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6H2O + 6CO2 + energy + nutrients = C6H12O6 + 6O2 Focus on left
6H2O + 6CO2 + energy + nutrients = C6H12O6 + 6O2 Focus on left

... surface waters during photosynthesis  Essential to the growth of phytoplankton  If these biolimiting nutrients increase in sea water, life increases  If these biolimiting nutrients decrease in sea water, life decreases  Where would you expect to find the highest biomass in the Pacific?? ...
(LOW) variability
(LOW) variability

... modes and the South Atlantic response to El Niño-Southern Oscillation induced climate variability. 2. A regional ocean model is used to investigate variability in the south east Atlantic, especially in the Angola Benguela Frontal Zone. Results: 1. A Rotated Empirical Orthogonal Function analysis of ...
L. Ciasto`s presentation notes: overview  - geo.uni
L. Ciasto`s presentation notes: overview - geo.uni

... Vertical Profile of Ocean Mixed(Surface) Layer: warm low-density water Responds to annual cycle of insolation: thinnest in summer and thickest in winter ...
Primary Production
Primary Production

... Euphotic Zone Light OK ...
1 - Raleigh Charter High School
1 - Raleigh Charter High School

... z. Iceberg 22. What is the difference between a castle berg and a tabular berg? w. Castle = tall & thin, tabular = large & flat x. Castle = large & flat, tabular = tall & thin y. Castle = tall & flat, tabular = large & thin z. Castle = large & thin, tabular = tall & flat 23. What is the average pH o ...
Arnaud_lecture8
Arnaud_lecture8

Algae and Climate Change
Algae and Climate Change

... • Vertical mixing is a key variable because stratification affects light and nutrient availability for growth. Smaller, buoyant species have an advantage under reduced mixing. • Warming increases consumption by herbivores more strongly than primary production which strengthens top down control (Somm ...
henrichs-sinking particles
henrichs-sinking particles

... traps to monitor the role of plankton and other particles in changes occurring in the oceanography of the Bering Sea. ...
pices xv - North Pacific Marine Science Organization
pices xv - North Pacific Marine Science Organization

... Coagulation is an important process accelerating the sinking of particles and creating microhabitats. Its rate increases with particle concentration. Spring blooms and iron fertilization experiments provide useful situations to test the predictions of simple coagulation models. The predicted propert ...
Topo. Tubs
Topo. Tubs

convection in the atmosphere and oceans
convection in the atmosphere and oceans

Biogeochemical Cycles
Biogeochemical Cycles

... Nitrogen and Phosphorous is Limiting • In areas with sufficient rainfall, H2O, CO2, and O2 are in plentiful supply. • Thus, the primary limiting factors for plant growth are the availability of N and P in the soil. • But, sometimes it can be too much… ...
Image: Marine biologists use plankton nets to sample phytoplankton
Image: Marine biologists use plankton nets to sample phytoplankton

turbulence @ ocean observatories - Center for Coastal Physical
turbulence @ ocean observatories - Center for Coastal Physical

field surveys - essie-uf
field surveys - essie-uf

... Field surveys will be conducted at instrument development and testing phases to compare data obtained from different sources (PIV and microstructure profilers). St. Augustine Inlet (Florida) and the Penobscot River (Maine) have been selected as the field sites because of their energetic currents (>1 ...
Full-text PDF - Association for the Sciences of Limnology
Full-text PDF - Association for the Sciences of Limnology

... in the bay and not in the open gulf outside of it. These records suggest a preference for coastal water over oceanic water if brackish water can be avoided. Unfortunately, we have, no information on the salinity at Tongatabu during the bloom. Harmful effects associated with blooms vary from negligib ...
nakamoto4
nakamoto4

General objective
General objective

... in the C02 biological pump and biogas production, focusing on their responses to change in forcing parameters: iron supply, statrification, light (visible and UV), ...
274 - CIESM
274 - CIESM

... regular sinking mechanisms. In our study, Chl a signal was detected up to 400 m depth (Fig. 1B), indicating recent subduction of the surface water. The measured PAR depths ranged from 66.5 to 74.5 m therefore the convective event brought phytoplankton cells down to the aphotic zone. The phytoplankto ...
What is the difference between primary production and primary
What is the difference between primary production and primary

... What three factors affect the density of seawater and why is it important to determine density when study marine systems?  What causes the ocean to be divided vertically into 3 zones (surface mixed layer, pycnocline, and deep zone)?  What factors are measured to determine horizontal pressure gradi ...
The role of phytoplankton in the carbon cycle
The role of phytoplankton in the carbon cycle

... in the ocean. If so, these taxonomic shifts, and their associated impact on net air–sea CO2 exchange, would be linked mechanistically to the seasonal dynamics of the upper mixed layer, interannual variations in climatic forcing, contemporaneous trends in anthropogenic climate warming, and historical ...
IMPACTS OF CLIMATE CHANGE ON HARMFUL ALGAL BLOOMS
IMPACTS OF CLIMATE CHANGE ON HARMFUL ALGAL BLOOMS

... There are three contrasting views on the factors contributing to an apparent global increase in HABs; 1. they are caused by increased anthropogenic input of nutrients into the sea (eutrophication); 2. the increase may be an artefact due to increased interest and reporting; and 3. any increase is rel ...
Lab/Fieldwork Activity Example
Lab/Fieldwork Activity Example

... The availability of light controls plant growth and phytoplankton distributions in the ocean. Light is absorbed as it passes through water. The clearest open-ocean water is most transparent (absorbs the least amount of light) in the blue-green range of colors. As concentrations of particules and di ...
Marine Productivity and Nutrient Cycling Base of the food chain
Marine Productivity and Nutrient Cycling Base of the food chain

Earth Layers
Earth Layers

... ...
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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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