Geometry

We now develop the mathematical tools needed to specify directions and angles in three-dimensional space. These mathematical concepts are fundamental to the specification of how much light there is and what direction it is traveling.

Directions

We have frequent need to specify directions. In order to do this in Euclidean three-dimensional space, let $î1$, $î2$, and $î3$ be three mutually perpendicular unit vectors that define a right-handed Cartesian coordinate system. We choose $î1$ to be in the direction that the wind is blowing over the ocean surface, (i.e. $î1$points downwind), and $î3$points downward, perpendicular to the mean position of the water surface; $î2$is then in the direction given by the cross (or vector) product $î2$= $î3$$\times$ $î1$. Our choice of a ”wind-based” coordinate system simplifies the mathematical specification of sea-surface wave spectra, as must be done when we discuss radiative transfer across a wind-blown sea surface. The choice of $î3$ pointing downward is natural in oceanography, where depths are customarily measured as positive downward from an origin at mean sea level.

With our choice of $î1$, $î2$, and $î3$, an arbitrary direction can be specified as follows. Let $\widehat{\xi }$denote a unit vector pointing in the desired direction. The vector $\widehat{\xi }$has components $\xi 1$, $\xi 2$, and $\xi 3$in the $î1$, $î2$, and $î3$directions, respectively. We can therefore write $\widehat{\xi }$= ${\xi }_1$$î1$+ ${\xi }_2$$î2$+ ${\xi }_3$$î3$, or just $\widehat{\xi }$= (${\xi }_1,{\xi }_2,{\xi }_3$) for notational convenience. Note that because $\widehat{\xi }$is of unit length, its components satisfy ${\xi }_1^2+{\xi }_2^2+{\xi }_3^2=1.$

An alternative description of $\widehat{\xi }$is given by the polar coordinates $𝜃$ and $\varphi$, defined as shown in Fig. 1. The nadir angle $𝜃$ is measured from the nadir direction $î3$ and the azimuthal angle $\varphi$ is measured positive counterclockwise from $î1$, when looking toward the origin along $î3$ (i.e. when looking in the $-$$î3$ direction). The connection between $\widehat{\xi }$ = (${\xi }_1,{\xi }_2,{\xi }_3$) and $\widehat{\xi }$ = ($𝜃,\varphi$) is obtained by inspection of Fig. 1:

$$\begin{array}{llll}\hfill {\xi }_1=& sin𝜃cos\varphi & \hfill & \\ \hfill {\xi }_2=& sin𝜃sin\varphi & \hfill \text{(1)}\\ \hfill {\xi }_3=& cos𝜃& \hfill & \end{array}$$ where $𝜃$ and $\varphi$ lie in the ranges $0\le 𝜃\le \pi$ and $0\le \varphi <2\pi$. The inverse transformation is

$$\begin{array}{llll}\hfill 𝜃=& {cos}^{-1}\left({\xi }_3\right)& \hfill & \\ \hfill \varphi =& {tan}^{-1}\left(\frac{{\xi }_2}{{\xi }_1}\right)& \hfill \text{(2)}\end{array}$$ The polar coordinate form of $\widehat{\xi }$could be written as $\widehat{\xi }$= $\left(r,𝜃,\varphi \right),$ but since the length of $r$ is 1, we drop the radial coordinate for brevity.

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Another useful description of $\widehat{\xi }$is obtained using the cosine parameter

$$\mu \equiv cos𝜃={\xi }_3.$$

(3)

The components of $\widehat{\xi }$= (${\xi }_1,{\xi }_2,{\xi }_3$) and $\widehat{\xi }$= ($\mu ,\varphi$) are related by

$$\begin{array}{llll}\hfill {\xi }_1=& {\left(1-{\mu }^2\right)}^{1∕2}cos\varphi & \hfill & \\ \hfill {\xi }_2=& {\left(1-{\mu }^2\right)}^{1∕2}sin\varphi & \hfill \text{(4)}\\ \hfill {\xi }_3=& \mu ,& \hfill & \end{array}$$ with $\mu$ and $\varphi$ in the ranges $-1\le \mu \le 1$ and $0\le \varphi <2\pi$. Hence a direction $\widehat{\xi }$ can be represented in three equivalent ways: as (${\xi }_1,{\xi }_2,{\xi }_3$) in Cartesian coordinates, and as ($𝜃$, $\varphi$) or ($\mu$, $\varphi$) in polar coordinates.

The scalar (or dot) product between two direction vectors $\widehat{{\xi }^{\prime }}$ and $\widehat{\xi }$ can be written as

where $\psi$ is the angle between directions $\widehat{{\xi }^{\prime }}$ and $\widehat{\xi }$, and $\left|\widehat{\xi }\right|$ denotes the (unit) length of vector $\widehat{\xi }$. The scalar product expressed in Cartesian-component form is

Equating these representations of $\widehat{{\xi }^{\prime }}\cdot \widehat{\xi }$ and recalling Eqs. (1) and (4) leads to

$$\begin{array}{llll}\hfill cos\psi & ={{\xi }^{\prime }}_1{\xi }_1+{{\xi }^{\prime }}_2{\xi }_2+{{\xi }^{\prime }}_3{\xi }_3& \hfill & \\ \hfill & =cos{𝜃}^{\prime }cos𝜃+sin{𝜃}^{\prime }sin𝜃cos\left({\varphi }^{\prime }-\varphi \right)& \hfill \text{(5)}\\ \hfill & ={\mu }^{\prime }\mu +\sqrt{1-{{\mu }^{\prime }}^2}\sqrt{1-{\mu }^2}cos\left({\varphi }^{\prime }-\varphi \right)& \hfill & \end{array}$$

Equation (5) gives very useful connections between the various coordinate representations of $\widehat{{\xi }^{\prime }}$ and $\widehat{\xi }$, and the included angle $\psi$. In particular, this equation allows us to compute the scattering angle $\psi$ when light is scattered from an incident to a final direction.

The set of all directions $\widehat{\xi }$ is called the unit sphere of directions, denoted by $\Xi$. Referring to polar coordinates, $\Xi$ therefore represents all $\left(𝜃,\varphi \right)$ values such that $0\le 𝜃\le \pi$ and $0\le \varphi <2\pi$. Two subsets of $\Xi$ frequently employed in optical oceanography are the downward (subscript d) and upward (subscript u) hemispheres of directions, ${\Xi }_d$ and ${\Xi }_u$, defined by

$$\begin{array}{llll}\hfill {\Xi }_d& \equiv \text{ all }\left(𝜃,\varphi \right)\text{ such that }0\le 𝜃\le \pi ∕2\text{ and }0\le \varphi <2\pi ,& \hfill & \\ \hfill {\Xi }_u& \equiv \text{ all }\left(𝜃,\varphi \right)\text{ such that }\pi ∕2<𝜃\le \pi \text{ and }0\le \varphi <2\pi .& \hfill & \end{array}$$

Solid Angle

Closely related to the specification of directions in three-dimensional space is the concept of solid angle, which is an extension of two-dimensional angle measurement. As illustrated in panel (a) of Fig. 2, the plane angle $𝜃$ between two radii of a circle of radius r is

The angular measure of a full circle is therefore 2$\pi$ rad. In panel (b) of Fig. 2, a patch of area A is shown on the surface of a sphere of radius r. The boundary of A is traced out by a set of directions $\widehat{\xi }$. The solid angle $\Omega$ of the set of directions defining the patch A is by definition

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Since the area of a sphere is $4\pi r^2$, the solid angle measure of the set of all directions is $\Omega \left(\Xi \right)=4\pi rmsr$. Note that both plane angle and solid angle are independent of the radii of the respective circle and sphere. Both plane and solid angle are dimensionless numbers. However, they are given ”units” of radians and steradians, respectively, to remind us that they are measures of angle.

Consider a simple application of the definition of solid angle and the observation that a full sphere has $4\pi sr$. The area of Brazil is $8.5\cdot 10^6{km}^2$ and the area of the earth’s surface is $5.1\cdot 10^8{km}^2$. The solid angle subtended by Brazil as seen from the center of the earth is then $4\pi 8.5\cdot 10^6∕5.1\cdot 10^8=0.21sr$.

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The definition of solid angle as area on the surface of a sphere divided by radius of the sphere squared gives us a convenient form for a differential element of solid angle, as needed for computations. The blue patch shown in Fig. 3 represents a differential element of area $dA$ on the surface of a sphere of radius $r$. Simple trigonometry shows that this area is $dA=\left(rsin𝜃d\varphi \right)\left(rd𝜃\right).$ Thus the element of solid angle $d\Omega \left(\widehat{\xi }\right)$ about the direction $\widehat{\xi }$= ($𝜃,\varphi$) is given in polar coordinate form by

$$\begin{array}{llll}\hfill d\Omega \left(\widehat{\xi }\right)=& \frac{dA}{r^2}=\frac{\left(rsin𝜃d\varphi \right)\left(rd𝜃\right)}{r^2}=sin𝜃d𝜃d\varphi & \hfill & \\ \hfill =& d\mu d\varphi \text{(sr)}.& \hfill \text{(6)}\end{array}$$

(The last equation is correct even though $d\mu$ = $dcos𝜃$ = $-sin𝜃d𝜃$. When the differential element is used in an integral and variables are changed from ($𝜃,\varphi$) to ($\mu ,\varphi$), the Jacobian of the transformation involves an absolute value.)

Example: Solid angle of a spherical cap

To illustrate the use of Eq. (6), let us compute the solid angle of a “polar cap” of half angle $𝜃$, i.e. all (${𝜃}^{\prime },{\varphi }^{\prime }$) such that $0\le {𝜃}^{\prime }\le 𝜃$ and $0\le {\varphi }^{\prime }<2\pi$. Integrating the element of solid angle over this range of (${𝜃}^{\prime },{\varphi }^{\prime }$) gives

$${\Omega }_{\text{cap}}={\int \; <!--nolimits-->}_{{\varphi }^{\prime }=0}^{2\pi }{\int \; <!--nolimits-->}_{{𝜃}^{\prime }=0}^{𝜃}sin{𝜃}^{\prime }d{𝜃}^{\prime }d{\varphi }^{\prime }=2\pi \left(1-cos𝜃\right),$$

(7)

or

$${\Omega }_{\text{cap}}={\int \; <!--nolimits-->}_{{\varphi }^{\prime }=0}^{2\pi }{\int \; <!--nolimits-->}_{{\mu }^{\prime }=\mu }^{1}d{\mu }^{\prime }d{\varphi }^{\prime }=2\pi \left(1-\mu \right).$$

(8)

Note that ${\Xi }_d$ and ${\Xi }_u$ are special cases of a spherical cap (having $𝜃=\pi ∕2$), and that $\Omega \left({\Xi }_d\right)=\Omega ({\Xi }_u$) = $2\pi sr$.

Delta functions

It is sometimes convenient to specify directions using the Dirac delta function, $\delta \left(\widehat{\xi }-{\widehat{\xi }}_o\right)$. This peculiar mathematical construction is defined (for our purposes) by

$$\delta \left(\widehat{\xi }-{\widehat{\xi }}_o\right)\equiv 0if\widehat{\xi }\ne {\widehat{\xi }}_o,$$

(9)

and

$${\int \; <!--nolimits-->}_{\Xi }f\left(\widehat{\xi }\right)\delta \left(\widehat{\xi }-{\widehat{\xi }}_o\right)d\Omega \left(\widehat{\xi }\right)\equiv f\left({\widehat{\xi }}_o\right).$$

(10)

Here $f\left(\widehat{\xi }\right)$ is any function of direction. Note that $\delta \left(\widehat{\xi }-{\widehat{\xi }}_o\right)$ simply ”picks out” the particular direction ${\widehat{\xi }}_o$ from all direction in $\Xi$. Note also in Eq. (10) that because the element of solid $d\Omega \left(\widehat{\xi }\right)$ has units of steradians, it follows that $\delta \left(\widehat{\xi }-{\widehat{\xi }}_o\right)$ has units of inverse steradians.

Equations (9) and (10) are a symbolic definition of $\delta$. The mathematical representation of $\delta \left(\widehat{\xi }-{\widehat{\xi }}_o\right)$ in spherical coordinates ($𝜃$,$\varphi$) is

$$\delta \left(\widehat{\xi }-{\widehat{\xi }}_o\right)=\frac{\delta \left(𝜃-{𝜃}_o\right)\delta \left(\varphi -{\varphi }_o\right)}{sin𝜃}\left({sr}^{-1}\right),$$

(11)

where $\widehat{\xi }$ = $\left(𝜃,\varphi \right)$, ${\widehat{\xi }}_o=\left({𝜃}_o,{\varphi }_o\right)$, and

$$\begin{array}{llll}\hfill {\int \; <!--nolimits-->}_0^{\pi }f\left(𝜃\right)\delta \left(𝜃-{𝜃}_o\right)d𝜃\equiv & f\left({𝜃}_o\right)& \hfill & \\ \hfill {\int \; <!--nolimits-->}_0^{2\pi }f\left(\varphi \right)\delta \left(\varphi -{\varphi }_o\right)d\varphi \equiv & f\left({\varphi }_o\right).& \hfill & \end{array}$$ Note that the $sin𝜃$ in the denominator of Eq. (11) is necessary to cancel the $sin𝜃$ factor in the element of solid angle when integrating in polar coordinates. Thus

$$\begin{array}{llll}\hfill & {\int \; <!--nolimits-->}_{\Xi }f\left(\widehat{\xi }\right)\delta \left(\widehat{\xi }-{\widehat{\xi }}_o\right)d\Omega \left(\xi \right)=& \hfill & \\ \hfill & {\int \; <!--nolimits-->}_0^{2\pi }{\int \; <!--nolimits-->}_0^{\pi }f\left(𝜃,\varphi \right)\frac{\delta \left(𝜃-{𝜃}_o\right)\delta \left(\varphi -{\varphi }_o\right)}{sin𝜃}sin𝜃d𝜃d\varphi =& \hfill & \\ \hfill & f\left({𝜃}_o,{\varphi }_o\right)=f\left({\widehat{\xi }}_o\right).& \hfill & \end{array}$$

Likewise, we can write

$$\delta \left(\widehat{\xi }-{\widehat{\xi }}_o\right)=\delta \left(\mu -{\mu }_o\right)\delta \left(\varphi -{\varphi }_o\right)\left({sr}^{-1}\right),$$

(12)

where