midterm 2 part 2 Flashcards
Waters general characteristics that enable to store great quantities of heat
- It’s high heat capacity
- Transparent to light
- Mixes vertically
Attenuated
Light that is lost by a combination of absorption and scattering
Absorption
Water molecules absorb some light energy
Most light energy is absorbed by various particles in the water and dissolved materials
Lakes have a lot of dissolved materials making them a yellow brown colour, therefore, less light penetrates to the bottom
Scattered
Reflects off of particles, including air bubbles and dissolved materials
Beer’s Law:
The rate of light attenuation is constant
* Every meter a certain percentage is lost
Extinction coefficient:
Constant rate light is lost, ranges from 0 to 1.0
Diffuse attenuation coefficient:
Represented by k, function of the degree to which the water is clouded with dirt and other foreign materials
Diffuse attenuation coefficient: High k means
- Lots of dissolved materials
* Often the case for coastal waters
* The faster light disappears with depth
Electromagnetic spectrum:
ranges of wavelength from cosmic rays to radio waves, includes viable light
Visible light: 400-700nm
Red 700nm, Purple 400nm
Selective attenuation:
Longer wavelengths (red, 700nm) as the penetrate into the ocean
* Are absorbed before they penetrate very deep * Why the sea is blue to blue-green colour as shorter wavelets are less attenuation the least
Air Composition:
- Nitogene 78%
- Oxygene 21%
- Other trace gases 1%
- Water vapour: Up to 4%
warmer air is ___ dense than cold hair
less, therefore it rises
Dew point:
air has become saturated with water vapour and can not hold any more
warm air can hold ___ water vapour
more, therefore becomes less dense, and rises