Results 271 to 280 of about 33,778 (318)
The C‐Shaped Landmass: A Key Driver of Monsoon Formation
Abstract Monsoon dynamics research has largely focused on idealized rectangular continents, primarily in the Northern Hemisphere mid‐latitudes. To investigate the broader impact of landmass configuration on monsoon formation and variability, we conducted extensive sensitivity experiments.
Junyu Mei+3 more
wiley +1 more source
Abstract In coarse resolution ocean models, eddy diffusive effects are parameterized using an isopycnal mixing coefficient, which controls mixing strength along isopycnals. Recent high‐resolution simulations show that increasing the wind stress over the Southern Ocean leads to increased local isopycnal mixing.
Nicole K. Neumann, C Spencer Jones
wiley +1 more source
Fast Proxy Centers for the Jeffreys Centroid: The Jeffreys-Fisher-Rao Center and the Gauss-Bregman Inductive Center. [PDF]
Nielsen F.
europepmc +1 more source
Mercury's Tidal Love Number h2 ${h}_{2}$ From Co‐Registration of MLA Profiles
Abstract Due to its eccentric orbit, Mercury experiences a varying gravitational pull from the Sun along its orbit, leading to periodic surface tidal deformation. The previous measurement of Mercury's tidal h2 ${h}_{2}$ by Bertone et al. (2021, https://doi.org/10.1029/2020je006683) is based on minimizing height differences at cross‐overs of the Mercury
Haifeng Xiao+5 more
wiley +1 more source
Circumcenter extension maps for non-positively curved spaces. [PDF]
Incerti-Medici M.
europepmc +1 more source
Abstract Observations of the 2019 magnitude 7.1 Ridgecrest, California, earthquake indicate a relatively slow rupture (∼ ${\sim} $2 km/s). The fault is surrounded by sedimentary rocks and low‐velocity damage zones, which can amplify ground motions but also slow down rupture.
Elif Oral+2 more
wiley +1 more source
What Causes the Hemispheric Difference in the Asymmetry of the Temperature Annual Cycle?
Abstract Previous studies have noted the asymmetry in the annual cycle of zonal mean surface air temperature, defined as the difference in the lengths of warming and cooling periods. Pronounced north‐south hemispheric differences in this asymmetry, by up to 40 days, were attributed to the eccentricity of Earth's orbit.
Fucheng Yang+2 more
wiley +1 more source
A geodesic completenss theorem for locatly symmetric Lorentz manifolds
Javier Lafuente López
openalex +2 more sources