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88 Cards in this Set

  • Front
  • Back

is based on the geometric phenomenon of triangulation.

GPS

the ground segment of GPS (US) has one master control, one alternative master control station, 12 command and control antennas and 16 monitoring site

Control segment

Working GPS Consist of two main components

Reciever


Location

collects satellite signals, and decodes and processes them.

Reciever

once the GPS receiver has located its position it is usually displayed in of two common format

Location

are angles both use the center of the earth as the vertex, but they use a different zero reference.

Latitudes and Longitudes

The world is divided into 60 zones of latitude, each 6' wide at the equator, that extend from 84' N to 80' s

UTM zone

the more spread out the satellites are in the sky, the better the satellite geometry

DOP

Advantage of GPS

Easy to navigate


Search for nearby area


Weather information


Tracking

implies that the location of the data items are known, or can be calculated, in terms of geographic coordinates (Latitude, Longitude)

Geographic

implies that the data in a GIS are organized to yield useful knowledge, often as colored map images, but also as statistical graphics, tables, and various on-screen responses to interactive queries.

Information

implies that a GIS is made up from several inter-related and linked components with different functions. GIS have functional capabilities for data input, manipulation.

System

a system of earth-orbiting satellites which can provide precise (100 m- sub-cm)

GPS

Use of Satellites or aircraft to capture information about the earths surface

RS

Software Systems with capabilities for input, storage, manipulation/analysis and output/display of geographic (spatial) information

GIS

Angles and Directions maybe defined by means of the following;

Bearings


Deflections angles


Azimuths


Angles to the right


Interior angles

Types of meridian

Assumed meridian


True meridian


Magnetic meridian

a fixed line of reference which may be any line in the survey or it may be purely imaginary.

Meridian

one which is arbitrarily chosen.

Assumed meridian

a true north – and – south line passing through the geographical poles of the earth.

True meridian

one which lies parallel with the magnetic lines of force of the earth as indicated by the magnetic needle.

Magnetic meridian

is the direction of any line with respect to a given meridian.

Bearing

Types of Bearing According to their corresponding line

True or astronomic bearing


Magnetic bearing


Assumed bearing

reckoned from the true meridian

True or astronomic bearing

reckoned from the magnetic meridian.

Magnetic bearing

reckoned from some arbitrary line of reference.

Assumed bearing

of a line is its direction given by the angle between the meridian and a line measured in a clockwise direction usually from the north branch of the meridian.

Azimuth

are customarily reckoned from the true south. In surveying, azimuths are reckoned from the north.

Azimuth

Types of Azimuth According to their line of References

Assumed azimuth


True azimuth


Magnetic azimuth

reckoned from any arbitrarily chosen line of reference.

Assumed azimuth

reckoned from the true south or true north.

True azimuth

reckoned from the magnetic north or magnetic south

Magnetic azimuth

is the angle between a succeeding line and the prolongation of the preceding line.

Deflection angle

In closed polygon, the angles inside two adjacent sides or lines are called

Interior angle

The angle between the true meridian and the magnetic meridian is called the

Magnetic declination

the north end of the compass needle points to the east of the true meridian.

East magnetic declination

the north end of the compass needle points to the west of the true

West Magnetic declination

Magnetic declination changes more or less systematically in cycles over period of approx. 300 years, one year or even one day.

Variation in magnetic declination

Types of variation

Secular variation


Annual variation


Daily variation


Irregular variation


Local attraction

the magnetic meridian swings in one direction for a century.

Secular variation

small annual ring; swing of the magnetic needle in a period of one year.

Annual variation

solar di-urnal variation; periodic swing of the magnetic needle in a period of one year.

Daily variation

due to magnetic disturbances because of sunspots. They cannot be predicted but are most likely to occur during magnetic storms.

Irregular variation

the deviation of the compass needle from the magnetic meridian caused by the presence of objects of iron or steel or some kinds of iron ore. Also called local disturbance.

Local attractions

It is a vast of land dominated by trees. A biological community consisting a plant (flora) and animals (fauna) living symbiotically on the same site. Is a land with an area of more than 0.5 hectare.

Forest

art of measuring horizontal and vertical distances between terrestrial points, angles between lines, and of determining the direction of lines and of establishing points by predetermined angular and linear measurements.

Surveying

is the application of science and maths to solve problems. While scientists and inventors come up with innovations, it is engineers who apply these discoveries to the real world.

Engineering

is the application of scientific, economic, social, and practical knowledge in order to invent, design, build, maintain, and improve structures, machines, devices, systems, materials and processes concerning to Forest.

Forest surveying and engineering

Two General Types of Surveying

Plain surveying


Geodetic surveying

Type of surveying that considered the earth as a plane and not a spheroid.

Plane surveying

takes into account the spheroidal surface of the earth.

Geodetic surveying

Importance of Surveying

Land Classification


Road Location


Location of nurseries, sawmills, spar trees, cable ways


Planting surveys for planting plan


Location of dam sites, irrigation canals


Determination of the place of fire in plantations


Settling boundary conflicts.

Kinds of Surveying (Operations of Surveying)

Land survey


Topographic survey


Route survey


Mine survey


Cadastral survey


City survey


Photogrammetric survey


Hydrographic survey

Use of the Bureau of Lands, Relocation Surveys.

Land surveys

securing of data necessary for the preparation of topographic maps. Determining elevation of points.

Topographic survey

for the location of transportation and communication lines.

Route survey

for mineral explorations.

Mine survey

to determine the extent, value, ownership, and transfer of lands for urban and rural areas.

Cadastral survey

in and near a city for purposes of planning city improvements.

City survey

application to surveying of the science of measurement by means of photographs.

Photogrammetric survey

survey of bodies of water for purposes of navigation, water supply or subaqueous construction.

Hydrographic survey

Principles Involved in Surveying

Geometry


Physics


Adjustments of errors


Trigonometry


Astronomy

Measurements are Inexact Even with the most sophisticated equipment, a measurement is only an estimate of the true size of a quantity . Exactness simply does not exist in the physical world.

Errors in measurement

Types of measurement

Direct measurement


Indirect measurement


Error measurement

Measurements made first-hand using some type of measuring device or instrument in a direct manner



Measurements made using an observable proportion or ratio



Defined as the difference between a measured value and the true value Mistakes are not errors. They are also called blunders

Direct measurements


Indirect measurement


Error measurement

Error source

Natural errors


Instrument errors


Personal erros


Errors caused by some variability in natural conditions such as temperature - Stretch in a steel tape, Pressure - measurements in a total station, wind-holding a level rod straight, magnetic declination - variation in a compass

Natural errors

Errors caused by imperfections in the manufacture of an instrument.

Instrument errors

The error caused by the inability to line up crosshairs exactly on a measurement point or sight exactly on a line.

Personal error

two types of errors related to measurements:

Systematic error


Random errors

Also called bias. Errors that are constant and also are cumulative.

Systematic error

These errors follow a natural distribution and tend to be offsetting.

Random errors

(the lack of systematic mistakes) is how close a measurement or observation is to the true value.

Accuracy

has two connotations. One is how many decimals of precision exist. Thus, a measurement of 8.4079 ft is said to be more precise than 8.4 ft.

Precision

Measurements of dimention

Horizontal length


Vertical length


Horizontal angle


Vertical angle

is the straight line distance measured in a horizontal plane. In most cases horizontal distance is calculated from a distance measured on a slope.

Horizontal length

is a measurement of a difference in height or elevation. Direct measurements can be made by an altimeter, which indicates barometric pressure or by a plumb line and tape for short vertical distances

Vertical length

A horizontal angle is the difference in direction betwe 1) two intersecting lines in a horizontal plane; (2) two intersecting vertical planes; or (3) two intersecting lines of sight to points in different vertical planes.

Horizontal angle

is the difference in direction between a horizontal plane and an intersecting line, plane, or a line of sight to a point. It is measured in the vertical plane in degrees of arc. Measurements are referenced "up" or "down" from the horizontal as "plus angles" or "minus angles"

Vertical angle

Rough measurement of horizontal distance, although it is a rapid means of approximating distances.

Pacing

length of step in walking, maybe measured from toe to toe or heel to heel.

PACE

equivalent to two or double step.

Stride

As the ratio of the measured distance in the number of paces made by an individual to cover the measured distance.

Pace factor

is also known as plane distance and is either measured directly with the measuring tape held so that the slope is zero or is calculated from the slope distance.

Horizontal distance

is the length of slope from the bottom to the top of the slope and is larger than both the vertical and horizontal distance. Slope distance can be calculated when the vertical height (rise)

Slope distance

It is often the case that a long horizontal distance will have a number of slope angle changes.

Breaking chain

At this point, it is a good time to talk about field book notation with regard to decimals.

Field book notation

device that shows the cardinal directions used for navigation and geographic orientation. It commonly consists of a magnetized needle or other element, such as a compass card or compass rose.

Compass