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Answers to: Ocean Clean Up Coming Now
Answers to: Ocean Clean Up Coming Now

... there's more than one of these patches. At least one more lies in the Pacific, and they dot the entire globe. Most often, "Great Pacific Garbage Patch" refers to the one extending from Hawaii to San Francisco. That patch of trash is supposed to be the biggest, sporting an impressive 3.5 million tons ...
chapter 3 - McGraw Hill Higher Education
chapter 3 - McGraw Hill Higher Education

... The thickness of pelagic sediment increases with increasing distance from mid-ocean ridges (fig. 3.16). ...
Water-mass transformation by sea ice in the
Water-mass transformation by sea ice in the

... a proxy for polar climate change27 . It has also been hypothesized that expanded Antarctic sea ice during the last glacial period was accompanied by a more vigorous AABW overturning circulation28,29 . From the ocean’s perspective, however, it is sea-ice freshwater transport, rather than extent, that ...
Seamounts Project
Seamounts Project

... fauna to date indicates that many species grow and reproduce slowly and are therefore much more vulnerable to overexploitation. Evidence has shown that deep-sea bottom fisheries can cause depletion of commercially-important fish stocks in just a few years and irreparable damage to slow-growing deep- ...
Reducing ocean model imbalances in the equatorial region caused
Reducing ocean model imbalances in the equatorial region caused

... • The bias pressure correction aims to reduce the impact of slowly varying biases, we want to provide a scheme which can balance the ocean increments and reduce initialisation shock. • The Incremental pressure correction (IPC) scheme is based on the bias pressure correction, but aims to reduce imbal ...
White Paper on National Environmental Management of the Ocean
White Paper on National Environmental Management of the Ocean

... Prince Edward and Marion Islands ("Prince Edward Islands") in the sub-Antarctic Indian Ocean. Generally most documents reference South Africa's mainland coastline as being approximately 3 000 km. This coastline stretches from the Namibian border on the West Coast to the Mozambique border on the East ...
Amundsen - The Journal of Ocean Technology
Amundsen - The Journal of Ocean Technology

... Lakes. The Amundsen is part of a fleet of icebreakers that maintain a continuous flow of ice in the St. Lawrence Seaway during winter, preventing the formation of ice jams and the excessive accumulation of ice in flood prone regions. The critical work of the Canadian Coast Guard icebreaking fleet en ...
1 2 Fifteen years of ocean observations with the global Argo array 3
1 2 Fifteen years of ocean observations with the global Argo array 3

... More detailed, regional views of the effects of changing near-surface temperature and salinity, from the central ...
Double-Diffusive Convection and Interleaving in the Arctic Ocean
Double-Diffusive Convection and Interleaving in the Arctic Ocean

... alternating maxima and minima in the vertical indicate interleaving between two different water masses, one warm and saline, the other cool and fresh. Between the layers, and the two water masses, alternating diffusive and saltfinger interfaces are formed. A warm intrusion has a saltfinger interface ...
[Subramaniam et al. 2008]
[Subramaniam et al. 2008]

... (19%) denoted the mesohaline DDA population, Axis 3 (13%) represented Trichodesmium population, and Axis 4 (7%) correlated with total integrated primary production and dFe. The key result was that the largest nonconservative changes in DIC were associated with high Richelia abundance and high N2 fi ...
Reconstructing geographical boundary conditions for palaeoclimate
Reconstructing geographical boundary conditions for palaeoclimate

... causes large discrepancies between model simulations because different studies use reconstructions of varying age and approach. A simple but striking example is given by Gasson et al. (2014), who used the output of several coupled global atmosphere-ocean models to force an ice sheet model simulating ...
1 Mapping in the Arctic Ocean in Support of a Potential Extended
1 Mapping in the Arctic Ocean in Support of a Potential Extended

... steaming north to pick up mapping of the region thought to represent the foot of the slope in the vicinity of 82° N and 162° W. Surveying continued east to follow the morphologic expression of the base of the slope until approximately 150° W where the character of the base of the slope changed and t ...
Applications of ocean transport modelling  Hanna Corell
Applications of ocean transport modelling Hanna Corell

... frequently denoted the thermohaline circulation, with “thermo” and “haline” referring to the temperature and salinity in the ocean determining the density. This circulation and its pathways play an important role for the climate and a simple model describing the interbasin exchanges was introduced b ...
Fifteen years of ocean observations with the global Argo array
Fifteen years of ocean observations with the global Argo array

... presently operating over the world-ocean. A defining aspect of Argo is that all data are reported in near real- ...
1. STATIONARY AND ERGODIC RANDOM PROCESSES 13.42 Design Principles for Ocean Vehicles
1. STATIONARY AND ERGODIC RANDOM PROCESSES 13.42 Design Principles for Ocean Vehicles

... that the time statistics are equivalent to the event statistics, we can also show that if y ( t ) is a realization of the random process y (t , ζ ) (which is stationary and ergodic) then ergodicity says that hi and Ti will provide the statistics on y (t , ζ ) and vice versa. ...
Marine Primary Productivity: Measurements and Variability
Marine Primary Productivity: Measurements and Variability

... the next satellite image). The fertilizing effect of the inflow of the nutrient-rich water during the flood season once resulted in exceptionally dense blooms of phytoplankton off the Nile Delta. This "Nile bloom" provided sustenance to sardines and other pelagic fishes. It also constituted a large ...
15.2 The Diversity of Ocean Life
15.2 The Diversity of Ocean Life

... areas are the only locations where large marine algae, often called seaweeds, are found attached to the bottom. These are the only areas of the seafloor that receive enough sunlight for the algae to survive. Throughout most of the deeper parts of the seafloor, animals live in perpetual darkness, where ...
15.2 The Diversity of Ocean Life
15.2 The Diversity of Ocean Life

... that feeds preferentially on pinnipeds (seals and sea lions) and has attacked humans swimming or surfing in pinniped habitat areas. A great white can grow to 7 m long and weigh up to 2250 kg. Sharks are classified as nekton. ...
Press Release - English ()
Press Release - English ()

... The state-of-the-art Japanese drilling vessel Chikyu will travel to the central Nankai Trough, ~120 kilometers off the coast of Japan where the ocean is 4.7 kilometers deep, and drill a further 1.2 kilometers beneath the ocean’s floor to collect sediment and rock cores. The total distance from the ...
Seabed Disposal
Seabed Disposal

... wastes in the seabed were carried out for over a decade by a host of scientists from around the world. In 1976, the Organization for Economic Cooperation and Development (OECD) and the Nuclear Energy Agency coordinated research at the international level and formed the Seabed Working Group. Members ...
Dohan, K., and N. Maximenko, 2010: Monitoring ocean currents with
Dohan, K., and N. Maximenko, 2010: Monitoring ocean currents with

... scales, including basin-wide gyres, fast narrow boundary currents, eddies, and turbulence. To understand the full system requires measuring a range of motions, from thousands of kilometers to less than a meter, and time scales from those that are climate related (decades) to daily processes. Present ...
chlorophyll concentration estimated from irradiance measurements
chlorophyll concentration estimated from irradiance measurements

... measurements made at fluctuating depths, it would be necessary to determine the depthdependence of α ij ( z ) and β ij ( z ) . The depth-dependence of these parameters results from the depth variations of rij ( z ) in homogeneous waters, which in turn result from spectral attenuation and scattering ...
Census of seafloor sediments in the world`s ocean
Census of seafloor sediments in the world`s ocean

... at the sea surface. We present the first digital map of seafloor lithologies based on descriptions of nearly 14,500 samples from original cruise reports, interpolated using a support vector machine algorithm. We show that sediment distribution is more complex, with significant deviations from earlie ...
the response of echinoderms to ocean acidification
the response of echinoderms to ocean acidification

... waters.” To explore this situation further, Ericson et al. “investigated the effects of present-day pH 8.0, predicted ocean surface pH for the years 2100 and 2300 (pH 7.7 and pH 7.3, respectively) and an extreme pH (pH 7.0) on fertilization and embryogenesis in the Antarctic nemertean worm Parborla ...
What are Phytoplankton?
What are Phytoplankton?

... Hundreds of thousands of species of phytoplankton live in Earth's oceans, each adapted to particular water conditions. Changes in water clarity, nutrient content, and salinity change the species that live in a given place. Because larger plankton require more nutrients, they have a greater need for ...
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Indian Ocean



The Indian Ocean is the third largest of the world's oceanic divisions, covering approximately 20% of the water on the Earth's surface. It is bounded by Asia on the north, on the west by Africa, on the east by Australia, and on the south by the Southern Ocean or, depending on definition, by Antarctica. It is named after India.The Indian Ocean is known as Ratnakara, ""the mine of gems"", in ancient Sanskrit literature and as Hind Mahasagar in Hindi and other Indian languages.
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