A review of the deep and surface currents around Eirik Drift, south of Greenland: Comparison of the past with the present. Global and Planetary Change 79(3-4), 244-254.STANFORD J D, ROHLING E J, BACON S, et al. A review of the deep and surface currents around Eirik Drift, south ...
The deep navigation channel along the eastern boundary was found to be ultimately responsible. The deep channel allows the density and tidally-induced subtidal currents to intensify over it, producing the eastern intensification. Both mechanisms operate in the non-rotating limit and consequently do ...
Data from six surveys of the region off the Cape of Good Hope and one in the Benguela Current have been used to calculate dynamic height anomalies and surface currents. The temperature and salinity distributions and the nature of the water masses are also discussed. Current velocities up to 70...
the MISO (Kikuchi and Wang, 2010), given the reverse direction of background currents during boreal summer and boreal winter, the relationship between the u ISV in the equatorial Indian Ocean and the MJO/MISO remains an interesting topic which is short of deep investigation in previous studies....
Shearing along subduction zones, laboratory experiments on analogue faults, and sliding along glacier beds are all associated with aseismic and co-seismic slip. In this study, an ocean-bottom seismometer is deployed near the terminus of a Greenlandic tid
A third generation numerical wave model SWAN (Simulating WAves Nearshore) was applied to study the spatio-temporal effect of surface currents and sea level height on significant wave height; and to describe the mechanisms responsible for wave–current interaction in the eastern Baltic Sea. Simulation...
A total of 3200 time-domain traces are captured and averaged to resolve this spectrum. d Measured terahertz pulse energy/power from the fabricated nanoantenna array as a function of the optical pulse energy/power (inset) in comparison with other passive optical-to-terahertz converters reported in ...
Yellow arrows represent the bottom currents and undercurrents, Green arrows represent the Antarctic Intermediate Water, Red arrows represent the surface and sub-surface currents; AAIW: Antarctic Intermediate Water, KC: Kuroshio Current, LCPW: Lower Circumpolar Water, LUC: Luzon Undercurrent, MC: Mindan...
and Veron29conducted mesocosm studies with artificially generated rain in a wind wave flume to investigate the influence of rain on near-surface currents. In addition, mesocosm studies with artificial rain have been applied to investigate air–water gas exchange18,30. Our experiments do not aim to...
Three types of defect on the crystal surface, namely, FA vacancies, uncoordinated lead and Pb–Pb dimers caused by bromide loss, are found to form deep traps, resulting in non-radiative charge recombinations at the metal/perovskite interface. By tailoring the passivation functional groups, we ...