Results 111 to 120 of about 3,825 (220)
Global GNSS Observation of Mesoscale Ionospheric Irregularities (2006–2024)
Abstract Mesoscale ionospheric irregularities are statistically investigated using an unprecedented 19‐year long‐term global GNSS (Global Navigation Satellite System) TEC (total electron content) data set. These irregularities are represented by ionospheric fluctuations within a 5°× ${}^{\circ}\times $ 3.75° ${}^{\circ}$ (latitude by longitude) region ...
Shun‐Rong Zhang +7 more
wiley +1 more source
Seismic evidence for deep hydrothermal circulation and faulting at slow spreading Mid-Atlantic Ridge
Vaddineni V, Jian H, Singh S.
europepmc +1 more source
Synoptic Controls of Extreme Ice Area Flux Events Along Nares Strait
Abstract Nares Strait, the channel between Ellesmere Island and northwest Greenland, connects the Arctic Ocean's Lincoln Sea to northern Baffin Bay. The transport of thick, multi‐year sea ice southward down the Strait contributes to the overall loss of this important ice class from the Arctic.
K. McNeil +3 more
wiley +1 more source
CO2 degassing in the mantle triggers deep earthquakes at the Mid-Atlantic Ridge
Yu Z +7 more
europepmc +1 more source
Sediment structure at the equatorial mid-atlantic ridge constrained by seafloor admittance using data from the PI-LAB experiment. [PDF]
Saikia U +3 more
europepmc +1 more source
Episodic Northward Transport Along Nares Strait Brings Anomalously Warm Water Into the Arctic Ocean
Abstract Nares Strait is one of the primary Arctic export pathways for sea ice and freshwater, connecting the Arctic Ocean to the subpolar North Atlantic. The southward transport along the strait, primarily driven by the higher sea level in the Arctic compared to Baffin Bay, has occasionally been observed to reverse.
Yarisbel Garcia‐Quintana +2 more
wiley +1 more source
Author Correction: A distinct and active bacterial community in cold oxygenated fluids circulating beneath the western flank of the Mid-Atlantic ridge. [PDF]
Meyer JL +10 more
europepmc +1 more source
Abstract The Indian Ocean plays a crucial role in the abyssal overturning circulation, transforming Antarctic Bottom Water (AABW) into lighter water. In the western Indian Ocean, the only path for AABW to reach the subtropics as part of the global overturning is through the fracture zones of the Southwest Indian Ridge.
Viviane V. Menezes +4 more
wiley +1 more source
Abstract Buoyancy forcing in the subpolar North Atlantic Ocean (SPNA) is an important driver of the Atlantic Meridional Overturning Circulation (AMOC). To advance understanding of the mechanisms connecting the two processes and their relative importance in sub‐basins within the SPNA, we apply the Water Mass Transformation Framework to a matched‐pair of
Ben Moore‐Maley +4 more
wiley +1 more source

