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... 8. Where and when do seed populations come from? - What defines the variability of the annual spring bloom system of the North Atlantic and the Arctic? Is it chaotic, spatially variable, how does it get seeded, do the seed population matter, and how does the timing vary and why? What are the effects ...
PDF: Printable Press Release
PDF: Printable Press Release

What are Phytoplankton?
What are Phytoplankton?

... SPECIES AND THEIR FECES ...
Quantifying the contribution to atmospheric iodine from
Quantifying the contribution to atmospheric iodine from

... parameterizations using novel conservative and volatile tracers, Global Biogeochem. ...
Slide 1
Slide 1

Word Doc
Word Doc

... Color the plot by a third variable, so you can: ○ Make a map of salinity or oxygen ○ Make a salinity vs. temperature diagram showing which water is low oxygen ○ Make a profile of fluorescence over time or longitude ● Limit the selected data by an additional constraint, so you can: ○ Make a map of ne ...
Microbial Food Webs - Cornell Geological Sciences
Microbial Food Webs - Cornell Geological Sciences

... with it - this forms an efficient biological carbon pump. The opposite is true when the dominant phytoplankton is small and the biological pump is more inefficient. ...
Estimation of the Barrier Layer Thickness in the Indian Ocean using
Estimation of the Barrier Layer Thickness in the Indian Ocean using

Empirical relationship for marine primary production : the
Empirical relationship for marine primary production : the

... different studies. Chlorophyll a alone is of little value (r 2 =0.42) in predicting daily production integrated over the euphotic zone among different areas. The depth of the mixed layer, surface temperature, water extinction coefficient and the mean light level within the mixed layer significantly ...
chlorophyll concentration estimated from irradiance measurements
chlorophyll concentration estimated from irradiance measurements

Exam in BI3061 Biological Oceanography
Exam in BI3061 Biological Oceanography

... E. Colour of the sea surface is strongly affected by the sky and its clouds 14. Light: What statement is NOT true? A. Light is electromagnetic radiation B. Light has two modes: Either it is a stream of particles or a train of waves C. An experiment cannot reveal both modes perfectly at the same time ...
Document
Document

... 1)Why does diurnal vertical migration occur? 2) Do plankton have high or low Reynolds numbers? Explain what a Reynolds number is. 3) How does plankton’s Reynolds number influence feeding in copepods? 4) Define the term drag in marine hydrodynamics. What adaptations do plankton have to decrease drag? ...
PPT
PPT

... and the large fecal material easily sinks to the deep ocean taking organic carbon with it - this forms an efficient biological carbon pump. The opposite is true when the dominant phytoplankton is small and the biological pump is more inefficient. ...
Multiple-Choice Questions - Raleigh Charter High School
Multiple-Choice Questions - Raleigh Charter High School

... z. tropical rain forest Most sea life is found in which area? w. On or above continental shelves x. In trenches y. Along mid-ocean ridges z. Near deep-sea hydrothermal vents Coastal upwelling results in ________. w. carbon dioxide-rich water surfacing x. warm water surfacing y. mixing of salt and fr ...
Summary and Conclusion
Summary and Conclusion

validation of satellite derived primary production models in
validation of satellite derived primary production models in

... primary production of phytoplankton (PP) from remote sensing data, a choice of the most realistic one for a particular ocean region remains a non-trivial issue. In this work, we estimate PP in the Northeast Atlantic Ocean (200 - 510 N and 100 – 400 W) from 1998 to 2005 using three frequently used mo ...
File
File

... kilometers) east of the Mariana Islands, the Mariana Trench is a crescent-shaped scar in the Earth’s crust that measures more than 1,500 miles (2,550 kilometers) long and 43 miles (69 kilometers) wide on average. The distance between the surface of the ocean and the trench’s deepest point—the Challe ...
Lecture 7. Marine Sediments
Lecture 7. Marine Sediments

Reviewing Key Skills Chapter 4 Ecosystems and Communities
Reviewing Key Skills Chapter 4 Ecosystems and Communities

Indian Ocean heating affects micro plants and fish on the
Indian Ocean heating affects micro plants and fish on the

... warming during the past century is up to 1.2 degrees Celsius, which is very large as compared to a global surface warming of up to 0.8 degrees Celsius during the same period. Rising ocean surface temperature results in less dense water on the surface and dense water in the subsurface. Such a conditi ...
Ch 15 - FCUSD.org
Ch 15 - FCUSD.org

...  Temperatures are just a few degrees above freezing  Constant high-density water ...
Atlantic Ocean Floor Topography Lab.
Atlantic Ocean Floor Topography Lab.

... Use a large nautical chart for another interesting area of the ocean. With the help of a ruler or large straightedge read and record the depth of the ocean and heights of islands or land masses at regular intervals, (such as every 2 miles or some other appropriate distance). Make another line graph ...
PPT
PPT

OCEANS
OCEANS

... picture? 22. Such blooms are common in the spring and summer, when ____ brings minerals & nutrients from deeper waters to the surface. ...
Ecology of polar oceans
Ecology of polar oceans

... • disturbance by scouring ice • sublittoral benthos can only develop fully in polar regions out of reach of scouring sea ice, around 10 m below low tide level • below these depths an extreme example of severe habitat transformation is caused by icebergs • without significant mechanical distubŕbance ...
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Critical Depth

In biological oceanography, 'Critical Depth' is defined as a hypothesized surface mixing depth at which phytoplankton growth is precisely matched by losses of phytoplankton biomass within this depth interval.
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