The Role of Light Flashcards
Why does solar radiation vary with latitude and seasons
Sun Angle: Varies with latitude, time of year and time of day
Very high reflectance when sun angle is below 5 degrees
Length of day
Atmospheric Conditions
Scattered Light
Light reflects or bounces off particles/molecules so we can see them
Absorbed Light
Absorption by molecules of water to heat (Infrared)
What is the impact of absorbed and scattered light
Absorbed light used for photosynthesis
Scattering and absorption effects the quantity/quality of light available
Solar Energy Percentages Ocean
50% absorbed, reflected and scattered in the atmosphere
50% absorbed/scattered in the first ~10m – UV scattered and IR absorbed
50% penetrates (visible light) to about 1000m and decays exponentially with depth
Coastal vs Open Ocean Light Profiles
More scattering and absorption when more particulates in coastal waters. Less in open ocean
Coastal waters have green shifted light profiles from sediments
1% surface light at 10m in Coastal and 100m in open ocean
Light Exponential Decay
ID = IOe^(-kD)
ID = irradiance at depth (micromol photons/ms)
IO = irradiance at the surface (micromol photons/ms)
k = light extinction coefficient 1/m
D = depth
Light Extinction Coefficient
Describes how rapidly light is attenuated
k is higher in coastal waters
Composed of 3 terms: kw (water), kp (particulates) and kd (dissolved)
Two Ways to Measure k
PAR Sensor: Record light intensity directly at surface and at depth (k = ln(Io) - ln(ID) / D)
Secchi Disk: White circular disk lowered until not visible, that depth is Ds (k = 1.7/Ds)
Main Characters of Phytoplankton
Unicellular microscopic photoautotrophs
Very small in size
Most have a hard outer covering
Many are eukaryotic
Both prokaryotic and eukaryotic forms have thylakoids
Role of Phytoplankton in Marine Ecosystems
Primary producers in marine ecosystems
Form base of virtually all food webs
Represent available energy for transfer up the trophic pyramid
Form extensive blooms, can be toxic
Influence atmospheric and aquatic chemistry (produce O2, CO2 drawdown and C export, cloud formation)
Oil and sediment deposits
Major impact on global climate
Four Major Groups
Cyanobacteria
Diatoms
Coccolithophores
Dinoflagellates
Cyanobacteria
Two Main Groups
Prokaryotic
Coccoid: Discovered first because of bright orange phycoerythrin fluorescence
Prochlorophytes: Discovered later because of its dim red fluorescence
These two groups make up a major fraction of phytoplankton in ocean
Trichodesmium
N2 fixer and colonial or free-living filaments
Form large blooms and surface aggregationsDia
Diatoms
Have silica dioxide frustule
Single cells or chains of cells
Two Groups of Diatoms
Centric: Radial symmetry and pelagic
Pennate: Bilateral symmetry and benthic
What is a frustule made of
Made of silica and two valves (epitheca and hypotheca)
Raphe: elongated groove in frustule – excretes sticky stuff
Where are diatoms most productive
In areas of upwelling
Diatom sediment
They make silica sediment called diatomaceous earth found on sea bottom
Psuedonitzschia
This is a diatom that forms large toxic blooms off our shores
Domoic acid