Results 191 to 200 of about 92,051 (340)
Building Treatment and Its Effects on City‐Scale Urban Flood Modeling
ABSTRACT Physics‐based flood hydrodynamic models are widely used for predicting inundation in urban basins with complex building layouts. While the treatment of urban buildings in these models has been extensively discussed, over‐assumptions can introduce inaccuracies, uncertainties, and excessive computational effort, particularly under data‐scarce ...
Zekai Li +3 more
wiley +1 more source
Coastal wave refraction in variable currents over a varying bathymetry. [PDF]
Halsne T, Li Y.
europepmc +1 more source
P‐Wave Reverberations in the Water Column of the Chilean Subduction Trench
Abstract P‐waves generated by subduction earthquakes can get trapped within the submarine trench, where they reverberate and contaminate the initial seismic signals. We analyze the behavior of P‐wave reverberations for 43 earthquakes of magnitude larger than 6.0 that occurred along the Chilean margin between 1995 and 2023. We compared the energy of the
H. Schwarze, R. Madariaga, S. Ruiz
wiley +1 more source
A wave glider for passive acoustic monitoring of cetaceans and anthropogenic sources in the central Mediterranean Sea. [PDF]
Ferri S +7 more
europepmc +1 more source
The synthesis of estuarine bathymetry from sparse sounding data
Janet Eirlys Burroughes
openalex +2 more sources
Abstract Turbidity currents are destructive flows that are hazardous to critical seafloor infrastructure on submarine slopes because run‐up heights can be 10–100s of meters, as their relative density is 2–3 orders of magnitude lower than terrestrial flows. Currently, risk analysis is hindered by poor prediction of run‐up heights that are mainly derived
Ru Wang +6 more
wiley +1 more source
Features and trends of marine heat waves and marine cold spells along the Western Iberian Coast from four decades of satellite data. [PDF]
Biguino B, Haigh ID, Dias JM, Brito AC.
europepmc +1 more source
Abstract In the present day, global oceans have absorbed most of the excess anthropogenic heat, abating surface temperature warming. The Mid‐Pliocene Warm Period (MPWP; ∼ ${\sim} $3.2 million years ago) offers an opportunity to understand how globally warmer climates store oceanic heat.
Harry J. Grosvenor +3 more
wiley +1 more source
Seismic oceanography data in the Gulf of Cadiz. [PDF]
Duarte AF, Mendes R, Azevedo L.
europepmc +1 more source

