Results 101 to 110 of about 2,406 (195)
3D Atmospheric Imprint of Mesoscale Eddies Driven by the Thermal Feedback in the Gulf Stream Region
Abstract The 3D imprint of mesoscale ocean eddies on the overlying atmosphere is investigated using coupled ocean‐atmosphere high‐resolution simulation of the Gulf Stream region, distinguishing cyclones and anticyclones. Sea surface temperature (SST) anomalies are predominantly warm for anticyclones and cold for cyclones, driving a Thermal Feedback ...
Alexandre Barboni, Lionel Renault
wiley +1 more source
Abstract Turbulence dissipation rate (EDR) governs the conversion of turbulent kinetic energy to heat and thereby controls vertical mixing, transport, and energy exchange in the convective boundary layer (CBL). The spatiotemporal structure of EDR remains poorly constrained, as observations are limited to point measurements or sparse vertical profiles ...
Yufei Chu +10 more
wiley +1 more source
How Can the Latent Heat Entrainment Flux in the Convective Boundary Layer be Characterized?
Abstract A proposed theoretical description of the latent heat entrainment flux at the top of a convective boundary layer (CBL) was tested. It is related to the vertical velocity scale times the ratio of the water vapor mixing ratio (WVMR) gradient to the Brunt‐Väisälä frequency. This relation was tested with different LiDAR and radiosonde measurements.
Linus von Klitzing +4 more
wiley +1 more source
Abstract Emissions of nitrogen oxides (NOx = NO + NO2), a precursor to ozone and secondary aerosol formation have become increasingly important to understand as ozone production transitions to NOx limited in most regions of the US. Recent studies suggest that NOx emissions associated with agricultural activities, particularly cropland soils, are an ...
Ilana B. Pollack +28 more
wiley +1 more source
Enhancing impacts of mesoscale eddies on Southern Ocean temperature variability and extremes. [PDF]
He Q +6 more
europepmc +1 more source
Divergent Influences of Oceanic Western Boundary Currents on Weak and Strong Tropical Cyclones
Abstract Tropical cyclones (TCs) in the Northern Hemisphere often cross oceanic western boundary currents (WBCs), yet how these warm currents modulate TC intensity remains unclear. We analyze TCs traversing the Kuroshio and Gulf Stream during 1993–2025 and find that weak TCs respond more favorably than strong TCs.
Wenting Lou +5 more
wiley +1 more source
Conventional wisdom about mesoscale eddies is that cyclonic (anticyclonic) eddies are commonly associated with cold(warm) surface cores. Nevertheless, plenties of surface warm cyclonic eddies (WCEs) and cold anticyclonic eddies (CAEs) in the North ...
Yaowei Ma +4 more
doaj +1 more source
Doubling of surface oceanic meridional heat transport by non-symmetry of mesoscale eddies. [PDF]
Wang H, Qiu B, Liu H, Zhang Z.
europepmc +1 more source
Microphysics and Kinematics of a High Flash Rate Storm With a Bottom‐Heavy Charge Structure
Abstract An atypical thunderstorm with unusual lightning and charge structure characteristics propagated through Cordoba province, Argentina, during the austral warm season in late 2018. This storm exhibited echo tops near 10.5 km, with high lightning activity concentrated at low altitudes.
Bruno L. Medina +4 more
wiley +1 more source
Hidden heatwaves and severe coral bleaching linked to mesoscale eddies and thermocline dynamics. [PDF]
Wyatt ASJ +5 more
europepmc +1 more source

