Results 141 to 150 of about 1,864 (260)
Deep mantle anomalies block early Earth melting, challenging a primordial origin. [PDF]
Roy A, Mittelstaedt E, Cooper CM.
europepmc +1 more source
Abstract Extreme weather in the Antarctic Peninsula arises from interactions among large‐scale circulation variability, atmospheric rivers (ARs), extratropical cyclones, and complex coastal terrain, yet the linkages across these scales remain insufficiently resolved.
D. Bozkurt +4 more
wiley +1 more source
Mesoscale Convective Systems in Northeastern North America: identification and evaluation with the convection-permitting version of the Canadian Regional Climate Model. [PDF]
Alpizar M +3 more
europepmc +1 more source
A flexure‐based variable stiffness structure is developed by integrating phase‐change modulation and adhesive interfacial locking of gallium. The design enables a wide stiffness variability, transitioning from soft, flexible behavior to rigid, load‐supporting performance.
Sungjin Kim +2 more
wiley +1 more source
A Theory on Parameterization of Cumulus Convection
openaire +2 more sources
Reduced cloud cover errors in a hybrid AI-climate model through equation discovery and automatic tuning. [PDF]
Grundner A +5 more
europepmc +1 more source
Gray‐Zone Simulation of the Dry Convective Boundary Layer Using Fourier Neural Operator
Abstract Previous machine learning (ML) weather prediction models primarily focus on global mesoscale forecasting. This study develops three‐dimensional Fourier neural operator (FNO) models for simulating the dry convective boundary layer (CBL) at 800‐m grid spacing, which is a resolution in the gray zone. The filtered large‐eddy simulation data of the
Tengfei Luo +5 more
wiley +1 more source
Neural general circulation models for modeling precipitation. [PDF]
Yuval J, Langmore I, Kochkov D, Hoyer S.
europepmc +1 more source
Abstract Many Earth System Models (ESMs) approximate surface emissivity as constant over all wavelengths (broadband). This approximation misrepresents the spectral distribution of longwave (LW) flux and introduces error in the LW atmospheric heating rate.
Lili Manzo +3 more
wiley +1 more source
PINN for stiff moving-boundary PDE to predict the locking point in superheated steam drying. [PDF]
Malekjani N +3 more
europepmc +1 more source

