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Common signals between physical and atmospheric variables and
Common signals between physical and atmospheric variables and

... climatic signal is possibly present in the oceanic biota. Finally, the 14-month periodicity observed is similar to that found in another oscillation, the Pole Tide, also known as Chandler wobble. Originally found in 1891, following analysis of astronomical data by Chandler, as an oscillation of the ...
Chapter 1 - Beck-Shop
Chapter 1 - Beck-Shop

... analogous to the very thin skin on an apple. The crust is separated from the underlying mantle by the Mohorovičić (Moho) discontinuity. Two major types of crust occur. Oceanic crust Oceanic crust is composed largely of darkcolored, mafic rocks enriched in oxides of magnesium, iron and calcium (MgO ...
PowerPoint
PowerPoint

... the earth's crust. It is this squeezing of the crust that causes the 300 or so small earthquakes that are located in southwestern British Columbia each year, and the less-frequent (once per decade, on average, damaging crustal earthquakes (e.g., a magnitude ...
Divergent Plate Boundaries
Divergent Plate Boundaries

... Convergent plate boundaries are locations where lithospheric plates are moving towards one another. The plate collisions that occur in these areas can produce earthquakes, volcanic activity and crustal deformation. Convergent Plate Boundary – Oceanic-Continental: When continental and oceanic plates ...
PDF - compatibile with Acrobat 4.0
PDF - compatibile with Acrobat 4.0

... Waves longer than the peak wavelength make only a very small contribution to the surface slope, and the influence of high frequency wave components on the statistics of sea surface slopes is substantial. In the classical JONSWAP spectrum (Massel 1996), the high-frequency tail is represented in the fo ...
Influence of bacterial uptake on deep
Influence of bacterial uptake on deep

... bacterial production has also been shown to correlate with both temperature and chlorophyll in the surface layers of the global ocean [Rivkin and Legendre, 2001]. From these experiments we also determine a yield factor of w = 0.33 which lies within the range of earlier reported values for the marine ...
Plate tectonics
Plate tectonics

...  Emperor Sea Mount chain  islands or sea mountains formed over hotspots (fixed area where magma comes up) ...
Convergent Plate Boundaries
Convergent Plate Boundaries

... • Earth’s interior is layered, and the layers are arranged by density. Each deeper layer is denser than the layer above. • Continents are not supported above sea level by resting mechanically on a rigid base. Instead, continents rise to great height because they “float” on a dense, deformable layer ...
Geology 3015 Lecture Notes Week 4b
Geology 3015 Lecture Notes Week 4b

... • Plate tectonics has had a profound affect on Earth’s geologic and biologic history. • Interaction of plates along their boundaries controls the distribution of most earthquakes and volcanoes as well as the formation of mountain ranges. • Geologists recognize three major types of plate boundaries b ...
Key Concept Review (Answers to in-text “Concept Checks”) Chapter
Key Concept Review (Answers to in-text “Concept Checks”) Chapter

... process, the ocean's sedimentary "memory" does not start with the ocean’s formation as originally reasoned by early marine scientists. 25. Scientists now have instruments capable of analyzing very small variations in the relative abundances of the stable isotopes of oxygen preserved within the carbo ...
The NOAA Ship Okeanos Explorer To Boldly Go…
The NOAA Ship Okeanos Explorer To Boldly Go…

... CIRCULATIONv4(# WHICHPLAYSANIMPORTANTROLEIN transporting heat, dissolved oxygen and nutrients. Dense water sinking in the North Atlantic Ocean is one of the principal forces that drives the circulation of the THC, and there are growing concerns about how these forces may be affected by cha ...
Chapter I - Shodhganga
Chapter I - Shodhganga

... part of the world has an area of about 361 million sq km, an average depth of about 3,730 m and a total volume of about 1,347,000 million cubic km. The deepest part of the oceans is the Mariana Trench (11,516 m) in the Pacific Ocean. Compare this with the Mount Everest, 8,849 m above sea level of th ...
Image: Marine biologists use plankton nets to sample phytoplankton
Image: Marine biologists use plankton nets to sample phytoplankton

... photosynthesis to turn it into chemical energy. They consume carbon dioxide, and release oxygen. All phytoplankton photosynthesize, but some get additional energy by consuming other organisms. Phytoplankton growth depends on the availability of carbon dioxide, sunlight, and nutrients. Phytoplankton, ...
- Marine Spatial Ecology Lab
- Marine Spatial Ecology Lab

... region-wide categorization of the physical environments of the Caribbean Sea (PECS). The classification approach is hierarchical and focuses on physical constraints that drive many aspects of coastal ecology, including species distributions, ecosystem function, and disturbance. The first level repre ...
Thermodynamic Properties
Thermodynamic Properties

... 4.1.4 Mantle Convection and Mantle Temperatures The acceptance of mantle convection in the late 1960s provided a natural explanation for the high thermal gradients near the Earth's surface; they are a consequence of thermal boundary layers associated with mantle convection. Beneath the boundary laye ...
Shallow-Water Waves
Shallow-Water Waves

... Wave Speed is C - Group Speed is V wave speed = wavelength / period or C=L/T T is determined by generating force so it remain the same after the wave formed, but C changes. In general, the longer the wavelength the faster the wave energy will move through the water. ...
4.3 Read
4.3 Read

... you thought about heating water in a pot as a model of convection in the mantle. All of these can help you understand how convection might occur in Earth’s mantle. Like any model in science, though, there are some parts of the models you thought about that do not represent the real thing very well. ...
Ocean Science - International Science Center
Ocean Science - International Science Center

... year. It is strongest in the tropics and decreases to non-existent in the polar winter season. ...
Report - My FIT (my.fit.edu)
Report - My FIT (my.fit.edu)

... Due to a large gap in NDBC station coverage on the East coast of Florida, LOCOS has designed hurricane stations along the continental shelf and stations leading back to the coast on the northern and southern boundaries of the state. These stations are out this far in order to detect hurricanes and t ...
North Atlantic ecosystem sensitivity to Holocene shifts in Meridional
North Atlantic ecosystem sensitivity to Holocene shifts in Meridional

... surface water masses northward and deeper southward circulation of cooler, fresher waters [Hansen and Østerhus, 2000; Read, 2001]. The surface limb of the AMOC, the North Atlantic Current (NAC), loses much of its heat to the atmosphere on its way north, which helps regulate the climate over Europe [ ...
Projected changes in Arctic Ocean freshwater budgets
Projected changes in Arctic Ocean freshwater budgets

... analysis of sea ice transport and storage, ocean transport and storage, and net surface flux exchange. Simulated budgets for the late 20th century are compared to available observations, followed by an analysis of simulated changes from 1950 to 2050. The consistent theme over this period is an accel ...
The Inside of Earth: Deep-Earth Science from the Top Down
The Inside of Earth: Deep-Earth Science from the Top Down

... and trench system once existed off the California coast, but the ridge was overridden by North America. The ridge and trench collided and annihilated each other, and now western North America sits on top of what used to be the East Pacific rise. The tomographic images show reddish regions underneath ...
Seamobile Guide 2001 - Natural History Museum of Los Angeles
Seamobile Guide 2001 - Natural History Museum of Los Angeles

... student understanding. In most cases, students already have some preconceptions of a new topic or area of study, having gathered ideas from experience in the world around them. Unfortunately, these preconceptions may be inaccurate, and are often difficult to adjust or dispel altogether. One way to i ...
ppt link
ppt link

... Convergent plate boundaries have the following characteristics: 1. plate motion is toward plate boundary, 2. oceanic lithosphere sinks back into Earth and is recycled, 3. the volcanic arc is region of highly explosive volcanoes, like Mt. St. Helens and Mt. Rainer in Washington, 4. The plate boundary ...
Earthquakes
Earthquakes

... Along low lying coasts of Java the waves washed 8 km onshore, dragging people along with them as they washed back to sea. The tsunami was recorded as a small rise in sea level as far away as the California coast (20 hours after the fourth blast). An estimated 36,417 people were killed by the tsunami ...
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Ocean



An ocean (from Ancient Greek Ὠκεανός, transc. Okeanós, the sea of classical antiquity) is a body of saline water that composes much of a planet's hydrosphere. On Earth, an ocean is one of the major conventional divisions of the World Ocean, which covers almost 71% of its surface. These are, in descending order by area, the Pacific, Atlantic, Indian, Southern, and Arctic Oceans. The word sea is often used interchangeably with ""ocean"" in American English but, strictly speaking, a sea is a body of saline water (generally a division of the world ocean) partly or fully enclosed by land.Saline water covers approximately 72% of the planet's surface (~3.6×108 km2) and is customarily divided into several principal oceans and smaller seas, with the ocean covering approximately 71% of Earth's surface. The ocean contains 97% of Earth's water, and oceanographers have stated that only 5% of the World Ocean has been explored. The total volume is approximately 1.35 billion cubic kilometers (320 million cu mi) with an average depth of nearly 3,700 meters (12,100 ft).As it is the principal component of Earth's hydrosphere, the world ocean is integral to all known life, forms part of the carbon cycle, and influences climate and weather patterns. It is the habitat of 230,000 known species, although much of the oceans depths remain unexplored, and over two million marine species are estimated to exist. The origin of Earth's oceans remains unknown; oceans are thought to have formed in the Hadean period and may have been the impetus for the emergence of life.Extraterrestrial oceans may be composed of water or other elements and compounds. The only confirmed large stable bodies of extraterrestrial surface liquids are the lakes of Titan, although there is evidence for the existence of oceans elsewhere in the Solar System. Early in their geologic histories, Mars and Venus are theorized to have had large water oceans. The Mars ocean hypothesis suggests that nearly a third of the surface of Mars was once covered by water, and a runaway greenhouse effect may have boiled away the global ocean of Venus. Compounds such as salts and ammonia dissolved in water lower its freezing point, so that water might exist in large quantities in extraterrestrial environments as brine or convecting ice. Unconfirmed oceans are speculated beneath the surface of many dwarf planets and natural satellites; notably, the ocean of Europa is estimated to have over twice the water volume of Earth. The Solar System's giant planets are also thought to have liquid atmospheric layers of yet to be confirmed compositions. Oceans may also exist on exoplanets and exomoons, including surface oceans of liquid water within a circumstellar habitable zone. Ocean planets are a hypothetical type of planet with a surface completely covered with liquid.
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