Results 151 to 160 of about 6,971 (293)
ABSTRACT The main purpose of this paper is to design a fully discrete local discontinuous Galerkin (LDG) scheme for the generalized Benjamin–Ono equation. First, we prove the L2$$ {L}^2 $$‐stability for the proposed semi‐discrete LDG scheme and obtained a suboptimal order of convergence for power nonlinear flux.
Mukul Dwivedi, Tanmay Sarkar
wiley +1 more source
Near-surface liquid water on Mars inferred from seasonal marsquakes. [PDF]
Shi J +12 more
europepmc +1 more source
Are West African Heat‐Lows Analogous to Dry Tropical Cyclones?
Heat‐lows qualitatively resemble dry tropical cyclones (TCs), though their underlying physics has yet to be compared. In this study, we show that West African transient heat‐low climatology correlates well with TC potential intensity generalised over land.
Aaron Kruskie +2 more
wiley +1 more source
Powering Ganymede's dynamo with protracted core formation. [PDF]
Trinh KT +3 more
europepmc +1 more source
Abstract Parameterizing boundary layer turbulence in Earth System Models (ESMs) introduces a key source of uncertainty. Here, we explore the impact of implementing a prognostic formulation (PMF) for momentum flux, which permits countergradient (CG) fluxes.
Kyle M. Nardi +5 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
Deployment Strategy Shapes the Polar Climate Response to Marine Cloud Brightening
Abstract Marine cloud brightening (MCB) is a proposed solar climate intervention strategy that increases marine cloud reflectivity to cool Earth's surface. While previous studies have largely examined its global temperature and precipitation effects, little is known about how MCB deployment strategies influence polar climate and sea ice.
E. J. Emme, C.‐C. Chen, H. M. Horowitz
wiley +1 more source
Evolution of shallow cumulus convection and its parameterization
Shallow cumulus convection is important not only because of its role in mediating local turbulent transport in the boundary layer (BL), but also because of its ability to affect large-scale atmospheric circulations at a climate scale.
Zhu, Ping
core
Helioseismic evidence that the solar dynamo originates near the tachocline. [PDF]
Mandal K, Kosovichev AG.
europepmc +1 more source
Abstract Wintertime open‐ocean convection is a key process in renewing deep water; however, the processes that promote convection on local scale remain poorly understood. We investigate the role of long‐lived anticyclonic eddies in facilitating deep convection in the Greenland Sea using a new model simulation and observations.
Dong Jian +3 more
wiley +1 more source

