142x Filetype PPTX File size 1.90 MB Source: www.hft.tu-berlin.de
Outline Underwater Optical Communications Introduction Underwater Channel Challenges Inter-Satellite Optical Communications Satellite-to-Underwater Optical Communications 2 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. 3 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 4 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. 5 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 6
no reviews yet
Please Login to review.