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Guyot Science 2005
Guyot Science 2005

... Satish Myneni was promoted to the rank of associate professor with continuing tenure. Two professors were named to endowed chairs: George Philander is now the Knox Taylor Professor of Geosciences and Bess Ward is now the William J. Sinclair Professor of Geosciences. In April, George was inducted int ...
Feely et al. - Western Washington University
Feely et al. - Western Washington University

... a depth as 50 m in the southern part of the Hood Canal Basin. Within Puget Sound, only the deepest sample from the southernmost station in Hood Canal was hypoxic (57 mmol kg1 ¼ 1.9 mg L1), and surface (<2 m depth) nitrate concentrations in this area were between 0.07 and 1.36 mmol kg1, indicating ...
Teacher Resources - Fish Eye Project
Teacher Resources - Fish Eye Project

... To  ‘see’,  they  have  developed  other  methods.  For  example,  some  vent  shrimp  have  sensory   organs  on  their  back  that  can  help  them  detect  the  faint  glow/heat  signature  that  vents  give  off.   If  there  is ...
Simulations of the mid-Pliocene Warm Period using two versions of
Simulations of the mid-Pliocene Warm Period using two versions of

... that narrow ocean passages that existed in the Pliocene remained open. Note that in ModelE2-R, a straits parameterisation is used to maintain ocean flow through grid cell locations where straits cannot be resolved at the 1◦ × 1.25◦ resolution of the land/sea mask in the ocean component of the model. ...
Waves that appear from nowhere and disappear without a trace
Waves that appear from nowhere and disappear without a trace

... much higher than that of the first order rational solution, Eq. (5). On the line x = 0, we now have |ψ| = 0 at 4 points, viz. t = ±0.465 and t = ±1.757. Comparing the solution in Fig. 4 with the one in Fig. 3, we can say that the latter is more likely to break up a ship than the former one. Are there ...
Ocean storage
Ocean storage

... and ecological impact of CO2 released into seawater, generally as liquid drop­ lets, larger liquid masses, or liquid–hydrate–water composites. In situ experiments conducted at the Monterey Bay Aquarium Research Institute (MBARI; see Key References), typically involving the release and observation of ...
Water-Mass Transformations in a Neutral Density Framework and
Water-Mass Transformations in a Neutral Density Framework and

... been considered in previous analyses (e.g., Large and Nurser 2001); the implicit assumption previously has been that the heating occurs only within the mixed layer. This is not generally the case (Fig. 2; see also Ohlmann et al. 1996) and, especially at midlatitudes in summer or in the equatorial an ...
Integrated Ocean Observing System
Integrated Ocean Observing System

... linked components (a system of systems), a global ocean component and a coastal component. The global component is part of an international collaboration that will improve nowcasts and forecasts of weather, surface waves and currents, sea surface temperature and global climate trends. It will also p ...
Progress in satellite remote sensing for studying physical
Progress in satellite remote sensing for studying physical

... of the (often more subtler) colour changes within the surface ocean. These “ocean colour” sensors thus operate at a number of narrow spectral bands, each of which covers specific wavelength regions of the visible spectrum (for example 8 spectral bands for the Sea Viewing Wide Field of View Sensor, S ...
Week 9a
Week 9a

... molluscs, corals, echinoderms, foraminifera and calcareous algae. Although it is not always clear what function this calcification has, it seems integral to their biology; so any decrease in calcification, as a result of increased CO2, is therefore likely to have significant consequences such as the ...
1 Lecture 12 - What Controls the Composition of River Water and
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... VrCr = Vhydro (Csw - Cexit fluid) for Mg2+, Cexit fluid = 0 thus: Csw = ( Vr / Vhydro ) Cr = 300 Cr The dominant control is the hydrothermal circulation rate (Vhydro), which is driven by tectonic activity. We can do the calculation backwards by assuming that the composition of seawater and river wat ...
Using dissolved oxygen concentrations to determine mixed layer
Using dissolved oxygen concentrations to determine mixed layer

... gas exchange (Fairall et al., 2000). Mixed layer depths could also be different, depending on whether they refer to temperature or to gases. Moreover, different gases respond at different rates to wind forcing, depending on their solubility, with less soluble gases (e.g., N2 , Ar or O2 ) responding ...
- GODAC Data Site -NUUNKUI
- GODAC Data Site -NUUNKUI

... sought a 6,500m France ...
1 Central Arctic Ocean paleoceanography from ~50 ka to present, 1
1 Central Arctic Ocean paleoceanography from ~50 ka to present, 1

... Manuscript under review for journal Clim. Past Discussion started: 28 March 2017 c Author(s) 2017. CC-BY 3.0 License. ...
conference handbook
conference handbook

... Due to its geographical position between Africa, Europe, and Asia Minor and due to its mild climate, Crete became a centre of culture as early as Neolithic times. The first prehistoric settlements appeared in Crete around 6000 BC while in 2600 BC settlers who knew how to craft bronze arrived in Cret ...
Alfred Wegener and Harry Hess
Alfred Wegener and Harry Hess

... a fingernail grows. In a human lifetime, this amounts to about two meters (just over six feet). Millions of years in the future, parts of California and Mexico will probably drift off. They’ll separate from North America and become an island. Most of Africa is pushing toward Europe. Eventually, it w ...
pdf version - Woods Hole Oceanographic Institution
pdf version - Woods Hole Oceanographic Institution

... world ocean. Perhaps nowhere on earth is climate change having as dramatic and rapid an effect as in the Arctic, where ice cover, ocean water circulation, geochemistry, and ecosystems are all responding to the pervasive rise in air and sea temperatures. These changing conditions will not only alter ...
Census of seafloor sediments in world`s ocean basins
Census of seafloor sediments in world`s ocean basins

... dominated by a large body of sand (Fig. 3). Sponge spicules form a significant component of seafloor sediment in parts of the Australian-Antarctic Basin where they co-occur with diatom and radiolarian oozes. Compared to earlier maps clay occupies a considerably larger area around eastern and western ...
Observing climate change trends in ocean biogeochemistry: when
Observing climate change trends in ocean biogeochemistry: when

... variables is shown in Fig. 1. The natural variability, here defined as the standard deviation of the residuals (see Materials and methods), is presented in Fig. S2. In many variables, n* is shorter at low than at high latitudes. This arises because at low latitudes trends are strong but variability ...
Uses and Abuses of the Ocean
Uses and Abuses of the Ocean

... The human population grew by 400% during the twentieth century. This growth, coupled with a 4.5-fold increase in economic activity per person, resulted in accelerating exploitation of Earth’s resources. By most calculations, we have used more natural resources since 1955 than in all of recorded huma ...
Chapter 7: Thermodynamics
Chapter 7: Thermodynamics

... The processes that determine the annual SST variability have been well studied (e.g., Wang B. and X. Fu, Journal of Climate, 2001; Swenson and Hansen, 1999, Journal of Physical Oceanography). 7.2 Sea surface salinity budget Except for the SST, the sea surface salinity (SSS) budget also plays an impo ...
Atmosphere-Ocean Coupling and Surface Circulation of the Ocean
Atmosphere-Ocean Coupling and Surface Circulation of the Ocean

... major surface currents of the world oceans aided by the observations of other scientists including Alexander von Humboldt. At approximately this same time, the importance of commercial whaling led the government of the United States to support an “exploring expedition.” This global voyage was led by ...
MODULE #1: The Oceans of Our Planet Introduction This course is
MODULE #1: The Oceans of Our Planet Introduction This course is

... 1.2 You have a sample of oceanic crust and a sample of continental crust. How could you tell which is which? Continental Drift and Plate Tectonics As early as the 1600s, scientists began looking at the shape of the continents and noticed that they seem to “match up” like puzzle pieces. This led many ...
Remote Sensing of the Diffuse Attenuation Coefficient and Related
Remote Sensing of the Diffuse Attenuation Coefficient and Related

... The main goal of the SeaWiFS ocean color mission was the assessment of the global climate change and its effects on the global carbon cycle (Hooker, Esaias et al. 1992). In this context, remote sensing of the marine chlorophyll concentration (CHL) and the diffuse attenuation of Photosynthetically Av ...
Downloaded
Downloaded

... similar magnitude (Sarmiento et al. 1995). One is the ‘solubility pump’ driven by ocean circulation and by the solubility of CO2 in seawater and the other is the ‘biological pump’ that is driven by the primary production of plant (phyto-) plankton and subsequent gravitational settling of carbon-rich ...
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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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