Results 181 to 190 of about 85,246 (286)
Contrasting climate oscillations impacts on phytoplankton in the western and eastern tropical Pacific. [PDF]
An L +10 more
europepmc +1 more source
Interacting Effects of Sea‐Level Rise and Ocean Warming Reshape Thermal Environments on a Coral Reef
Abstract Sea‐level rise (SLR) alters nearshore hydrodynamics, yet its influence on coral reef thermal regimes under climate‐driven ocean warming remains poorly quantified. Using a fully coupled hydrodynamic–wave model validated at Palmyra Atoll, we isolate how SLR modifies temperature variability during a projected 2050 marine heatwave.
Justin S. Rogers +4 more
wiley +1 more source
Tropical volcanism triggers pan-Asian monsoon droughts via circumglobal teleconnection. [PDF]
Nie W, Xia J, Kino K, She D, Oki T.
europepmc +1 more source
Abstract Using more than three decades (1993–2024) of satellite altimetry and ocean reanalysis, we reassess the dominant timescales of low‐frequency mesoscale eddy variability along the eastern boundary of the subtropical South Indian Ocean. After removal of the seasonal cycle, eddy kinetic energy (EKE) is primarily modulated on decadal timescales (8 ...
Yifei Zhou, Xuhua Cheng
wiley +1 more source
Volcanic eruptions disrupt ENSO teleconnections with land summer temperature. [PDF]
Zhang X +7 more
europepmc +1 more source
Enso diversity and global warming
El Niño-Southern Oscillation (ENSO) est le mode de variabilité dominant du Pacifique tropical à l'échelle inter-annuelle. Ce phénomène couplé océan-atmosphère est à l'origine d'événements météorologiques extrêmes qui affectent de nombreuses régions du monde.
openaire +3 more sources
Abstract Semi‐arid regions are expanding globally through divergent pathways: in East Asia (EA) via drying of semi‐humid lands, while in North America (NA) through wetting of arid areas. This interdecadal dry‐wet reversal across the Pacific has remained mechanistically unclear.
Shanshan Wang +4 more
wiley +1 more source
Influence of land-use history and ENSO on the flora of the Southern Line Islands. [PDF]
Nerfa L +5 more
europepmc +1 more source
ENSO Recharge Oscillator Theory Integrating the Southward Wind Shift
Abstract The El Niño–Southern Oscillation (ENSO) is one of the most‐well understood climate phenomena, and the Recharge Oscillator (RO) theory is widely used to conceptualize its physics in observations and models. ENSO‐associated equatorial zonal wind anomalies shift southward in boreal winter, contributing to ENSO termination.
Tomoki Iwakiri +3 more
wiley +1 more source
ENSO's changing grip on Bering Sea ice: The emerging control of the North Pacific meridional mode. [PDF]
Chen J +7 more
europepmc +1 more source

