Ocean Storage of CO2
... for carbon from the atmosphere to reach the deep ocean. This can be estimated from observations of 14C. Correcting for mixing with waters from various sources (polar ice, rivers, other oceans), the age of North Pacific deep water is estimated to be between 700 and 1000 years, while other basins, suc ...
... for carbon from the atmosphere to reach the deep ocean. This can be estimated from observations of 14C. Correcting for mixing with waters from various sources (polar ice, rivers, other oceans), the age of North Pacific deep water is estimated to be between 700 and 1000 years, while other basins, suc ...
Isotopic Tracers of the Marine Nitrogen Cycle: Present and Past
... Trichodesmium lacks heterocysts and in fact couples photosynthetic energy production to N2 fixation. How O2 inhibition is overcome is not well understood. The high requirement for Fe has further suggested an interaction between Fe and N biogeochemistry [6]. Since Fe is chiefly supplied by eolian dust ...
... Trichodesmium lacks heterocysts and in fact couples photosynthetic energy production to N2 fixation. How O2 inhibition is overcome is not well understood. The high requirement for Fe has further suggested an interaction between Fe and N biogeochemistry [6]. Since Fe is chiefly supplied by eolian dust ...
Full text in pdf format
... bacteria attached to particles (Kim 1985). But hydrolysates of aggregates of relativlely fresh particles in the mesopelagic zone should be mostly highly nutritious for bacteria and they are nearly entirely taken up by the bacteria inhabiting the water phase around the particles (which were of course ...
... bacteria attached to particles (Kim 1985). But hydrolysates of aggregates of relativlely fresh particles in the mesopelagic zone should be mostly highly nutritious for bacteria and they are nearly entirely taken up by the bacteria inhabiting the water phase around the particles (which were of course ...
23. Air Gun-Ocean Bottom Seismograph Seismic Structure across
... crust. Provided that the Moho depth is shallower than - 2 0 km, there is a good chance of observing PmP phase to define its depth. The apparent lack of arrivals from Layer 2 beneath the sedimentary prism at the lower inner trench slope is in agreement with another set of OBS-air gun refraction data ...
... crust. Provided that the Moho depth is shallower than - 2 0 km, there is a good chance of observing PmP phase to define its depth. The apparent lack of arrivals from Layer 2 beneath the sedimentary prism at the lower inner trench slope is in agreement with another set of OBS-air gun refraction data ...
VERTIGO (VERtical Transport In the Global Ocean): A study of
... blocks of marine particles in the surface ocean, and study changes in relative composition and flux with depth of carbon and associated elements. Our two initial hypotheses were that: (1) particle source characteristics determine transport efficiency of sinking particles and/or (2) mid-water processes ...
... blocks of marine particles in the surface ocean, and study changes in relative composition and flux with depth of carbon and associated elements. Our two initial hypotheses were that: (1) particle source characteristics determine transport efficiency of sinking particles and/or (2) mid-water processes ...
Welcome to Vibrationdata Megathrust Earthquake Disaster
... The speed slows in shallow depths due to frictional effects between the water and the seafloor. Most tsunamis do not create giant breaking waves on shore. Rather they generate fast tides that cause a rapid sea level rise, particularly as the tsunami reaches a shallow harbor. ...
... The speed slows in shallow depths due to frictional effects between the water and the seafloor. Most tsunamis do not create giant breaking waves on shore. Rather they generate fast tides that cause a rapid sea level rise, particularly as the tsunami reaches a shallow harbor. ...
AMSR-E Ocean Algorithms - Remote Sensing Systems
... atmosphere [Wentz and Meissner, 2000]. The simulation is based on a set of 42,195 radiosonde soundings launched from weather ships and small islands around the globe [Wentz, 1997]. These radiosondes are used to specify the atmospheric part of the RTM. A cloud layer of various columnar liquid cloud w ...
... atmosphere [Wentz and Meissner, 2000]. The simulation is based on a set of 42,195 radiosonde soundings launched from weather ships and small islands around the globe [Wentz, 1997]. These radiosondes are used to specify the atmospheric part of the RTM. A cloud layer of various columnar liquid cloud w ...
Experiments With Portable Ocean Bottom - OBSIP
... that control fault behavior requires studying the structure and slip patterns in detail in a number of different tectonic settings. The importance of ocean bottom studies is obvious; approximately 90% of the world’s plate boundaries are in the ocean. The locked portion of subduction zones that tend ...
... that control fault behavior requires studying the structure and slip patterns in detail in a number of different tectonic settings. The importance of ocean bottom studies is obvious; approximately 90% of the world’s plate boundaries are in the ocean. The locked portion of subduction zones that tend ...
Research on Hydrothermal Vents-Amit
... Some of the most successful vent animals, tube worms and giant clams, form symbiotic relationships with chemosynthetic bacteria. The bacteria live within the animals' tissues and provide a built-in food supply. Tube worms have no mouth, gut, or anus. Nutrients are absorbed directly into tissues. Tw ...
... Some of the most successful vent animals, tube worms and giant clams, form symbiotic relationships with chemosynthetic bacteria. The bacteria live within the animals' tissues and provide a built-in food supply. Tube worms have no mouth, gut, or anus. Nutrients are absorbed directly into tissues. Tw ...
- NERC Open Research Archive
... which observations of 8 biogeochemically relevant variables must be made to robustly detect ...
... which observations of 8 biogeochemically relevant variables must be made to robustly detect ...
Plate Tectonics Introduction Boundaries between crustal plates
... masses plow through oceanic rock. Because oceanic rock is more rigid than continental rock, and because he failed to provide an acceptable mechanism to account for how continents could have drifted great distances (not to mention the fact that Wegener was a meteorologist) his ideas were widely rejec ...
... masses plow through oceanic rock. Because oceanic rock is more rigid than continental rock, and because he failed to provide an acceptable mechanism to account for how continents could have drifted great distances (not to mention the fact that Wegener was a meteorologist) his ideas were widely rejec ...
Bioregionalisation of the Southern Ocean - WWF
... attributes, and contain different habitat types and communities of species. These different regions may occur adjacent to one another; however, each differs from the others in terms of physical and ecological characteristics. Some species may range across more than one region, whereas others will be ...
... attributes, and contain different habitat types and communities of species. These different regions may occur adjacent to one another; however, each differs from the others in terms of physical and ecological characteristics. Some species may range across more than one region, whereas others will be ...
Temperature Models for Mexican Subduction Zone
... The upper and lower boundaries of the model are maintained at constant temperatures of 0 ºC and 1450 ºC (asthenosphere), correspondingly. The right (landward) vertical boundary condition is defined by a 20 ºC/km thermal gradient for the continental crust. This value is in agreement with the back arc ...
... The upper and lower boundaries of the model are maintained at constant temperatures of 0 ºC and 1450 ºC (asthenosphere), correspondingly. The right (landward) vertical boundary condition is defined by a 20 ºC/km thermal gradient for the continental crust. This value is in agreement with the back arc ...
THE RISE OF TEOTIHUACAN
... incorporated in Earth’s core as the planet cooled and consolidated. lr is found in high concentrations in some meteorites, in which the solar system’s original chemical composition is preserved. Even today, microscopic meteorites continually bombard Earth, falling on both land and sea. By measuring ...
... incorporated in Earth’s core as the planet cooled and consolidated. lr is found in high concentrations in some meteorites, in which the solar system’s original chemical composition is preserved. Even today, microscopic meteorites continually bombard Earth, falling on both land and sea. By measuring ...
Drawing Magma - Volcanoes Alive!
... Hotspots are plumes of magma that migrate toward Earth’s surface from one spot. Magma flows from these hotspots, and piles up to form shield volcanoes above them. More than 100 hotspots around the world have been active over the past 10 million years. Convergent boundaries: Many cracks form at conve ...
... Hotspots are plumes of magma that migrate toward Earth’s surface from one spot. Magma flows from these hotspots, and piles up to form shield volcanoes above them. More than 100 hotspots around the world have been active over the past 10 million years. Convergent boundaries: Many cracks form at conve ...
Causes of Tsunami - Tsunami: Magnitude of Terror
... • Tsunamis are characterized as shallow-water waves due to their long periods and wavelengths. • A wind-generated wave might have a period of ten seconds and a wavelength of 150 meters, but it is possible for a tsunami to have a wavelength more than 100 kilometers and a period on the order of one ho ...
... • Tsunamis are characterized as shallow-water waves due to their long periods and wavelengths. • A wind-generated wave might have a period of ten seconds and a wavelength of 150 meters, but it is possible for a tsunami to have a wavelength more than 100 kilometers and a period on the order of one ho ...
Document
... the YOUNGER, WARMER, LESS DENSE plate, forming a topographical feature known as a DEEP-SEA TRENCH. Trenches are long, narrow, deep-cutting canyons (8 to 10 km deep) formed by slab pull (negative buoyancy) as the old, cold lithosphere descends into the hotter, less dense asthenosphere. The older, ...
... the YOUNGER, WARMER, LESS DENSE plate, forming a topographical feature known as a DEEP-SEA TRENCH. Trenches are long, narrow, deep-cutting canyons (8 to 10 km deep) formed by slab pull (negative buoyancy) as the old, cold lithosphere descends into the hotter, less dense asthenosphere. The older, ...
Chapter 36 F Open Ocean Deep Sea
... test the mechanisms that underlie latitudinal patterns in different fauna. Broad-scale depth and latitudinal patterns in benthic diversity are modified regionally by a variety of environmental factors operating at different scales. For example, OMZs strongly affect diversity where they impinge on th ...
... test the mechanisms that underlie latitudinal patterns in different fauna. Broad-scale depth and latitudinal patterns in benthic diversity are modified regionally by a variety of environmental factors operating at different scales. For example, OMZs strongly affect diversity where they impinge on th ...
Global Oceans Governance: New and Emerging Issues
... of oceans. Western constructions of oceans as unpeopled support a commitment to freedom of the seas (14). In the post–World War II era, nationalized spaces of the EEZ and UN measures for ABNJ reflected evolving understanding of biophysical features and changing political and social commitments (9, 1 ...
... of oceans. Western constructions of oceans as unpeopled support a commitment to freedom of the seas (14). In the post–World War II era, nationalized spaces of the EEZ and UN measures for ABNJ reflected evolving understanding of biophysical features and changing political and social commitments (9, 1 ...
File
... • The Earth’s surface is continually battered by wind and scoured by running water, which moves rocks around and changes their appearance. • Erosion is the process in which the materials of the Earth’s surface are loosened, dissolved, or worn away and transported form one place to another by a natur ...
... • The Earth’s surface is continually battered by wind and scoured by running water, which moves rocks around and changes their appearance. • Erosion is the process in which the materials of the Earth’s surface are loosened, dissolved, or worn away and transported form one place to another by a natur ...
A proposed biogeography of the deep ocean floor
... 1962), whereas others, such as the polychaetes, were thought to be widespread (Kirkegaard, 1995). Knudson (1970) also considered the Bivalvia to be widely distributed, but only three of 193 species appeared to be cosmopolitan (Vinogradova, 1997). Menzies et al. (1973) summarized the distributions of ...
... 1962), whereas others, such as the polychaetes, were thought to be widespread (Kirkegaard, 1995). Knudson (1970) also considered the Bivalvia to be widely distributed, but only three of 193 species appeared to be cosmopolitan (Vinogradova, 1997). Menzies et al. (1973) summarized the distributions of ...
Plate Tectonics Reading
... Boundaries between crustal plates The first type of plate boundary is found on the mid ocean ridge (MOR) system (e.g., the Mid Atlantic Ridge, the East Pacific Rise), where lava of basaltic composition upwells from the mantle and flows out onto the ocean floor where it cools and solidifies to creat ...
... Boundaries between crustal plates The first type of plate boundary is found on the mid ocean ridge (MOR) system (e.g., the Mid Atlantic Ridge, the East Pacific Rise), where lava of basaltic composition upwells from the mantle and flows out onto the ocean floor where it cools and solidifies to creat ...
Reply to reviewer ESDD-1-C149-2011 comments on “Assessing
... instantaneous extinction of life. We are very grateful for the suggestion of additional contributions and have included them in the manuscript. Following Schwartman & Volk (1989), it is important to note that if the geological carbon cycle were to relax to a steady state, then weathering of CO2 woul ...
... instantaneous extinction of life. We are very grateful for the suggestion of additional contributions and have included them in the manuscript. Following Schwartman & Volk (1989), it is important to note that if the geological carbon cycle were to relax to a steady state, then weathering of CO2 woul ...
Tides, lecture 9
... TIDES • periodic, short term changes in the height of the ocean surface at a particular place ...
... TIDES • periodic, short term changes in the height of the ocean surface at a particular place ...
Future of the Ocean and its Seas: a non
... nations – Canada, France, Germany, Italy, Japan, UK and USA – not only have direct responsibility for around 40 million km2 of marine habitat (nearly twice their total land area), but together they produce the overwhelming majority (more than 80%; Jappe, 2007) of oceanographic scientific publication ...
... nations – Canada, France, Germany, Italy, Japan, UK and USA – not only have direct responsibility for around 40 million km2 of marine habitat (nearly twice their total land area), but together they produce the overwhelming majority (more than 80%; Jappe, 2007) of oceanographic scientific publication ...
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.