Results 271 to 280 of about 116,829 (327)

The Emergence of a Human Fingerprint in the Boreal Winter Extratropical Zonal Mean Circulation

open access: yesGeophysical Research Letters, Volume 53, Issue 8, 28 April 2026.
Abstract The large‐scale atmospheric circulation plays an important role in regional climate. Recent studies have shown that poleward shifts in the Northern Hemisphere jet streams may be emerging, but the statistical significance and robustness are questionable.
Russell Blackport, Michael Sigmond
wiley   +1 more source

The Detection of Transient Subduction Zone Interface Properties Using Teleseismic Data

open access: yesGeophysical Research Letters, Volume 53, Issue 8, 28 April 2026.
Abstract The physical properties of subduction zone interfaces govern the transition between stable aseismic slip, episodic slow slip events (SSEs), and large earthquakes. Ultraslow velocity layers (USVLs) along the megathrust are commonly interpreted as indicators of elevated pore‐fluid pressures that promote slow slip, but their temporal variability ...
F. Rappisi, T. J. Craig, S. Rost
wiley   +1 more source

Stress Transfer From Slow Slip Events to Earthquake Swarms as a Cycle in the Southernmost Ryukyu Subduction Zone

open access: yesGeophysical Research Letters, Volume 53, Issue 8, 28 April 2026.
Abstract Recent megathrust earthquakes preceded by slow slip events highlight static stress transfer as a key triggering mechanism. However, there are limited insights into the interplay between static stress transfer and elevated fluid pressure before earthquake triggering.
Sean Kuanhsiang Chen   +4 more
wiley   +1 more source

Field Observations Validate LES‐Derived Scaling of Vertical‐Velocity Variance During the Afternoon Transition of the Convective Boundary Layer

open access: yesGeophysical Research Letters, Volume 53, Issue 8, 28 April 2026.
Abstract The convective velocity scale is commonly used to describe the vertical‐velocity variance in the convective boundary layer driven by surface heating, and is valid when the surface heat flux varies slowly compared to the eddy turnover time. This quasi‐equilibrium assumption typically holds from late morning to early afternoon, but breaks down ...
Omar El Guernaoui   +2 more
wiley   +1 more source

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