Introduction to Hydrographic Surveying

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1
Hydrographic surveying
surveying of water environments; considered the wet equivalent of topographic surveying.
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Hydrographic maps or nautical charts
maps that delineate submerged surfaces and provide data on water depths and underwater features.
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Hydrography
science of water surveying.
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Sounding
measurement of water depth.
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Stream gaging
measurement of stream discharge.
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Discharge
volume of water flowing per unit time.
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Fathom
unit of depth equal to 6 feet.
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Hydrographic chart
map showing water depths and features.
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Subaqueous contour
line connecting points of equal underwater elevation.
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Dredging
removal of underwater material.
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Stream
natural watercourse.
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1. Station location
2. Water depth
3. Discharge measurement
Basic Requirements
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1. Water Resources and Development
2. Transportation and Infrastructure
3. Navigation and Underwater Investigation
Applications of Hydrographic Surveying
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Tides
periodic changes in water level caused mainly by the gravitational effects of the Moon and Sun.
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Moon
primary celestial body responsible for tides.
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Sun
also contributes to tides through its gravitational attraction.
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Tidal current
horizontal movement of tidal water.
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Flood tide
incoming tide, when water moves toward the shore or into an area.
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Ebb tide
outgoing tide, when water moves away from the shore or out of an area.
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Slack water
period when there is little or no tidal current between incoming and outgoing tidal currents.
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Set
direction of the tidal current.
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Drift
speed of the tidal current.
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High water
maximum water level.
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Low water
minimum water level.
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Tide range
difference between high water and low water.
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Tidal day
period between successive high waters.
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Stand
period of little tidal change.
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Mean sea level
average sea surface level.
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Mean low water
average low-water level.
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Mean lower low water
average of the lower low waters.
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Semidiurnal tide
has two high waters and two low waters each day.
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Diurnal tide
has one high water and one low water each day.
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Mixed tide
has unequal high waters and unequal low waters.
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Tidal waves
long-period movements of tidal water.
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Tidal bores
occur when tidal waves move rapidly through rivers.
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1. Navigation
2. Salvaging
3. Fishing
Tidal information is particularly important in:
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Reconnaissance
first basic operation; involves inspecting the survey area before conducting the actual survey.
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Horizontal control
establishes the horizontal positions of survey observations.
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Vertical control
establishes the elevations or vertical references.
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Topographic survey
determines land features.
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Hydrographic survey
measures underwater features.
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Map preparation
produces the final hydrographic map.
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Sounding craft
vessel used for sounding.
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Sounding pole
measures shallow-water depth.
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Lead line
uses a weighted line to measure depth.
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Sounding machine
mechanically measures water depth.
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Fathometer
uses sound waves to measure water depth.
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Signals
provide position and navigation references.
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Tide gauges
measure water levels.
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Chief of party
leads the sounding chart party.
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Instrument man
operates surveying instruments.
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Recorder
records survey measurements.
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Leadsman
handles the sounding lead.
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Coxswain
operates the sounding craft.
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Lookout
watches for hazards.
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Signal man
communicates signals during sounding.
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Fathometer attendant
operates the fathometer.
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