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Coupling between Wind-Driven Currents and Midlatitude Storm Tracks
Coupling between Wind-Driven Currents and Midlatitude Storm Tracks

... and Hurrell 1994), the dominant mechanism for the coupling has not been determined. One of the obstacles in analyzing this process, besides the obvious inadequacy of the observational database on decadal timescales, is that different atmospheric general circulation models (AGCM) respond very differe ...
Plate Tectonics The unifying concept of the Earth sciences. Plate
Plate Tectonics The unifying concept of the Earth sciences. Plate

... Plate Tectonics The unifying concept of the Earth sciences. • The outer portion of the Earth is made up of about 20 distinct “plates” (~ 100 km thick), which move relative to each other • This motion is what causes earthquakes and makes mountain ranges ...
The deep sea is a major sink for microplastic debris
The deep sea is a major sink for microplastic debris

... of plastic debris in the natural environment. Debris is now present on shorelines and at the sea surface from pole to pole [1,2]. It has major environmental impacts and is recognized as one of the key challenges of our century [1–3]. However, despite extensive environmental monitoring, there is litt ...
The Wonders of the Ocean Floor
The Wonders of the Ocean Floor

... http://upload.wikimedia.org/wikipedia/commons/1/10/Submersible_named_Star_III_in_front_of_Scripps_Institution_of_Oceanography.JPG ...
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Evidence

... surface  and  provides  a  coherent  account  of  its  geological  history.  This  theory  is  supported  by  mul(ple  evidence   streams—for  example,  the  consistent  paNerns  of  earthquake  loca(ons,  evidence  of  ocean  floor  spreading ...
Climate change and Southern Ocean ecosystems I
Climate change and Southern Ocean ecosystems I

... island. Some circumpolar syntheses of the ecology of particular habitat types and the consequences of change are also available (e.g. sea-ice habitats – Massom & Stammerjohn, 2010; general – Turner et al., 2009a). In addition, a comprehensive assessment of the biogeography of ASO biota is currently ...
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... and stood motionless, rooted to the spot. I gradually realized that the noise I had heard in the forest belonged to the roar of the sea and the breaking waves. The horizon blended with the sky, clouds, and ocean. Wondering what lay beyond it, my heart raced; I felt breathless. In 2011, almost 60 yea ...
Chapter I - Shodhganga
Chapter I - Shodhganga

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Hotspot Ecosystem Research on Europe`s Deep-Ocean
Hotspot Ecosystem Research on Europe`s Deep-Ocean

... quired must be generated in an integrated way that ties research on biodiversity and biological processes intimately to the physical factors that control ecosystems (geology, sedimentology, physical oceanography, biogeochemistry). In addition, it is important to set present-day ecosystems in an hist ...
Antarctic Stratification, Atmospheric Water Vapor, and Heinrich Events
Antarctic Stratification, Atmospheric Water Vapor, and Heinrich Events

... rate of North Atlantic ventilation is indeed lower in the cold climate simulations [de Boer et al., in review], as one might expect [Toggweiler and Samuels, 1995]. However, in the EOS cold climate simulations, North Atlantic overturning is slightly greater than in the control simulation (Figure 1a). ...
Limitation of egg production in Calanus finmarchicus in the field: A
Limitation of egg production in Calanus finmarchicus in the field: A

... the biological pump, by consuming and remineralizing sinking particles, repackaging them into fecal pellets, and by fragmenting them into slower- or non-sinking particles. We characterized the mesopelagic zooplankton community and sinking particle flux at the Hawaii Ocean Time series (HOT) station A ...
The tilt of mean sea level along the east coast of North America
The tilt of mean sea level along the east coast of North America

... Applying the gap statistic to the ocean estimates showed there to be only one cluster. However, there is spatially structured variability within the cluster. From a principal component analysis based on the covariance matrix, we found the first spatial mode (Figure 2b). This mode accounts for 84% of ...
GEOTRACES National Reports - Scientific Committee on Oceanic
GEOTRACES National Reports - Scientific Committee on Oceanic

... in the Australian sector of the Southern Hemisphere has shown that variance in the observed fractional iron solubility is due to a combination of different soluble iron sources including mineral dust and biomass burning emissions. The research investigated differences in atmospheric iron solubility ...
On the depth of oceanic earthquakes - Archimer
On the depth of oceanic earthquakes - Archimer

... fact that radiogenic heating in continental shields is not as concentrated at shallow depths as previously believed, they show that most earthquakes in continental regions are confined to crustal regions cooler than 600°C. The temperature dependence of the mantle thermal conductivity results in deep ...
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Ocean acidification



Ocean acidification is the ongoing decrease in the pH of the Earth's oceans, caused by the uptake of carbon dioxide (CO2) from the atmosphere. An estimated 30–40% of the carbon dioxide from human activity released into the atmosphere dissolves into oceans, rivers and lakes. To achieve chemical equilibrium, some of it reacts with the water to form carbonic acid. Some of these extra carbonic acid molecules react with a water molecule to give a bicarbonate ion and a hydronium ion, thus increasing ocean acidity (H+ ion concentration). Between 1751 and 1994 surface ocean pH is estimated to have decreased from approximately 8.25 to 8.14, representing an increase of almost 30% in H+ ion concentration in the world's oceans. Since current and projected ocean pH levels are above 7.0, the oceans are technically alkaline now and will remain so; referring to this effect as ""decreasing ocean alkalinity"" would be equally correct if less politically useful. Earth System Models project that within the last decade ocean acidity exceeded historical analogs and in combination with other ocean biogeochemical changes could undermine the functioning of marine ecosystems and disrupt the provision of many goods and services associated with the ocean.Increasing acidity is thought to have a range of possibly harmful consequences, such as depressing metabolic rates and immune responses in some organisms, and causing coral bleaching. This also causes decreasing oxygen levels as it kills off algae.Other chemical reactions are triggered which result in a net decrease in the amount of carbonate ions available. This makes it more difficult for marine calcifying organisms, such as coral and some plankton, to form biogenic calcium carbonate, and such structures become vulnerable to dissolution. Ongoing acidification of the oceans threatens food chains connected with the oceans. As members of the InterAcademy Panel, 105 science academies have issued a statement on ocean acidification recommending that by 2050, global CO2 emissions be reduced by at least 50% compared to the 1990 level.Ocean acidification has been called the ""evil twin of global warming"" and ""the other CO2 problem"".Ocean acidification has occurred previously in Earth's history. The most notable example is the Paleocene-Eocene Thermal Maximum (PETM), which occurred approximately 56 million years ago. For reasons that are currently uncertain, massive amounts of carbon entered the ocean and atmosphere, and led to the dissolution of carbonate sediments in all ocean basins.
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