The length of the air base is increased
The scale of the model is altered
y-parallax is not affected
All the above
D. All the above
f tan θ
f sin θ
f cot θ
f cos θ
The horizontal direction of the pole is called astronomical north
The angle between the direction of true north and the direction of a survey line is called astronomical bearing
The astronomical bearing is generally called azimuth
All the above
In truly vertical photographs without relief angles are true at the plumb point
In tilted photographs without relief, angles are true at the iso-centre
In tilled photographs with relief, angles are true at the principal point
None of these
The standard meridian
The international date line
That of Greenwich
Both (a) and (c) of above
Refraction correction is zero when the celestial body is in the zenith
Refraction correction is 33' when the celestial body is on the horizon
Refraction correction of celestial bodies depends upon their altitudes
All the above
Greater than the longitude of the place
Less than the latitude of the place
Equal to the latitude of the place
None of these
Astronomical latitude
Astronomical longitude
Astronomical bearing
All of these
High oblique
Low oblique
Vertical
None of these
Standard meridian
Greenwich meridian
Equator
180° longitude
One less than mean solar days
One more than mean solar days
Equal to mean solar days
None of these
1 m
2 m
4 m
8 m
Length of the equator between their longitudes
Length of the parallel between their longitudes
Length of the arc of the great circle passing through them
None of these
The sun's right ascension increases for 0 h to 24 h when it returns to the First point of Aries
The maximum declination of the sun increases up to 23 ½° N on about 21st June
The minimum declination of the sun is zero' on 22nd September
All the above
sin H = tan φ . cot δ
cos H = tan φ . cot δ
tan H = tan φ . cot δ
None of these
Once
Twice
Thrice
Four times
L.M.T. - East longitude in time
L.M.T. + East longitude in time
L.M.T. - West longitude in time
None of these
Positive for points above datum
Negative for points below datum
Zero for points vertically below the air station
All the above
Plane surveying
Geodetic surveying
Star observations
Planet observations
Nadir point
Iso centre
Principal point
All the above
Co-declination
Co-altitude
Co-latitude
Polar distance
sin a cos A
cos a sin A
tan a cot A
cot A tan a
h tan α/S
h tan β/S
h (tan α + tan β)/S
h (tan α - tan β)/S
The vertical plane containing the zenith, the station of observation and the celestial pole is the observer's meridian plane
The angle between the direction of star in vertical plane and the direction of the star in horizontal plane is called the altitude of the star
The complement of the altitude of star is called the zenith distance of the star
All the above
Parallax
Height
Parallax difference
Height difference
North end of the polar axis is known as North Pole
South end of the polar axis is known as South Pole
Point where polar axis when produced northward intersects the celestial sphere, is known as north celestial pole
All the above
Horizon and equator
Equator and zenith
Zenith and pole
Pole and horizon
Ground principal point
Ground plumb point
Iso-centre
Perspective centre
1000 km
800 km
600 km
500 km
Altitude and azimuth system
Declination and hour angle system
Declination and right ascension system
Declination and altitude system
Reduction to mean sea level
Correction for horizontal alignment
Correction for slope
All the above