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N

A

v

1

G

12 milEs, AC egu.1

to

.o.~

aod ,he aogle BAC egu.1

10

33°

45', ,h; .dil!>n"< be, ,"eeo ,he

SEóS

aod

ESE

Ijnes. ' Vhcnce for the anLle

al

B.

il

will be,

As ,he fum

of

lh< fides AC aocl AB

3' 9

1.517'°

j~

10 lheir dill'ereoee

S·9 - 0 ·94930

fo io lhe

,~og.

of half 'he}

730,

07' _ 10 .5 1 606

fum of ,he .ngles B and C

to

taog.

of {lheir dilf.

41°, 43 '

T -

9·950 25

confequeotly ,he aogle B is

I

14°

5~ ',

aod fo Ihe leuiog

of ,he curreo' \ViII be

N

SI° 06'

E

or

EbE

2° 21 '

E.

Then for

Be

the

cu rrcol's

drifr in 3 hours,

it

wil!

be,

AsthelineofB

11 4°,51'

9·9' i OO

js 'o ,he dil!.oce run AC 20.9

1.3:02 5

foisthefioeofA

33°,45'

9·74474

t é

BC

12 .S

1.

10

7 19

lhe cllrrent's

drift

in

3 hours. and

co¡:¡fcquently

the

CUT·

rent fe\s

EóN

2° 2 l '

E 4.266

mi les an hour .

Sea. 8.

C'JI/('~,.nir.glh~

VAltlATION

of

l A!

COMPASS,

4nd

ho'UJ lo

jiJJd ;1

jro1Jl Ihe Iru,

4nd

objervd

A Ol PL l'

'TUDE8

Ir

A2IMVTHS O/th~ftln.

l.

T

H

E

variation of the compafs is how far the north

or

routh

poinr

of the needle Hands (rom the true

routh

or

north

paiOI

of the horizon towards tht:.

can

or

wen;

or

it

is 3n

arch

of lhe harizon intercepted

betw(!'eo the

m:·

ridian

of the place of obCcrvation éind the magnetic

me

ridian .

2. It is .abColutely necdTary to know (he variation of

the compaCs

al

f~a ,

in

order

[O

correél: {he {hip's courCe;

for fioee the !h¡p's eourfe i. direéted by the eompars, it is

evideot that

ir

the compars be

wrong

the

true

courfe wiU

differ from the o" fer",d, aod eoofe'luently the whole

reckoniog differ from {he truth.

3. The fun's true amplitude is an arch

oF

the horizon

comprehended becween che true eafl or wefi poinr thereof,

and lhe centre of the {un at ri{iog or Ceuine; or

it

is che

number

of

degrees,

&/,:.

that the centre

of

the Cuo is di·

fiant from

lhe

true ean or weH pOlDt

of the

horizon, to·

waFds the fouth or north .

4.

The

{un's

magnetic amplitude

i~

lhe

number

of

de·

grees

that tbe centre

of the

{uo is

from

(he

e;¡{l

or

~eH

POiOI

of the compaf., ,owards Ihe fou,h or oOrlh FOln, of the

fame at

rifing

or

feuing.

5.

Having thedeclinalionofthe fun,

together

with the

btitude of

the

place of

obrervation,

·\Ve

may from

thence

bod the fun's \Tue amplitude, by ,he following allronomic

proporition,

viz.

As the eo·line of tbe latitude

ís to

the

radius

S o is tbe

fine

of 1he

fun's

dceJination

tOlhe fine of lhe rlln'S lrue amp1itude

whieh

\ViII

be north or fouth aeeordi\lg as tbe fuo's declino·

tion is

north or romh .

EXAMPLE .

R equired lhe

fun's

true amplitude in lhe

lali,ude of 4to 50' oonh,

00

the 23d d.y of A pril 173 1.

Firll, I find (from Ihe lables of ,he fun's declioation)

tbatlhe fuo', declinalioo Ihe 23d of April is 15

0

54' north;

, hen for Ibe \Tue ampli,ude, it will be, by the former ana·

logy .

A, Ihe eo Iin, of Ihe !at, 410 50'

9 .8722

I

is

to

rad~us

10.COOOO

A

T

o

N .

fo i. ,he fine of Ihe der\. 15°, 5.1 ,

9 ' 437 69

tothefineoft.heampht. 21, 35 ,

9' S6S48

whieb

i.s

nonh, bee,lUfe lh e

decbnation

is nonh

at that

ti:lIt; anJ

confequently, in

the latitucie

of

41

o

50'

nonh.,

the fuo , ir.. on ,be 2

3d

of April 2'"

~5'

from the ..

11

pan of

the

horizon

tow;uds the

north, and

rets

fo much

from ,he \VeCl,he f, me \Vay .

6. The run's

true

3zimuth

jo;

the

areh

of the horiZOD

intercepted betwec n (he mcridian aod (be

vertical

circlc

.palTing through the centre

of

the fun

at

tbe time of

01.>.

fervation.

7. Tbe fuo's magoelie azjmUlh i. the areh of the he>–

riz.on

intereepterl betwe.:n the

ma~netic

meridian aod th:

venieal,

pdJing

through the

(un .

S. Ha\'iog the la,i,ude of ,he place of obfer.alioo, 10-

gether

wirh

tbe

fur,'s

declinatioo

and

altitude

at

the time

of obrervat ioo, we m..

y

lind

his üue:lz. mUlh after the..

foll owing method,

t:iz.

I\

r.ke

il,

As

lhe

ungent

of halr

t~le

cOl1lplement of the htitude

¡J

to the

[angen{

of hCllf lhe

fUIn

of (he dinanee of the fUD

from the pol e aod eompl. meo, of ,he alli,ude

So is the (angent of h:.df th e diffc:renee bc:tween rhe

~i­

Ilaoee of Ihe fun from the poie aod eomplemeot of tb,.

altitude

T o

the tangent

of a

fou

rth areh

whieh founh areh added 'o half the eomplement of Ihe

la,i,u:!e \ViII gi ve a 6f.h ",eh, and this 61,h areh lelfeoed

by

,he

eomplemeot of Ihe lati,ud" will give o

fix.,h

areb.

Then

make it

As

th e radius

is

to

the tangent of the alrilude

fo is the tangcnt

oC

(he

GXlh ..

arch

to.the

eo fine

of the (unJs

azimuth

which is to be

counted

from

the

fout h

or

nonh, to the:

eiR

or weet .

aeeording

as

the

fUD

is

fi,uated

with rcfpeél: to the

pl.ce

of obfervatioo.

If Ihe latilude of ,he place aod decli .",ion of ,be fUTl

be both north or both romh , then [he

declioation

taken

fro01

90~

will give the fuo 's d:ll.oee from the pole; but

if the latitude aod dec1ioa.toion be on contrary lides of

the equator,

then

the

declinadon added

te

90°

",iJl

mvc

the fuo ', di!lanee from Ibe nearell pole to ,he pl..

e~

of

obrervation.

EXA""PLE.

In the Jatitllde of 51'-' 32 oorrh, rhe fun

having 19() 39'

north

declination,

his

altilude

was fOllod

by obfer. a,ion tO be 38° 'IS: Reguired Ihe azimulh.

By Ihe firll of Ihe foregoi ng aoologie., i, will

be

As the tangeot

of

i

the eom·

?

'

plemement of the Jatitude

5

19°. 14 9 '54

2

69

from lhe pole and eomple

61 ..

01 10.25

6 55

;, 'o the ' ageot of

t

the fum

~

of the diU . nee of ,he fuo

meot of (he ahitude -

fo i, the tangeol of

h.lf

their

differeoee

__

9 .. 19 7. 21 199

to ,he tango of a 41h areh

40 .. 20 9 ' 92S8,-

\Vhieh fou rth areh 40° 20', .dded 10 19° 14' half tbe

eomplemeol of ,he latitud., give o fiflh areh 59

0

34';

and this fif,h areh I.lfcoed by '3So

2S',

,he eomplemen,

of the lalilude, gives the Iixtb ",eh

H

o

06'; ,beñ for

the