Sediment waves and other evidence of paleo-bottom currents at two locations in the deep Arctic Ocean. Sedimentary Geology 23:269-299.Hall, J.K. 1979: Sediment waves and other evidence of paleo-bottom current at two locations in the deep Arctic Ocean; Sedimentary Geology, v.23, p.269-299....
as the upper-ocean warming signal strengthens stratification23,24(see also Fig.1), barotropic tidal dynamics may be subject to two effects. First, increased vertical density contrast allows for enhanced generation and propagation of internal tides, ...
TheAtlantic Oceanis a long, narrow ocean basin bisected by the Mid-Atlantic Ridge (MAR) (Figure 2.9). Wind-driven gyres and the wind-driven tropical circulation dominate transports in the upper ocean (Figure 9.1). The gyres and their western boundary currents include the anticyclonic subtropical...
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
(Methods). Yellow markers indicate the locations of tide gauges used in this study. Geographical names mentioned in the main text are (A) Mozambique Channel, (B) Mascarene Ridge, (C) East China Sea, (D) Yellow Sea, (E) Luzon Strait, (F) Celebes Sea, (G) Banda Sea, (H) Solomon ...
Remote-sensing data are available fromhttps://oceancolor.gsfc.nasa.gov/l3; the specific data product names are the first 240 months of the monthly 9-km standard MODIS-AquaRrsat 412, 443, 469, 488, 531, 547, 555, 645, 667, and 678 nm. Model outputs are available fromhttps://doi....
and where to transition over the outer reef out to deeper waters. Due to the low tide, there were moderate breaking seas in multiple locations over the shallows, and the Blackhand reef area was breaking most of the time. For every big set coming in from the ocean, large breaking seas we...
For instance, the carbon sampling and analysis (DIC, TA, pH, and/or pCO2) on WOCE cruises was a JGOFS project; university scientists participated in OACES cruises; and JGOFS incorporated time series stations at fixed locations (Hawaii and Bermuda), while WOCE had a suite of sections that ...
The near-inertial currents are significantly modified by the presence of the coast (and reduced in magnitude) within one or two internal radii of deformation from the coast [e.g., Pettigrew, 1981; Kim et al., 2011; Shearman, 2005]. The generation and propagation of coastal near-inertial ...
(NYSERDA) and U.S. Bureau of Ocean Energy Management, and verified opportunistic sightings reported to the authors or pulled from social media and news reports. Basemap used with permission from ESRI Ocean Basemap and its partners, showing marine water body names, undersea feature names, and ...