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IOC Sub-Commission for the Western Pacific, fifth session
IOC Sub-Commission for the Western Pacific, fifth session

... Centre (RC) to be signed on the occasion of this Session. He thanked the Republic of Korea for the excellent organization of the Fifth WESTPAC International Scientific Symposium, held in Seoul, 27-31 August 2001. Another significant event was the International Conference on the International Oceanog ...
Reconciling plate-tectonic reconstructions of Alpine
Reconciling plate-tectonic reconstructions of Alpine

... 1. The controversial fate of Alpine Tethys Ever since Steinmann (1905) tried to relate the oceanic affinity of Alpine ophiolites to Alpine folding, a major challenge of Mediterranean geology has been to understand the fate of ocean basins preserved in the circum-Mediterranean mountain belts—how they ...
Author`s personal copy - Freie Universität Berlin
Author`s personal copy - Freie Universität Berlin

... size of Alpine Tethys and the precise age of its demise. The gap in knowledge between plate-motion studies and field-based tectonic syntheses was large, primarily because modern structural petrology and geochronology were in their infancy and also because geologists were preoccupied with understandin ...
The geological cycle of plastics and their use as a stratigraphic
The geological cycle of plastics and their use as a stratigraphic

... 1973 (Fig. 1). Development continues to this day, with some 15–20 main groups of plastic (Shah et al., 2008). The extraordinary global expansion of this now indispensible material (Andrady and Neal, 2009) can be seen in the dramatic rise of produced plastics, from the less than 2 million tonnes manu ...
The International thermodynamic equation of seawater
The International thermodynamic equation of seawater

... these quantities are fully consistent with each other.  Entropy and enthalpy are required  for an accurate description of the advection and diffusion of heat in the ocean interior and  for quantifying the ocean’s role in exchanging heat with the atmosphere and with ice.  The  Gibbs function is a fun ...
A new model for the global biogeochemical cycle of carbonyl sulfide
A new model for the global biogeochemical cycle of carbonyl sulfide

... approach that optimizes sources and sinks based on global measurements of atmospheric OCS mixing ratios collected in the NOAA network. This inversion points towards a larger global oceanic source of OCS with higher proportions of tropical emissions than previously established. The ocean is believed ...
PDF
PDF

... Depth profiles showing sound transmission losses in different ocean regimes, as predicted by a parabolic equation model (MMPE) for a low frequency (200 Hz) and high frequency (3 kHz) source at 50 m depth ................................................................................................ ...
Resolving the lithosphereasthenosphere boundary with seismic
Resolving the lithosphereasthenosphere boundary with seismic

... within the lithosphere and asthenosphere. It is still a matter of debate, however, how accurately and under what conditions surface waves can resolve the depth and thickness of the lithosphere–asthenosphere boundary (LAB). We investigate the sensitivity of Rayleigh waves to LAB properties and find t ...
Thesis proposal
Thesis proposal

... each intermediate serves as a terminal electron acceptor, albeit with sequentially increasing redox potentials that provide for moderate to marginal electron gradients within the respiratory chain. The denitrification process is not widespread throughout the ocean, but occurs in localized areas of h ...
the Zero Paradox Noble Gas Mantle
the Zero Paradox Noble Gas Mantle

... degassed from the mantle system. In this sense the numerical simulations are consistent with the 40Ar mass balance between the atmosphere and mantle reservoir. These models, however, are unable to preserve the large-scale heterogeneity predicted by models invoking geochemical layering of the mantle ...
the TRACES Science Plan (Nov 2009)
the TRACES Science Plan (Nov 2009)

... many cold-water corals in the deep sea a few produce large, complex and long-lived habitats for other species. Recent work has shown that the oldest animal in the oceans is a 4000 year old cold-water coral. Corals like this record a uniquely detailed history of seawater conditions in the chemistry o ...
Sample Midterm/Final
Sample Midterm/Final

... this mineral does not cleave. correct answer b. this mineral cleaves between the covalent bonds of shared oxygen atoms. c. the mineral cleaves between ionic bonds separating sheet pairs d. the mineral cleaves between covalent bonds separating sheet pairs e. none of the above are correct 13. Why are ...
OITHONA SIMILIS (COPEPODA: CYCLOPOIDA) - A - E-LIB
OITHONA SIMILIS (COPEPODA: CYCLOPOIDA) - A - E-LIB

... A further haplotype of O. similis was sampled in the Mediterranean Sea. However, from the genetic aspect, the haplotypes found in that area are very different. The second Mediterranean one is genetically closer to the O. frigida haplotype than to any other O. similis haplotype. Overall, almost no m ...
Mid-ocean ridges
Mid-ocean ridges

... in response to partial melting of mantle lherzolite undergoing adiabatic decompression in a narrow zone of upwelling (Fig. 5.2). Partial melting results in the formation of basaltic magma, which is injected through tensional fissures into a narrow zone only a few kilometres wide at the ridge axis. S ...
Plume heads, continental lithosphere, flood
Plume heads, continental lithosphere, flood

... mantle even though they are less voluminous than those treated by Griffiths & Campbell (1990). White & McKenzie (1989) attribute continental flood basalts (CFB) to lithospheric extension over hot upwellings while others assign a more active role to plumes in uplifting and breaking the lithosphere (R ...
Earth`s interior and tectonic plates notes
Earth`s interior and tectonic plates notes

... • Stress: the amount of force per unit area • Compression: stress caused by squeezing. Convergent boundary. • Tension: stress caused by stretching. Divergent boundary. QuickTime™ and a decompressor are needed to see this picture. ...
National Institute of Oceanography Goa, India
National Institute of Oceanography Goa, India

... pressure of CO2 (upto 62.5 nM and 700 μatm respectively) were off SW Indian coast during summer monsoon. These are the highest recorded for any oceanic surface waters. This reinforces the view that the coastal eastern boundary upwelling serve as significant source of greenhouse gases, particularly N ...
IOC-WMO-UNEP Intergovernmental Committee - unesdoc
IOC-WMO-UNEP Intergovernmental Committee - unesdoc

... U.S.A. stated that the initial implementation of GOOS (Global and Coastal modules) cannot be met with the level of resources presently being provided. Resources are even insufficient to sustain those components of the global module that have attained their initial deployment objectives. The membersh ...
Coral Reefs and Changing Seawater Carbonate Chemistry
Coral Reefs and Changing Seawater Carbonate Chemistry

... to the deeper ocean occurs via physical oceanographic (advection, diffusion) or biological processes. For example, the North Atlantic takes up CO2 disproportionately to its surface area because downward transport removes CO2-rich surface waters to the ocean interior more rapidly than in other ocean ...
Transport of Japan tsunami marine debris to the coast of British
Transport of Japan tsunami marine debris to the coast of British

... to the effects of surface currents, winds, and waves. It is important to note that the debris generated by the tsunami will be in addition to the existing debris load floating into Canadian waters and washing ashore in British Columbia every day. Existing patterns of debris deposition on shorelines ...
TSUNAMI HISTORY - RECORDED V.K.Gusiakov Tsunami
TSUNAMI HISTORY - RECORDED V.K.Gusiakov Tsunami

... International Tsunami Information Center (ITIC) in Honolulu, Hawaii (USA) in the mid-1970s. Following this initial work and in response to the recommendation of the ITSU-XI (Summary Report…, 1987), a standardized database format was developed, and the first tsunami database was compiled from many av ...
O ceanography THE OffICIAL MAGAzINE Of THE OCEANOGRAPHY SOCIETY
O ceanography THE OffICIAL MAGAzINE Of THE OCEANOGRAPHY SOCIETY

... in the overlying water column. Dispersal of larvae among vent sites is critical for population maintenance, colonization of new vents, and recolonization of disturbed vents. Historically, studying larvae has been challenging, especially in the deep sea. Advances in the last decade in larval culturin ...
Provided by the author (s) and NUI Galway in accordance with
Provided by the author (s) and NUI Galway in accordance with

... 2006a). Furthermore, primary production is not evenly distributed across the ocean. Although the highest production occurs in the shallow coastal and shelf environments (rich in light and nutrients), continental margins are important areas of export. The margins are the ocean's gateway, forming a tr ...
Science Plan - Scientific Committee on Oceanic Research
Science Plan - Scientific Committee on Oceanic Research

... courtesy of Centre for Marine Science and Technology, Curtin University, Perth, Western Australia. ...
Iodine chemistry reflects productivity and denitrification in the
Iodine chemistry reflects productivity and denitrification in the

... Fig. 1. Stations (filled circles) shown from R/V Thomas G. Thompson US JGOFS Spring Intermonsoon cruise TN045, ...
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Physical oceanography



Physical oceanography is the study of physical conditions and physical processes within the ocean, especially the motions and physical properties of ocean waters.Physical oceanography is one of several sub-domains into which oceanography is divided. Others include biological, chemical and geological oceanographies.
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