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Print this article - Latin American Journal of Aquatic Mammals
Print this article - Latin American Journal of Aquatic Mammals

... ABSTRACT: Historical data (1965-2000) of temperature, salinity, and dissolved oxygen (0 and 50m) were analyzed to understand the seasonal variability of the oceanographic conditions associated to the distribution of P. spinipinnis from Paita, Peru (05°01’S, 81ºW), in the Pacific Ocean, to Santa Cata ...
Lesson: Landforms and Oceans
Lesson: Landforms and Oceans

Simulating the mid-Pliocene climate with the MIROC general
Simulating the mid-Pliocene climate with the MIROC general

Age, spreading rates, and spreading asymmetry of the world`s ocean
Age, spreading rates, and spreading asymmetry of the world`s ocean

Forum Future Ocean Floor Mapping - Ismar-Cnr
Forum Future Ocean Floor Mapping - Ismar-Cnr

... the bathymetry, i.e. depth of the ocean floor, is today recognized to be of vital importance not only for navigation and coastal management but also a growing variety of inter-related uses. Bathymetry is a fundamental parameter for studies of deep water circulation, tides, tsunami forecasting, upwel ...
Reconstructing geographical boundary conditions for palaeoclimate
Reconstructing geographical boundary conditions for palaeoclimate

... 1/3 of the current ice thickness. The changes mainly affect Greenland and Antarctica, although for the time window chosen here a highly detailed palaeotopography of Antarctica was derived by Wilson et al. (2012), considering both isostatic rebound and sediment restoration with respect to the present ...
Ocean Challenge Vol. 6 No.1 1995
Ocean Challenge Vol. 6 No.1 1995

Moving in the Right Direction - Mid-Atlantic Regional Council on the
Moving in the Right Direction - Mid-Atlantic Regional Council on the

... coastal/description/2007projects/2-03-07.html), that identifies birds most at risk in the Mid-Atlantic region for which data were available. Of the 46 species for which data were available, six species were identified as being particularly vulnerable to population losses. Although far more data are ...
Chapter 4: Marine sediments
Chapter 4: Marine sediments

... Fecal pellets large enough to sink quickly (10-15 days) ...
What are Phytoplankton?
What are Phytoplankton?

... Productivity is expected to drop because as the surface waters warm, the water column becomes increasingly stratified; there is less vertical mixing to recycle nutrients from deep waters back to the surface. Over the past decade, scientists have begun looking for this trend in satellite observation ...
NGU Report 2006.067 Sediment composition and heavy
NGU Report 2006.067 Sediment composition and heavy

North Atlantic ecosystem sensitivity to Holocene shifts in Meridional
North Atlantic ecosystem sensitivity to Holocene shifts in Meridional

... surface/atmospheric processes and rates of deep water formation. Holocene climate changes, however, remain poorly documented due to a lack of high-resolution paleoclimate records, and their impacts on marine ecosystems remain unknown. We present a 4500 year absolute-dated sea surface radiocarbon rec ...
Using dissolved oxygen concentrations to determine mixed layer
Using dissolved oxygen concentrations to determine mixed layer

Marine Debris
Marine Debris

... The captain is seriously concerned about the debris, according to translation by Borodina. “The reason the huge commercial vessels travelling the North Pacific have not reported anything,” the captain said, “is because they cut through such stuff like through butter.” For the Pallada, however, alth ...
Conservation and Sustainable Use of Arctic Marine Biodiversity
Conservation and Sustainable Use of Arctic Marine Biodiversity

... Reports describe the loss of biodiversity as continuing.17 Virtually all ecosystems have been affected by human activities.18 Habitats and ecosystems have been affected, for example, by transformation to farmland and destruction of coral reefs. The rates of species extinction are 100 times higher th ...
Thermocline and Intermediate Water Communication Between the
Thermocline and Intermediate Water Communication Between the

... diminishes with increasing depth; it extends through the lower thermocline into the Antarctic Intermediate Water (AAIW) (about 50% is derived from the Indian Ocean) but not into the deep water. While much of the interocean exchange remains on an approximate horizontal "isopycnal" plane, as ...
Attachment 1
Attachment 1

... conceptual overview is below.  As each particle breaks into more and more particles, see an exponential increase in number of fragments. With this increase in fragments comes an exponential increase in TOTAL surface area. Note that the surface area of each piece shrinks, but the total combined surf ...
Student report - cloudfront.net
Student report - cloudfront.net

... boiling point of water especially due to the enormous pressure put on the water by the ocean or the rock around, making it about 400 degrees Celsius. The vents can be found at any depth, with the shallowest at 30 meters deep near coastlines, and 3600 meters for the deepest. Using GeoMapApp we looked ...
Impacts of 2009 Typhoons on Seawater Properties and Top Layer
Impacts of 2009 Typhoons on Seawater Properties and Top Layer

Achieving the Sustainable Development Goal for the Oceans
Achieving the Sustainable Development Goal for the Oceans

... grouped according to marine regions. This would not only facilitate assessments at the scale of ecosystems but also enhance cooperation through regional approaches. For instance, an assessment of commitments that identifies deficits with respect to a particular target in a region could highlight the ...
CHAPTER 1 - RECOGNIZING OCEAN ASSETS AND CHALLENGES
CHAPTER 1 - RECOGNIZING OCEAN ASSETS AND CHALLENGES

... Offshore Energy, Minerals, and Emerging Uses Valuable oil and mineral resources are found off our shores and in the seabed; they fuel our cars and our economy, provide materials for construction and shoreline protection, and offer exciting opportunities for the future. Currently, about 30 percent of ...
SANCOR Newsletter 210 - National Research Foundation
SANCOR Newsletter 210 - National Research Foundation

... Figure 2:  Multiple observed indicators of a changing global carbon cycle:   (a)  atmospheric  concentrations  of  carbon  dioxide  (CO2)  from  Mauna  Loa  (19° 32’N, 155°34’W – red) and South Pole (89°59’S, 24°48’W – black) since 1958;   (b)  partial pressure of dissolved CO2 at the ocean surface  ...
Southern Ocean and South Pacific Region, Working Group 1
Southern Ocean and South Pacific Region, Working Group 1

Renewable Energies from the Ocean.pdf
Renewable Energies from the Ocean.pdf

... During Hurricane Lili in 2002, the NDBC had two buoys, #42001 located near R, and #42003 located due east along 26 ◦ N, approximately 280 km from 42001. The wind speed measurement at both buoys was 10 m. From the NDBC website (www.ndbc.noaa.gov/), at 20Z 2 October 2002 at #42001, P0 = 956.1 mb. Subs ...
Alfred Wegener and Harry Hess
Alfred Wegener and Harry Hess

... directions and at different speeds. Their sizes don’t match the landmasses on top of them. For instance, the North American plate is much larger than the North American continent. The plate starts at the western coast of North America. Yet, it extends into the middle of the Atlantic Ocean. Iceland i ...
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Arctic Ocean



The Arctic Ocean (also known as the Northern Ocean), located in the Northern Hemisphere and mostly in the Arctic north polar region, is the smallest and shallowest of the world's five major oceanic divisions. The International Hydrographic Organization (IHO) recognizes it as an ocean, although some oceanographers call it the Arctic Mediterranean Sea or simply the Arctic Sea, classifying it a mediterranean sea or an estuary of the Atlantic Ocean. Alternatively, the Arctic Ocean can be seen as the northernmost part of the all-encompassing World Ocean.Almost completely surrounded by Eurasia and North America, the Arctic Ocean is partly covered by sea ice throughout the year (and almost completely in winter). The Arctic Ocean's surface temperature and salinity vary seasonally as the ice cover melts and freezes; its salinity is the lowest on average of the five major oceans, due to low evaporation, heavy fresh water inflow from rivers and streams, and limited connection and outflow to surrounding oceanic waters with higher salinities. The summer shrinking of the ice has been quoted at 50%. The US National Snow and Ice Data Center (NSIDC) uses satellite data to provide a daily record of Arctic sea ice cover and the rate of melting compared to an average period and specific past years.
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