Accurate focal depth determination of oceanic earthquakes using
... only P-wave arrival time data from teleseismic stations, the focal depth is in many cases poorly constrained. For example, Mendiguren (1971) studied an intraplate earthquake occurring on November 25, 1965 with an origin time of 10:50:40.2 and epicenter of 17.1◦ S and 100.2◦ W. The focal depth was es ...
... only P-wave arrival time data from teleseismic stations, the focal depth is in many cases poorly constrained. For example, Mendiguren (1971) studied an intraplate earthquake occurring on November 25, 1965 with an origin time of 10:50:40.2 and epicenter of 17.1◦ S and 100.2◦ W. The focal depth was es ...
Aluminium in an ocean general circulation model compared with the
... and Bruland, 1986; Moran and Moore, 1989; Bruland and Lohan, 2006). This is the combination of adsorption onto a solid surface, followed by sinking due to insufficient buoyancy of the particulates in the seawater (Goldberg, 1954; Bacon and Anderson, 1982; Bruland and Lohan, 2006). Typically, scaveng ...
... and Bruland, 1986; Moran and Moore, 1989; Bruland and Lohan, 2006). This is the combination of adsorption onto a solid surface, followed by sinking due to insufficient buoyancy of the particulates in the seawater (Goldberg, 1954; Bacon and Anderson, 1982; Bruland and Lohan, 2006). Typically, scaveng ...
Modeling of the Total Alkalinity and the Total Inorganic Carbon
... 2005. The reason for the slightly less steep slope and the less negative intercept in our correlation (Eq.1) compared to the other one (Eq.I) could be attributed to the difference of sampling locations (different specific total alkalinities between the Western and the Eastern basins). Located in the ...
... 2005. The reason for the slightly less steep slope and the less negative intercept in our correlation (Eq.1) compared to the other one (Eq.I) could be attributed to the difference of sampling locations (different specific total alkalinities between the Western and the Eastern basins). Located in the ...
investigation of the Red Sea circulation
... formation of the very saline outflowing water mass inside the basin, the buoyancy loss (mostly due to the large evaporation rate) has been thought by several investigators to be the basic controlling mechanism of the flow [Maury, 1855; Luksch, 1901; Neumann and McGill, 1962; Phillips, 1966; Tragou a ...
... formation of the very saline outflowing water mass inside the basin, the buoyancy loss (mostly due to the large evaporation rate) has been thought by several investigators to be the basic controlling mechanism of the flow [Maury, 1855; Luksch, 1901; Neumann and McGill, 1962; Phillips, 1966; Tragou a ...
Full text in pdf format
... ABSTRACT: This paper presents the general framework of a n ecological model of the English Channel. The model is a result of combining a physical sub-model with a biological one. In the physical submodel, the Channel is divided into 71 boxes and water fluxes between them a r e calculated automatical ...
... ABSTRACT: This paper presents the general framework of a n ecological model of the English Channel. The model is a result of combining a physical sub-model with a biological one. In the physical submodel, the Channel is divided into 71 boxes and water fluxes between them a r e calculated automatical ...
2MA-12 Draft guidelines for measuring Secchi depth
... Secchi depth is measured at stations when the ship is still: under calm seas, or while being held at the position using thrusters. Should the thrusters / side-propellers being used, they may cause considerable advection at typical Secchi depths which has to be accounted for. Allow sufficient time (p ...
... Secchi depth is measured at stations when the ship is still: under calm seas, or while being held at the position using thrusters. Should the thrusters / side-propellers being used, they may cause considerable advection at typical Secchi depths which has to be accounted for. Allow sufficient time (p ...
Modelling the tides and their impacts on the vertical stratification
... south-eastward direction. Figure 4a shows the elevation at high tide with the amplitude decreasing from 2.9 m at the coast at Beira to 1.9 m at the shelf edge. The maximum was located in the Pungwe River and the amplitude reduced along nearly straight lines parallel to the bathymetry. Two hours late ...
... south-eastward direction. Figure 4a shows the elevation at high tide with the amplitude decreasing from 2.9 m at the coast at Beira to 1.9 m at the shelf edge. The maximum was located in the Pungwe River and the amplitude reduced along nearly straight lines parallel to the bathymetry. Two hours late ...
Earth-9th-Edition-Tarbuck-Solution-Manual
... together based on their similar coastlines. 3. Pangaea was the supercontinent that existed in late Paleozoic time when Gondwanaland (the Southern Hemisphere landmass composed of Africa, India, South America, Australia, India, and Antarctica) collided with North America to form one, super-large landm ...
... together based on their similar coastlines. 3. Pangaea was the supercontinent that existed in late Paleozoic time when Gondwanaland (the Southern Hemisphere landmass composed of Africa, India, South America, Australia, India, and Antarctica) collided with North America to form one, super-large landm ...
Essential Question: How does the position of the Earth and
... causes the ocean water to bulge out in the direction of the moon. ...
... causes the ocean water to bulge out in the direction of the moon. ...
Closing the Global Water Vapor Budget with AIRS
... evaporation data from the Goddard Satellite-based Surface Turbulent Fluxes (GSSTF). The atmospheric total water vapor sink (S) is estimated from AIRS water vapor retrievals with MERRA winds (AIRS–MERRA S) as well as directly from the MERRA water vapor budget (MERRA–MERRA S). The global geographical ...
... evaporation data from the Goddard Satellite-based Surface Turbulent Fluxes (GSSTF). The atmospheric total water vapor sink (S) is estimated from AIRS water vapor retrievals with MERRA winds (AIRS–MERRA S) as well as directly from the MERRA water vapor budget (MERRA–MERRA S). The global geographical ...
Overview Plate Tectonics
... bottom. Only seven megaplumes in the world had been observed previously. ...
... bottom. Only seven megaplumes in the world had been observed previously. ...
GSA-Charlotte 2012
... Their calculations suggested that the crustal extension and creation of young ocean basins associated with supercontinent breakup would first cause sea level to rise, only to fall as the the new oceans aged. During supercontinent assembly, on the other hand, subduction of old ocean floor coupled wit ...
... Their calculations suggested that the crustal extension and creation of young ocean basins associated with supercontinent breakup would first cause sea level to rise, only to fall as the the new oceans aged. During supercontinent assembly, on the other hand, subduction of old ocean floor coupled wit ...
Chapter 8: Atmospheric Circulation and Pressure Distributions
... The NAO is the dominant mode of winter climate variability in the North Atlantic region ranging from central North America to Europe and much into Northern Asia. ...
... The NAO is the dominant mode of winter climate variability in the North Atlantic region ranging from central North America to Europe and much into Northern Asia. ...
Diversity of Arctic pelagic Bacteria with an
... 2009). In both polar oceans, picocyanobacteria follow a general trend of decreasing concentrations and relative abundance with increasing latitudes, and strong inverse correlations between cell densities and temperature have been reported (Marchant et al., 1987; Murphy and Haugen, 1985; Rosenbergl, ...
... 2009). In both polar oceans, picocyanobacteria follow a general trend of decreasing concentrations and relative abundance with increasing latitudes, and strong inverse correlations between cell densities and temperature have been reported (Marchant et al., 1987; Murphy and Haugen, 1985; Rosenbergl, ...
Nature of the Vrancea seismic zone (Eastern Carpathians) – New
... a b s t r a c t The Vrancea region of the southeastern Carpathians is one of the most active seismic zones in Europe and it is well-known for its strong intermediate depth earthquakes. Seismic tomography had revealed a high-velocity body beneath Vrancea and the Moesian platform that extends to a dep ...
... a b s t r a c t The Vrancea region of the southeastern Carpathians is one of the most active seismic zones in Europe and it is well-known for its strong intermediate depth earthquakes. Seismic tomography had revealed a high-velocity body beneath Vrancea and the Moesian platform that extends to a dep ...
Invitation and - FSU GK-12 Contact Information
... No—the oceanic crust is much thinner than the continental crust. The crust is many km thick but is thin relative to the rest of the planet. The crust is like the skin on an apple. 7. What is beneath the crust? Mantle (draw diagram w/ inner and outer core) 8. Do you think the crust has always been th ...
... No—the oceanic crust is much thinner than the continental crust. The crust is many km thick but is thin relative to the rest of the planet. The crust is like the skin on an apple. 7. What is beneath the crust? Mantle (draw diagram w/ inner and outer core) 8. Do you think the crust has always been th ...
Quantifying sea surface temperature ranges of the Arabian Sea for
... δ 18 O – salinity relationship in the northern Indian Ocean. Using atmospheric fluxes corresponding to Last Glacial Maximum (LGM) conditions in a multibox model, the authors conclude that there was no important change within the δ 18 O – salinity relationship during this period compared to the prese ...
... δ 18 O – salinity relationship in the northern Indian Ocean. Using atmospheric fluxes corresponding to Last Glacial Maximum (LGM) conditions in a multibox model, the authors conclude that there was no important change within the δ 18 O – salinity relationship during this period compared to the prese ...
Word file - FSU GK-12 Contact Information
... the oceanic crust is much thinner than the continental crust. The crust is many km thick but is thin relative to the rest of the planet. The crust is like the skin on an apple. 7. What is beneath the crust? Mantle (draw diagram w/ inner and outer core) 8. Do you think the crust has always been the w ...
... the oceanic crust is much thinner than the continental crust. The crust is many km thick but is thin relative to the rest of the planet. The crust is like the skin on an apple. 7. What is beneath the crust? Mantle (draw diagram w/ inner and outer core) 8. Do you think the crust has always been the w ...
The thermal structure of subduction zones constrained by seismic
... water could have an important secondary effect [16, 17]. Seismic attenuation is relatively unaffected by composition. Hence, to first order, regions of low Q should correspond to high temperatures. The overlying mantle wedge shows a high Q, indicating low temperatures, where the slab is less than 80 ...
... water could have an important secondary effect [16, 17]. Seismic attenuation is relatively unaffected by composition. Hence, to first order, regions of low Q should correspond to high temperatures. The overlying mantle wedge shows a high Q, indicating low temperatures, where the slab is less than 80 ...
Comparison of Argo and Aquarius sea surface salinity probability
... across metric distributions. In addition to traditional comparisons between mean or median values, the 1%, 10%, 25%, 50%, 75%, 90% and 99% quantiles of the statistical distributions are compared. The datasets compare well at the median, which is to be expected as the Aquarius retrieval algorithm is ...
... across metric distributions. In addition to traditional comparisons between mean or median values, the 1%, 10%, 25%, 50%, 75%, 90% and 99% quantiles of the statistical distributions are compared. The datasets compare well at the median, which is to be expected as the Aquarius retrieval algorithm is ...
DRAGONESS_D1.2
... observation well position of Xiaomaidao is relatively fixed, for many years the vicissitude has not been big. The meteorological observation field is located at the middle of Xiaomaidao in the commanding point, altitude above sea level 29.8m.There’s no big building and the woods influence around the ...
... observation well position of Xiaomaidao is relatively fixed, for many years the vicissitude has not been big. The meteorological observation field is located at the middle of Xiaomaidao in the commanding point, altitude above sea level 29.8m.There’s no big building and the woods influence around the ...
Short Bibliography on current European Marine Biotechnology
... The PharmaSea project focuses on obstacles in marine biodiscovery research, development and commercialization and brings together a broad interdisciplinary team of academic and industry researchers and specialists to address and overcome these. The partners are ideally placed to demonstrate how to w ...
... The PharmaSea project focuses on obstacles in marine biodiscovery research, development and commercialization and brings together a broad interdisciplinary team of academic and industry researchers and specialists to address and overcome these. The partners are ideally placed to demonstrate how to w ...
Coral Bleaching, an Imminent Threat to Marine Biodiversity
... water temperature exceeds seasonal mean maximum temperature over a short period of time which varies according to observed sites. However, for thirty years, the ocean mean temperature has been steadily ...
... water temperature exceeds seasonal mean maximum temperature over a short period of time which varies according to observed sites. However, for thirty years, the ocean mean temperature has been steadily ...
Percolating Through Volcanic Subsurface Rocks, Seawater is
... reactions is recorded in the miner➤ als and chemical composition of the rocks. By investigating samples of rocks that have been altered, we can learn about the sequence of water-rock interactions taking place in the subsurface. We can then begin to understand the processes responsible for the chemic ...
... reactions is recorded in the miner➤ als and chemical composition of the rocks. By investigating samples of rocks that have been altered, we can learn about the sequence of water-rock interactions taking place in the subsurface. We can then begin to understand the processes responsible for the chemic ...
here - EuroGOOS
... 4. Cooperation EuroGOOS should further enhance cooperation between key institutions that develop Operational Oceanography at Global, European and Regional Scales The development of Operational Oceanography involves major investments in infrastructures, including observing systems and high performan ...
... 4. Cooperation EuroGOOS should further enhance cooperation between key institutions that develop Operational Oceanography at Global, European and Regional Scales The development of Operational Oceanography involves major investments in infrastructures, including observing systems and high performan ...
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.