Results 191 to 200 of about 28,122 (271)
Using wavelet decomposition to determine the dimension of structures from projected images. [PDF]
Mayboroda S, Spergel DN.
europepmc +1 more source
Deforestation Impacts on Clouds and Precipitation Over Borneo Vary Across the Diurnal Cycle
Abstract The impact of tropical deforestation on clouds and precipitation remains uncertain due to complex interactions between land and atmospheric processes on convective and mesoscales. Here, we examine convective‐scale processes controlling the short‐term atmospheric response to deforestation over Borneo using multi‐day large eddy simulations ...
G. Leung, S. C. van den Heever
wiley +1 more source
Extreme rainfall over land exacerbated by marine heatwaves. [PDF]
Wang H +5 more
europepmc +1 more source
Abstract Coastal cities face critical challenges in managing ozone pollution because of high population density and complex interactions between urbanization and coastal meteorology. Using New York City (NYC) as a case study, this work examines how urban surfaces influence heatwaves, sea‐breeze circulations, and boundary‐layer dynamics, and how these ...
H. Gamarro +7 more
wiley +1 more source
Microfibers Accumulation within a Mediterranean Submesoscale Cyclone. [PDF]
Testa G +11 more
europepmc +1 more source
Submesoscale Eddies Buffer the Atlantic Niño/Niña Weakening Under Greenhouse Warming
Abstract The Atlantic Niño/Niña is a leading mode of tropical climate variability with profound global environmental and socioeconomic impacts. Conventionally, its variability is projected to weaken under greenhouse warming, primarily attributed to suppressed basin‐scale air–sea interactions.
Shengpeng Wang +6 more
wiley +1 more source
Characterisation of pelagic seascapes through micronektonic and zooplanktonic scattering layers. [PDF]
Diogoul N +7 more
europepmc +1 more source
Decoding Biases in Simulated Time‐Mean Equatorial Pacific Subsurface Temperatures
Abstract Equatorial subsurface ocean temperature (Tsub) strongly influences tropical Pacific climate variability, yet the Coupled Model Intercomparison Project Phase 5 (CMIP5) and Phase 6 (CMIP6) models exhibit persistent Tsub cold biases and substantial inter‐model uncertainty.
Aoyun Xue +6 more
wiley +1 more source
Oceanic uptake of CO<sub>2</sub> enhanced by mesoscale eddies. [PDF]
Li X +6 more
europepmc +1 more source
Ocean transit times: from basin to planetary scales. [PDF]
Cessi P.
europepmc +1 more source

