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Outline
Underwater Optical Communications
Introduction
Underwater Channel
Challenges
Inter-Satellite Optical Communications
Satellite-to-Underwater Optical Communications
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Underwater (UW) Optical Communications
Modeling the channel is the first step in UW communications
The channel is completely different from other FSO systems
The transmitter and receiver can be very similar to
aforementioned FSO systems
Ocean water has widely varying optical properties depending
on location, time of day, organic and inorganic content, as well
as temporal variations such as turbulence and surface motion.
To construct an optical link it is important to understand these
properties.
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UW Channel
The physical properties of water is important in modeling the
channel
Ocean water vary both geographically and vertically with depth
Geographically it changes from the deep blue ocean to littoral
waters near land
Vertically, the amount of light that is received from the sun is used
to classify the type of water.
The water depth also determines the background radiation from
sun light
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UW Channel
The topmost layer is called the euphotic zone and is defined by how
deeply photosynthetic life can be found
Below this zone is the
disphotic zone (1 km deep):
the light is too faint to
support photosynthesis.
From the lower boundary
of this zone and extending
all the way to the bottom is
the aphotic zone, where no
light ever passes and
animals have evolved to
take advantage of other
sources of food.
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UW Channel
The various water types are divided into two categories:
oceanic (blue water) and coastal waters (littoral zone).
The oceanic group is subdivided into 3 groups: Type I-III
types I: extremely pure ocean water
type II: turbid tropical-subtropical water
type III: mid-latitude water
The coastal group are subdivided into Types 1 through 9
1-9: coastal waters of increasing turbidity
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