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SMS 204: Physics for marine sciences�Today’s topic: light and vision

Instructor: E. Boss

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What is light?

Light: electromagnetic radiation (energy) extending from ~300nm (UV) to ~800nm (IR). Visible light, 400-700nm.

Why should organisms care about (be affected by) light?

An available form of energy (sometimes damaging).

Enables sensing (phototaxis, vision).

Affects physical stratification (warms water).

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Available form of energy near the ocean surface.

Used as source of energy by:

  • Prokaryotes (with at least 3 different photosynthetic pathways with different electron donors).
  • Eukaryotes.
  • Multicellular plants (macro Algae).
  • Symbiotic algae (e.g. Zooxantella in corals).
  • Some Sea Slugs.

http://www.reefkeeping.com/issues/2002-06/bcap/feature/index.php

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Some ecological ‘behaviors’ associated with light:

Phototropism is plant growth towards a light source.

Photomorphogenesis is the light-induced control of plant growth and differentiation. Certain wave lengths function as a signal causing the generation of an information within the cell that is used for the selective activation of certain genes.

Photoperiodism is the ability of plants to measure the length of periods of light. Certain species (short-day plants) stop flowering as soon as the day length has passed a critical value, while long-day plants begin to flower only after such a value has been passed.

Circadian rhythm is the fact that many function of organism are regulated by the diel cycle. Artificial change of light periodicity often leads to change in the circadian rhythm (e.g. the division cycles of cyanobacteria and diatoms).

Phototaxis is the induction of movement of organisms to or from light. Diel migrations are observed in many marine organisms (think dinoflagellates, zooplankton, visual predators etc’).

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Relevant physical characteristics of light:

  • Quantized energy (photon) of a given frequency: E=hν

Where ν is frequency [s-1] and h=6.63 ⋅10-34 plank’s constant.

  • Distributed over a continuum of frequencies (wavelengths): λ=c/ν

Where c is the speed of light [m s-1] and l the wavelength [m nm A].

  • Polarized (has directionality) 🡨 affects vision and camouflage.

  • Propagates in vacuum (unlike sound). Slows down in water (changes wavelength).

n1c1=n2c2, where n is the (real part of the) index of refraction.

  • Refract, reflects and diffracts when encountering inhomogeneities: scatters off organisms and the environment (see later).

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The Solar Constant is 1366.1 W m-2. It is defined as the amount of solar radiation on a surface perpendicular to the solar beam, at the outer limit of earth’s atmosphere, at the mean sun-earth distance.

  • Why is it different at the TOA from ideal black body?
  • Why is it different at the Earth’s surface?

https://www.sciencedirect.com/topics/physics-and-astronomy/solar-spectra

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http://www.uwsp.edu/geo/faculty/ritter/

geog101/uwsp_lectures/lecture_earth_sun_relations.html

Sun light intensity as function of latitude changes with time of the year.

The cosine effect: E(θ)=Ecos(θ)*

*Note, from here on E denotes irradiance [W m2], not energy

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Solar Radiation Incident on the Ocean

  • Transmission through the atmosphere depends on:
      • Solar zenith angle (latitude, season, time of day)
      • Cloud cover
      • Atmospheric pressure (air mass)
      • Water vapor
      • Atmospheric turbidity
      • Column ozone (important for UV-B)
      • Albedo – scattering of light back to the atmosphere from below

  • Midsummer Solar Irradiance at 45°N (midday)
      • about 400 W m-2 (PAR, energy units)
      • 1900 µmol m-2 s-1 (PAR, quanta)
  • Midwinter Solar Irradiance at 45°N
      • about 130 W m-2; 600 µmol m-2 s-1

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UVA

UVB

Visible and UV Irradiance�Typical Spectrum for summer in Maine

  • -Visible: 400 to 700 nm
    • Also called Photosynthetically Available Radiation (PAR)

ABOUT 45% OF INCIDENT SOLAR RADIATION IS PAR

  • -Ultraviolet
    • UVA 315 (or 320) to 400 nm, UVB 280 to 320 nm, UVC 200 to 280 nm

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Examples: Vernal Equinox

Sun angle accounts for a 50% reduction. Atmospheric pathlength is also longer.

Diffuse irradiance is enriched in the shorter, scattered wavelengths

60°N — March 21 — noon

901 µmol m-2 s-1 PAR

Equator — March 21 – noon

2184 µmol m-2 s-1 PAR

Why is the color of the sky and the ‘blue’ oceans blue?

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Radiation within the water:

Changes in spectral light penetration with depth for different water bodies.

What causes the difference?

‘blue ocean’

‘Coastal’

‘Pond’

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Radiation within the water:

Attenuation of light with depth

Light attenuates approximately exponentially

Note: in an ocean with constant biogeochemistry and optical properties the diffuse attenuation coefficient, k, can still change with:

1. Sun angle (angle of light rays).

2. Depth (competition between absorption and scattering).

WRT PAR, kPAR is certain to change with depth (Morel, 1988, JGR) as different parts of the spectrum attenuate at different rates (e.g. after a few meters very little NIR is left due to water absorption) to contribute to PAR.

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Loss due to absorption and scattering (attenuation)

Φa Absorbed Radiant Flux

Φb Scattered Radiant Flux

Φt

Φo

Incident

Radiant

Flux

Transmitted

Radiant

Flux

Absorption: disappearance of photons along the beam path.

Scattering: redirection of photons away from the beam path.

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The ocean is a dilute medium containing a complex mixture of particulate and dissolved materials

What interacts with light?

water, algae, dissolved organics, non-algal particles (organic and inorganic).

+ Fluorescence.

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Spectral characteristics of absorbing agents in the oceans:

These absorbing agents affect phytoplankton by ‘competing’ on photons (as well as removing potentially harmful ones in the UV).

These absorbing agents affect visual organism by changing the spectrum of available light.

Beer Lambert’s law:

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Phytoplankton chromatic adaptation:

Changing number of pigment complexes, amount of pigments and types of pigments in response to changing light.

Different species adapt to the low light levels by (O(day)):

  • Producing more pigments.
  • Producing accessory pigments.

Different species adapt to high light levels by (O(day)):

  • Reducing pigmentation
  • Producing photoprotective pigments

Short term adaptations (O(sec-min)):

  • Migration of chloroplasts to the center of the cell (self-shading)
  • Dissipation of excess photons to heat
  • Nonphotochemical quenching - reduction of fluorescence in cells that have recently been exposed to high light levels.

NB: Macro- and Micro-nutrient availability affects the ability of cells to cope with changes in light.

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Scattering:

Affecting light propagation, refraction, reflection and diffraction

Increases with ‘index of refraction’, a measure of how different the light speed is within the particle.

Increases with size. Mass-normalized scattering has a peak at micron-sized particles.

Angular scattering changes with size. Symmetric when D<<λ and forward peaked with D>λ.

Spectral dependency ~ λ0🡪-4

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Pigment biomass is often not phytoplankton (volume) biomass

Fennel and Boss, 2003. Data from 1989-2000 (C. D. McIntyre)

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Chlorophyll fluorescence is NOT chlorophyll:

Falkowski and Raven, 1997

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Some concepts associated with vision and imaging:

Contrast.

Scattering effects?

Absorption effects?

High contrast

Low

contrast

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Pin-hole optics - light travels in straight lines

Eyes: in many organisms, including jellyfish…

SMS 204: Integrative Marine Sciences II

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The human eye perceives photopic parameters, that is, it observes light spectra convolved with the spectral sensitivity of the human eye.

UV NIR and polarized…

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Polarized vision and ecological functions

Secret communication (cuttlefish)

Navigation (Bee’s)

Detection of nearby water surface

Target recognition

Breaking camouflage

Increase detection range (enhance contrast)

This ctenophore plankton can be squid prey. Almost transparent to normal vision (left), it acquires good contrast between crossed polarizer (center), and even better with combined processing (right). �From: http://polarization.com/octopus/octopus.html

Common to crustaceans, cephalopods and some fishes

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Marine birds could use polarization to see through the surface:

Some shrimp send sexual messages through polarized signals

http://oceanexplorer.noaa.gov/explorations/04deepscope/background/polarization/polarization.html

Bikini bottom is not the same without my glasses

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Summary:

  • Light is one of the primary determinant of habitat in the oceans.

  • Primary energy source of the biogenic food web.

  • Light is also used for ecological functions such as finding prey/food, locating mate, and evading predators.

  • Bulk/individual optical properties and imaging are common strategies to study biological oceanography.