Global tidal model which does not require open boundary assumption was developed in order to provide lowest-order estimate on the tidal changes occurred in the Southeast and East Asian seas since the last glacial maximum. The model results suggested large changes in tides and tidal currents over ...
The surface and upper (0–500 m) layers of the subpolar North Atlantic (SPNA) have exhibited notable spatially coherent temperature anomalies across a broad range of timescales1,2,3,4,5. Extreme cold conditions characterised the middle years (2014–2016) of the past decade and have been...
Combined analysis of all three metagenome datasets (Red Sea, ALOHA, and MProfile) revealed significant differences (Kruskal-Wallis χ2 = 72.762, df = 2, p < 2.2 × 10–16) in AGS estimates of marine prokaryotes inhabiting the three canonical ocean depth layers (Fig. 2b...
This paper presents a five-year global simulation of HYCOM, the HYbrid Coordinate Ocean Model, that simultaneously resolves the eddying general circulation, barotropic tides, and baroclinic tides with 32 layers in the vertical direction and 1/12.5掳 (equatorial) horizontal grid spacing. A ...
Isolation of sulfate‐reducing bacteria from deep sediment layers of the pacific ocean Bacterial populations exist at great depths in marine sediments, but little is known about the type and characteristics of organisms in this unique bacteri... Stephen,P.,Barnes,... - 《Geomicrobiology Journal》...
The exponential - linear approximation has been used to reduce the number of discretized vertical layers while maintaining the accuracy. This model is developed to serve the remote sensing community in harvesting physical parameters from multi-platform, multi-sensor measurements that target different ...
Text Study Text TUenxtderstanding the Text Text Analysis Questions for Discussion 5 Healthy oceans can help ease the increasing burden our population is placing on this planet, but we need to be able to explore, observe and learn about the oceans in their entirety in order to protect ...
The model employed in (Sanay and Valle-Levinson 2005) used between 10 and 30 vertical layers in their model which we believe to add a dissipation that we are unable to reproduce. Fig. 11 Wind-induced circulation in a semi-enclosed homogeneous, rotating basin: scaled velocities at t =...
Previous authors have suggested the warming of the Upper Circumpolar Deep Water might be driven by increased stratification at the base of the Winter Water layer due to freshening, which would reduce mixing between the two layers and heat removal from the Upper Circumpolar Deep Water to the ...
In the large EHF regions, the magnitude of this EHF increase exceeds up to one-third of the EHF itself (Fig. 1c, d). In order to examine the respective roles of mesoscale and submesoscale eddies in the total EHF and its enhancement, the mesoscale and submesoscale EHFs (EHFme and EHF...