STANDARD - Survey Instrument Antique Center!
STANDARD - Survey Instrument Antique Center!
STANDARD - Survey Instrument Antique Center!
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68<br />
From the -(- sign of the " difference" of declination, we see that the decimation is<br />
of the same name as the latitude, whence the correction is an increment, and accordingly<br />
the -f- sign as suffixed. This sign belongs to the refraction.<br />
When the object is in the meridian, refraction a.ffects declination by its full<br />
amount; but, if both the observer and the object were in the plane of the equator,<br />
refraction would have no effect on the object with regard to refraction ; whence, between<br />
these limits, only a part of refraction is effective in changing the declination.<br />
Just what portion is effective, is shown by table II. of this paper.<br />
Thus, in the given Lat. 44, and for, say 4 hours from noon, the percentage of re-<br />
fraction to be is .74 of that<br />
applied corresponding to the altitude of the object at the<br />
time of observation. The sign ^ to be used must be determined, as above, by considering<br />
whether the sun is going north or south at the time.<br />
This part of the reduction of declination cannot, of course, be made till the altitude<br />
is found at the time of observation.<br />
To Find the Latitude.<br />
Having prepared the declination for the day, as above, level up the transit carefully.<br />
Level the main telescope, observing that the vertical arc reads zero, arid set<br />
the polar axis to a vertical position by means of the solar telescope level.<br />
These points being attained, set the main telescope, pointing south. Then for a<br />
declination ><br />
south [<br />
the south end of the te1680^ elevate |<br />
6 tin . the vertical arc in-<br />
dicates the declination thus found.<br />
Then, having turned the solar telescope into a vertical plane parallel with that<br />
containing the optical axis of the main telescope, level it carefully and clamp it.<br />
A few minutes before the time of the sun's culmination, bring the telescope into<br />
with<br />
1 '<br />
the vertical plane passing through the observer and the sun, and "find the sun<br />
the solar telescope. This is readily done by varying the altitude when the sun's<br />
image will appear on the diagonal eye-piece.<br />
Having "found the sun," bisect his image with the vertical wire, by varying the<br />
azimuth with the tangent screw of the transit plate, or with that of the outer center;<br />
and, simultaneously, follow him in altitude the horizontal wire bisecting the image<br />
till it ceases to rise, then clamp and read the vertical arc. This reading should<br />
be the sum of the co-latitude and refraction, the refraction being that due to the meridian<br />
altitude of the sun, which is the algebraic sum of declination and co-latitude. From<br />
this reading the latitude is readily deduced. With the latitude and declination<br />
known, we are prepared<br />
To Find the Meridian.<br />
(a.) As for finding latitude, level up the instrument carefully, the vernier of plate<br />
lamped, reading zero.<br />
(b.) Point the telescope to the sun to find his altitude for the refraction. This<br />
can be found with sufficient accuracy by turning the telescope, till the shadow of a<br />
pencil held across the end, or till the shadow of the screws on the side, are parallel<br />
with the tube.<br />
(c.) The refraction corresponding to this altitude must be multiplied by the corresponding<br />
coefficient, for the time from noon and the latitude, and applied to the<br />
declination, as per instructions above, for the corrected declination.<br />
(d.) Point the telescope to the south, tne south end for decli<br />
^evithi'g )<br />
south |<br />
'<br />
nation, till the vertical arc reads the corrected declination, and clamp the vertical<br />
arc.<br />
(e.) The main telescope being dipped to the corrected declination, level the solar<br />
telescope by means of its level, being careful to do so when it is in a vertical plane<br />
parallel with that containing the optical axis of the main telescope, for only when it<br />
is in this plane can the declination be properly set off.<br />
(f.) Elevate the south end of the main telescope to the co-latitude, by means of<br />
the vertical arc, and turn the telescope approximately into the meridian, by means<br />
of tb magnetic needle.<br />
(g.) " Find the sun " with the solar telescope. This is done by turning the whole instrument<br />
in azimuth, on its outer center, simultaneously with a motion of the solar telescope<br />
in right ascension, till the sun's image is seen in the eye-end of solar telescope.<br />
Bisect the image, as nearly as may be, by the two motions above named clamp<br />
and complete the bisection, by both wires, or by the wires forming a square, by means<br />
of the transit's lower tangent screw, and by that of the solar telescope. If the image<br />
of the sun should be so large that it cannot all be seen from one position of the eye.