulations from the Deep‐Time Model Intercomparison Project …