Third, elastic deformation of the ocean floor occurs due to changing ocean mass loads (Mitrovica et al., 2001, 2011), affecting both near-field and far-field ocean heights. Sea level gravitational, rotational and deformational (GRD) fingerprints (Tamisiea et al., 2010; Kim et al., 2019;...
2021a), where it was pointed out that noise harmonics appear in spectra at depths of more than 15 m because the surface waves have faded to the instrumentation noise floor of the devices and the nonlinear constituents of the surface gravity waves have strengthened. Fortunately, this is of no...
Container details and voyage summaries: Access a complete summary of container movements and vessel details. Sanctions information: Review the vessel's sanctions status, including any links to restricted entities. Complete port coverage: Track container movements through key commercial ports globally. ...
IPCC (2023) Sixth assessment report. Summary for policymakers, A.1. It is virtually certain that the global ocean has warmed unabated since 1970 and has taken up more than 90% of the excess heat in the climate system (high confidence). Since 1993, the rate of ocean warming has more than...
and sought to obstruct government investigations of his conduct. The Committee will take no further action at this time on the allegations that he may have shared inappropriate images or videos on the House floor, misused state identification records, converted campaign funds to personal use, and/...
Sea floor spreadingTopographic and magnetic dataSummary Within the past decade, abundant data have been collected in the South Pacific Ocean (Pacific-Antarctic Ocean), and analysis of the geophysical data has shown the southeastern Pacific to be extremely interesting geologically. Two active spreading ...
These loggers sit ∼1 m off the sea floor in water depths ranging from 6 to 13 m and measure temperature at hourly or two-hourly sample rates. Time series of daily means were calculated as above. The Maria Island Time Series also provided Acoustic Doppler current profiler measurements...
SCIENTIFIC DATA | 3:160013 | DOI: 10.1038/sdata.2016.13 1 www.nature.com/sdata/ Background & Summary More than 20 years of altimeter data have greatly improved our understanding of upper ocean processes, including large scale ocean circulation1,2, mesoscale variability3,4, sea floor topography...
resolution and avoids the introduction of interpolation errors. This leads to a total of 78 different initial states. Examples of the match between the initial states both before and after relaxation can be found in Supplementary Note1(Supplementary Figs.1–3) alongside summary statistics for the ...
sensors mounted on the CTD, by miniature autonomous plume recorders (MAPR supplied by the PMEL Earth-Ocean observation programme of the National Oceanic and Atmospheric Administration (NOAA)) and by custom-made sensors for temperature, redox, pH and H2S mounted on an ocean floor observation system...