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Earthquakes - Earth Science
Earthquakes - Earth Science

... The point where the rock first breaks is called the focus of an earthquake. The point directly above the focus on the Earth’s surface is the epicenter. After an earthquake event, smaller earthquakes called aftershocks often occur near the focus of the original earthquake. ...
Synchronicity of Kuroshio Current and climate system variability
Synchronicity of Kuroshio Current and climate system variability

... The Kuroshio Current (KC) is the northward branch of the North Pacific subtropical gyre (NPG) and exerts influence on the exchange of physical, chemical, and biological properties of downstream regions in the Pacific Ocean. Resolving long-term changes in the flow of the KC water masses is, therefore, cr ...
Pronounced zonal heterogeneity in Eocene southern high
Pronounced zonal heterogeneity in Eocene southern high

... findings (24, 25) that the relationship between molluscan carbonate growth temperature and Δ47 agrees with inorganic calcite calibration data. Some recently published clumped isotope analyses of modern bivalve shells have suggested the possibility of significant deviations from the synthetic-calcite ...
GSA-Charlotte 2012
GSA-Charlotte 2012

... Earth’s tectonic, biogeochemical and paleoceanographic record. Subdividing the cycle into three main phases – supercontinentality, breakup and dispersal, and supercontinent assembly – they identified a variety of trends in tectonic activity, platform sedimentation, climate, life, and the stable isot ...
On Which Crust Do Volcanoes Form? - EHS
On Which Crust Do Volcanoes Form? - EHS

... 7) Set the thickness and composition of your crust somewhere in the middle. a) What type of crust do you have? b) What happens when you change the temperature of the crust? ...
Development of an operational coastal flooding early warning system
Development of an operational coastal flooding early warning system

... The northwestern part of the Pacific Ocean globally features numerous and intense tropical cyclones (typhoons). With strong wind entering the coast, the direct force by huge waves and rising sea levels caused by storm surges resulting from typhoons destruct the coastal defense, accelerate the coasta ...
Earthquakes
Earthquakes

... (height) of the largest seismic wave - Moment magnitude: determined from the displacement (movement) of the fault zone ...
Word - Manchester Geological Association
Word - Manchester Geological Association

... Generally, the lithological composition of each locality is harzburgitic, and hosts lenses and layers of dunite, chromitite and pyroxenite that are interpreted as representing SSZ-related (channelised) melt migration and melt-rock interaction. Although the bulk of the harzburgitic rocks have approxi ...
Multiple Equilibria as a Possible Mechanism for
Multiple Equilibria as a Possible Mechanism for

... become a research topic of continued interest. Geostrophic velocities derived from satellite altimetry data show a distinct weakening of the gyre by 7–10 Sv (1 Sv [ 106 m3 s21) (Häkkinen and Rhines 2004), corresponding to up to one-quarter of its total volume transport of 37– 42 Sv (Bacon 1997; Read ...
Seamobile Guide 2001 - Natural History Museum of Los Angeles
Seamobile Guide 2001 - Natural History Museum of Los Angeles

... 2. Next, ask students to take a piece of paper and fold it in half lengthwise, creating two columns. Ask students to write “Deep Sea Environment” at the top of the left side; then ask them to list short descriptions of what the underwater environment is like in that column. Descriptions should be br ...
Oceans and Coasts
Oceans and Coasts

... Ocean Water Temperature Ocean surface T varies inversely with latitude.  Water buffers wide T shifts moderating climate.  Surface water approaches a uniform T with depth.  Ocean bottom water is near freezing < 4 °C (39 °F) ...
Wind direction over the ocean determined by an
Wind direction over the ocean determined by an

... On November 27, the wind conditions were less favorable. At the time of data collection (around noon local time) the wind speed was 6 m/s with a 110 direction, but during the morning, the wind had dropped gradually from 10 m/s, 330 to a zero wind speed and direction jump to 110 just one hour prior t ...
An analysis of young ocean depth, gravity and global residual
An analysis of young ocean depth, gravity and global residual

... Since then, a number of physical explanations have been put forward for this flattening. These include (1) the addition of heat from convective instability underneath the rigid mechanical boundary layer (Parsons & McKenzie 1978); (2) radioactive heating in the upper part of the mantle (Forsyth 1977) ...
The strengthening East Australian Current, its eddies and
The strengthening East Australian Current, its eddies and

... et al. (2011) investigate physical processes in the ocean along the coast of southeastern Australia. A high resolution hindcast of ocean state from 1992 – 2006 using a Bluelink assimilation product (BODAS) is used to investigate connectivity of nonswimming particles such as planktonic larvae, eggs a ...
CTENOPHORA comb jellies, ctenophores
CTENOPHORA comb jellies, ctenophores

... disturbed [1]. ...
Slide 1
Slide 1

... When rocks are strained beyond their limit, they break and grind past each other, releasing huge amounts of energy in the form of an earthquake. As the rocks break and move, potential energy is transformed into kinetic energy in the form of seismic waves. ...
Chapter 22: Section 5
Chapter 22: Section 5

... When rocks are strained beyond their limit, they break and grind past each other, releasing huge amounts of energy in the form of an earthquake. As the rocks break and move, potential energy is transformed into kinetic energy in the form of seismic waves. ...
Quaking, Shaking, Earth
Quaking, Shaking, Earth

... much upward or downward movement. • The San Andreas Fault is the boundary between two of Earth’s plates that are moving sideways past each other. ...
PDF - Oxford Academic - Oxford University Press
PDF - Oxford Academic - Oxford University Press

... DO, there is no single value of pH (or any other carbonatesystem variable) that can be used as a ubiquitous “threshold” for biologically significant effects. The challenges from OA differ among oceanic regions. OA effects may be particularly strong in regions such as the CCS, where anthropogenic CO2 ...
The Science of Tsunamis
The Science of Tsunamis

... attenuated by viscous damping in the water. For a large tsunami, all three effects are minimal. Since the energy for initiation occurs along an extended fault, the waves spread out linearly rather than cylindrically, resulting in little spreading. For extremely long wavelengths, the waves are not hi ...
Lab: Exploring Patterns in Regional Seismicity
Lab: Exploring Patterns in Regional Seismicity

... Geomorphology - the study of the physical features of the surface of the earth and their relation to its geological structures Background: Plate Tectonics The lithosphere can be divided into many large plates, which are moved around the surface of the planet over time. During this motion, plates int ...
File
File

... Why is molten magma rising to the surface at divergent plate boundaries? A. because it is more dense than the hotter rock around it B. because it is affected by anti-gravity C. because it is less dense than the cooler rock surrounding ...
national unit specification: general information
national unit specification: general information

... candidates will also gain a knowledge of the local weather conditions associated with the Monsoon. Outcome 4 This Outcome explores the general circulation of the atmosphere and examines the main climatic zones over the ocean. This includes the global pressure distribution and the prevailing winds du ...
conference handbook
conference handbook

... ResponSEAble aims at supporting the emergence of an effective and dynamic European ocean knowledge system that contributes to raising awareness on everybody’s (individual and collective, direct and indirect) responsibility and interest in a healthy and sustainable ocean. The ResponSEAble project wil ...
Plate Tectonics -- Structure and Behavior of Oceanic Ridges
Plate Tectonics -- Structure and Behavior of Oceanic Ridges

... “Mid-Atlantic Ridge”. (Except north of this large transform fault, where it is called the Reykjanes Ridge. It is still the same spreading center.) This works also in the Indian Ocean, where there is a “Mid-Indian Ridge”, but not in the Pacific (East Pacific Rise) or Arctic (Nansen Ridge) where the r ...
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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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