1. Curt Mobley Sequoia Scientific, Inc. 2700 Richards Road, Suite 107 425-641-0944 ext 109 curtis.mobley@sequoiasci.com www.curtismobley.com Heavy stuff!!

2. relevant to this lecture: "The beginning of wisdom is calling things by their correct names." Antisthenes, 5 th century B.C., Greece relevant to the entire course: “Is it not pleasant to learn and to review constantly what one has learned?” Confucious, 6 th century B.C., China relevant to my lectures: “Do not worry about your difficulties in mathematics; I can assure you that mine are still greater." Einstein, 20 th century A.D., USA

3. Where we’re going today: Overview of quantities needed for this course: How do you quantitatively describe how much light there is, where it is going, etc.? (ref: Light and Water, Chapter 1) What is light? How to specify directions Radiance--the fundamental quantity for describing light Irradiances--often more useful Remote-sensing reflectance--fundamental to ocean color remote sensing Pretty picture

4. Light and Water, p 143

5. Light consists of elementary particles called photons, which are characterized by their wavelength  (or frequency  ) state of polarization Photons carry energy and (linear and angular) momentum have no detectable physical size (point particles, like electrons??) always travel at the same speed in vacuo Both wave and particle properties are always present, and this wave-particle duality cannot be described by classical physics; you must always use quantum mechanics and special relativity theory when describing photons. However, you can use either the wave or the particle properties to describe light, depending on which is convenient for your particular problem (e.g., photons are created or destroyed like particles, but propagate like waves). You will measure either the wave or particle properties of light, depending on the measurement device being used in the experiment. No one knows what photons actually are, but their behavior can be predicted.

9. Warning on directions: In radiative transfer theory (i.e., in the radiative transfer equation, in Light and Water, and in HydroLight),  and  always refer to the direction the light is going. Experimentalists often let  and  refer to the direction the instrument was pointed to measure the radiance. I call the instrument direction the viewing direction,  v and  v, where  v =  -  and  v =  + .

14. Radiance is always a bit hard to plot because of so many variables. Example plot: L(z, , ,  ) as a function of z and  for the nadir-viewing direction (aka the upwelling radiance L u : light traveling straight up, detector pointed straight down)

15. Another example plot: L(z, , ,  ) as a function of  and  at z = 5 m depth and  in the plane of the sun. Note: +z is downward, so  = 0 is light heading straight down, viewed by looking straight up in the  v = 180 deg direction.

17. Example plot: E d as a function of depth and wavelength

18. Another example plot: E d as a function of depth for 3 selected wavelengths

22. Ed(λ)Ed(λ) Lr(θ,φ,λ)Lr(θ,φ,λ) Lt(θ,φ,λ)Lt(θ,φ,λ) Lw(θ,φ,λ)Lw(θ,φ,λ) Lu(θ,φ,λ)Lu(θ,φ,λ) L u (θ,φ,λ) = L w (θ,φ,λ) + L r (θ,φ,λ) R rs (θ,φ,λ) = upwelling water-leaving radiance downwelling plane irradiance = L w (θ,φ,λ)/E d (λ) [sr -1 ] Remote-sensing Reflectance, R rs The foundation for ocean color remote sensing

23. Warning on spectral vs band-integrated radiance and irradiance: For example, spectral downwelling plane irradiance E d (  ) is per unit wavelength interval, with units of W m -2 nm -1. Band-integrated downwelling plane irradiance is the spectral irradiance integrated over some finite wavelength band, e.g., Note: PAR is always a band-integrated quantity.

24. Another warning: When reviewing papers I sometimes get “…and the measured irradiance was.75.” Which irradiance? Ed, Eu, Eo…? What units? W m -2 nm -1, W cm -2  m -1, W m -2 …? Is the magnitude 0.75, or is the. a fly spec, in which case the magnitude is 75? Sloppy notation and terminology + no units or inconsistent units = PAPER REJECTED!! (ditto for figures without axes labeled) “…and the measured downwelling spectral plane irradiance was 0.75 W m -2 nm -1. For brevity we henceforth call this the irradiance E.”

25. Rainbows (I can’t remember where, but somewhere out West, many years ago). There is much to see here: the order of the colors is different in the two bows, the sky appears darker between the bows, there is scattered white light on the inside of the primary bow, but not on its outside, etc. A polarizer will reveal much more….