280 109 9MB
English Pages [346] Year 1918
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New York State College of Agriculture
At Cornell University Ithaca,
N. Y.
Library
QC
873.866""""'"""'""'"^
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3 1924 002 999 831
[based
Cornell University Library
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original of
tiiis
book
is in
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?mwi
OF
OEPT. OF yEIEOEOLBeY
SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME
69.
NUMBER
1
SMITHSONIAN
METEOROLOGICAL TABLES [based on guyot's meteorological
and physical tables]
FOURTH REVISED EDITION (Corrected to January, 1918)
^
s\n
which B„
in
is
all
£)
With
B.
g g the correction
In general, sufficient accuracy will be attained correction for a station once for
—
is
+ C = 0.002640 cos 24> — 0.000007 cos^ 20 + ife
0.000045
R = r]
=
6367324 meters. (A. R. Clarke: Geodesy,
=0.002396.
R
8°,
Oxford, 1880.)
(Ferrel: Report Chief Signal Officer,
1885, pt. 2,
pp. 17 and 393.) TABLES
S1
,
S2, 53, 64, 66.
THE DETERMINATION OF HEIGHTS BY THE BAROMETER. Tables 51 52, 53, 54, 55. ,
English Measures.
Since a barometric determination of the height will rarely be made at a place where gi is known, the discussion which follows will be confined to the second form of the barometric formula developed in the preceding section (see
page xxxix). For convenience form
in
computing heights
it is
arranged
in the following
Z = KilogBo-logB)
+ ad) + (l + kcOS2 Z + 2h 1 + R
(i (i
1 s
ff)
k'
COS^2+C)
(l
Comptes Rendus, Quatrieme Conference Generale Poids et Mesures, 1907, ^ Lehrbuch der Meteorologie, dritte Auflage, Leduc I.e.
+ v)
pp. 60-61. 191S.
s.
5.
INTRODUCTION.
xlii in
which
K
B^ —
(log
log
B)
is
an approximate value of Z and the factors depending respectively on the air
in the brackets are correction factors
temperature, the humidity, the variation of gravity with latitude, the its effect on the weight of mercury in
variation of gravity with altitude in
the barometer, and the variation of gravity with altitude in its effect on the weight of the air. With the constants already given, the formula becomes
measures:
in English
Z (feet)
= 60368
1
(log J5o-log5)
"[1+0.002039
-
{e
32°)]
(I+/3) (l
+ 0.002640 cos 2 — 0.000007 COS^ 2 + 0.000045) (l + 0.00239)
+ 0.000007 co^' 2
its
acceleration at
Table 84.
RELATIVE ACCELERATION OF CRAVtTY AT DIFFERENT LATITUDES. Ratio of the acceleration of gravity at sea level for each lo' of latitude, to latitude 45°.
.
its
acceleration at
Table 85.
LENGTH OF ONt DEGREE OF THE MERIDIAN AT DIFFERENT LATITUDES.
Latitude.
Table 86.
LENGTH OF ONE DEGREE OF THE PARALLEL- AT DIFFERENT LATITUDES.
Table 87.
DURATION OF SUNSHINE AT DIFFERENT LATITUDES.
Declination of tlie
Sun.
Table 87.
DURATION OF SUNSHINE AT DIFFERENT LATITUDES.
Declination of tlie
Sun.
Table 87.
DURATION OF SUNSHINE AT DIFFERENT LATITUDES.
Declination of tlie
Sun.
Table 87.
DURATION OF SUNSHINE AT DIFFERENT LATITUDES.
Declination of
ihe Sun.
Table 87.
DURATION OF SUNSHINE AT DIFFERENT LATITUDES.
Declination of
the Sun.
Table 87.
DURATION OF SUNSHINE AT DIFFERENT LATITUDES.
Declination of llie
Sun.
Table 87.
DURATION OF SUNSHINE AT DIFFERENT LATITUDES.
Declination of tlie
Sun.
Table 87.
DURATION OF SUNSHINE AT DIFFERENT LATITUDES.
Declination of the Sun.
Table 87.
DURATION OF SUNSHINE AT DIFFERENT LATITUDES. LATITUDE NORTH.
Declination of
the Sun.
60° h.
-8
0'
62°
61°
m.
h.
m.
10 40
1037
20
1045 1050
10 42
20 O
40 20
O
-3 -3 -3 -2 —2
1047
1055 1059 11 4
1052 1056
II 8 II 13
II 6 II II II 16
II
18
11
I
70°
9 43
936
928
919
950
9 43
927
3 9
9 57 10 4
950
9 35 9 43
9 57
950
10 15 10 22 10 28
10 10 10 i5
1023
10 4 10 II 10 18
9 57 10 5 10 12
1034
10 29
1025
1047 1053
1038 1044 1050
10 40 10 46
1036
10 31
10 19 10 26
10 42
1038
1034
10 14 10 21 10 29
10 49
I
1052 1058
10 41 10 48
1036 1044
7
11
11
I
1045 1052 1058
1055
10 51
11 5 II II II 18
11 2 II 9 II 16
1059
1025 10 31
10 20 10 26
10 40
1036
1032
1045 1050 1056
10 41
033 038 043 049 054 059
69^
h. jn.
1034
1032
10 13 10 18
68°
m.
h,
10 29
103s
40
m.
023 028 1023
o 17
7
67°
950 956
h.
10 2 10 8 10 14
10 22 10 27
6
m.
10 8 10 13 10 19
10 26 10 31
20 o
10
956
ID 12
"7 -7
h.
66°
65°
64°
2
10 17
40
O
m.
h.
10 21
7
40
63°
10
10 10
I
1058
1055
I
9
I
14
II 7 II 12
11 4 II 10
11 II
II 17 II 22 II 28
II 15
II 13
II 10
II
20 II 26
II 19 II 24
II 16 II 22
II 8 II 14 II 20
30 36
II 28 II 34 II 40
II 27 II 33 II 40
11 25 II 32 II 38
II 23 II 30 II 37
II 21 II 28 II 35
II 46 II 52 11 58
II 45 II 52 11 58
II 44 II 51 11 58
II 43 II 50 11 58
12 5 12 12
12 5 12 12
1225
12 19 la 26
12 19 12 27
4
1055
II 21 II 26 II 31
I
19
II 27 II 32
I
24 29
—2 —
II 37 II 41 II 46
II 35 II 40 II 45
134 II 33 139 1138 144 II 43
II 31 II 37 II 43
II
20 O
I
40
II
—
II 50
I
20
II 55 11 59
1155
II
54 11 59
II 48 II 53 11 59
II 47 II 53
11 59
149 154 159
II 49
11 59
II 45 II 52 11 58
40
12 12
2 2
4 9
12 4 12 10
12 4 12 10
12 4 12 10
12 4 12 10
12 4 12 II
12
20
12 12
— -0 —O I
O
4 9
4 9
6
11
II 22
50
10
4
20
40
951 958
I
40 o
9 35 9 43
1
II
II 41
5
12. II
11 6 II 13
12 13 12 18 12 22
12 14 12 19 12 23
2 14 2 19 2 24'
12 15 12 20 12 25
12 15 12 20 12 26
12 16 12 22 12 27
12 16 12 22 12 28
12 17 12 23 12 29
12 18
12 31
12 33
1234
12 27 12 32
12 28
2 29
12 32
12 36 12 42
1238 1244 1251
12 41
234 239
1233 1234 1239 12 40 1244 12 46
12 40
1233 1238
1231 1236
1247 1254
1249 1256
12 41 12 46 12 50
1243 1247
13 I 13 8 13 15
13 4 13 II 13 19
1255
1257
244 12 46 12 48 1250 12 52 1255 1258 249 1252 1253 12 56 1259 13 I 13 4 254 1257 1259 13 2 13 5 13 7 13 II 259 13 2 13 5 13 8 13 II 13 14 13 17
20 40
o 13 4
13 13
20 40
-fO 20 o 40 20 40 20
40
20
40 20
40
1237
12 52
12 41
1237 1243
1249
13 22
13 25
1327
1329 1336
1334
1323
13 24 13 31
13 31
1329 1335 13 41
1343 1350 1358
1349 1356
1337
1335 1338 1340 1345 1345 1352
13 27
330 1334 1338 1343 1347 1353 1358
1332 1337
3 35
14 5 14 12 14 19
14 II 14 19
1342 1347 1352
346 1350 1355 351 1356 14 I 356 14 I 14 7
14 14 7 14 13
14 6 14 12 14 18
14 26
1435 1443
14 19
1425
1424
14 31
13 10 13 16
13 13 13 19
13 17
13 20
3 10
13 7 13 13
13 12 13 17 13 22
315
13 18
1325
20
1323
13 22 13 27
3 25
13 29
1332
13 23
1328 1333
2
3
7
13 9 13 14 13 19
13
1338 1343 1347
3
5
341
1340 1344 1349 1354 1359 1345 1350 1355 14 o 14 6 I
7
7 4 12
14 7 14 13 14 18
14 12 14 18
14 12
417
1423
1430 1437
1352 1357
1357
4
20
2
4
40
14
2
14 14
14
7
I
Smithsonian Tables.
211
1425
14 5 14 12
13 41
14
4
1427
14 13 14 19 14 26
14 19 14 26
1432 14 31 1439 1438 1446
1440 1448 1455
1449 1457 4
15 7 15 15
2
15 12
^523
1445
1452
1433
15
1434 1442
15
14 51
1459
Table 87.
DURATION OF SONSHINE AT DIFFERENT LATITUDES.
Declination of tlie
Sun.
Table 87.
DURATION OF SUNSHINE AT DIFFERENT LATITUDES. I,ATITUDE NORTH. Declination of
the Sun.
60°
h.
+
m,
0' 8 20 8 40
9
4 22
9 20 9 40
427 432
10 10 20 10 40
4 37
11
8°
II 11
h.
m.
62°
b.
m.
m.
428
4 35
427 432 438
4 34 4 39 4 45
450 456
4 47
4 43 4 49 4 54
452
4 59
4 57
5
5 7 5 13
5
5
2
519 525
12 12 20 12 40
5
8
518
516 521 527
13 13 20 13 40
5 23 5 29
5 33 5 39
14 14 20 14 40
540 546 551
15 15 20 15 40
5 57 6 2
6 8 6 14
8
6 20
16 16 20 16 40
6 14 6 20
17 17 20 17 40
632 638 645 651 658
626 632 639 645 652 658 7 5 7 12 7 19
7 20 7 28
26 7 33
5 13
5 35
6
626
7
4
531
536 542 548
458
15 6 15 13 15 19
5 15 5 22
528
1525 1532 1539
1535 1543 1550
516 1525
5 35
1546
1558 16 5 16 13
5 4 5 10 5 22
5
9
1531
541
15 53
528 1538
548
16
1544 540 1550 546 1557
5 55 6 2
16 7 16 15 16 22
5 34
6
9
625
1638
6 19
632 16 46 639 1653 646 17 I
7 I 7 9 7 17
639 646 652
653
725
659
750
6
7 22
1739
7
729 1747 7 37 1756
8
7
o
7
7
17 8 17 16 17 23
714
17 31
631
7 33
741 59 8
b.
m.
15 2 15 10 15 17
1525 1532 1540 1547 1555 16
3
i5 II 16 19 16 27
69°
h.
m.
15 12 15 20
1528 1536 15 44
1634 1643
17
1652
17 20
17 41
1730 1740
18
17 29
1750
18 14
1738 1748
18 o 18 II
1826 1838
1737 1758 1746 18 8 1735 1755 18 18 1744 18 5 1829 1753 18 15 18 40 18 2 1825 18 51
1822 1833 1845
19 3 19 16
1923
20
1835 1846 1857
19 3 19 15
1936 1950
20 17
19 41
1645
17
I
17 10 17 19 17 28
17 17 17 26
18 II 18 21
1831
1857 19 10
1928 20 6
9
18 51 19 I 19 12
919 1950 20 30 21 23 2259 930 20 4 2047 2447 942 20 19 21 5 22 17
21 21 20 21 40
752
8 II
o
8 20
22
S16
22 20 22 40
8 24
856 1923
828
832 841 850
837 846 855
9 o 9 10 9 20
927 1958 2037 938 20 II 2053 950 2025 21 II
9 4 9 13
931 20 941 20 946 20
9 6 9 16
1937
20 14
2
20 40
2056 21
2
MITHSONIAN Tables.
213
21 31 21 54 22 3
21 29 21 52 22 21
23
3
23
2
17 II 17 21 17 31
1752 3
1850
1930 1945 I
2035 2055
1955
20 22 20 40
20 10
2059
21 17 21 42 22 13
20 26
21 20
2258
2044 2145 21
925 2034 21 26 23 1934 20 8 2050 21 50 1946 20 22 21 8 22 19
14 19
I
17 2 17 10 17 19
18 41
815 823
1652
17 I 17 II
1637
8 10 8 19
738
1633
1635 1644 1653
16 21 i5 29
751
20 20 20 40
6
16 42
1823 1832
7
1549 1557
16 26
8
828 837 846
1532 1540
16
7 43
7
m.
16 15 16 24
7 35
7 59
h.
15 23
16 o i5 8 16 17
817 1841 19 8 826 1852 19 20 836 19 3 1933 846 19 14 1946 856 1925 20 o
2
70°
1552
18 5 18 14
8
917
1528
68°
7 45 7 53
748 756 4
7
638 1653 646 17 I 653 17 9
6 19
8
o
616 1630 1645 623 1637 1653
7
7
o
15 15
16 4 16 II 16 17
6
741
832 841 849 852
15 14 15 21
2
613
24
8
15 5 15 II 15 18
5
6
7 13
m.
456
16 24 16 31
7
h.
441 1448 446 1454 452 15 o
1442
6 12
626 632
m.
1453
I
2
h.
67°
1445 1452 450 1458
6
731 45
m.
66°
4 37 4 43
5 55
20
7
b.
544 550 556
7 II 7 17 7
65°
5 53 5 59 6 5
19 19 20 19 40
20 27
h.
4 22
5 10
23 23
m.
41^
4 12
417
2
23
h.
64°
423 1430 429 1436
4 12
5
18 iS 20 iS 40
63°
417 423
4 7
442
20 40
61°
3
I
22 16
Table 87.
•
DURATION OF SUNSHINE AT DIFFERENT LATITUDES.
Declination of
the Sun.
Table 88.
DECLINATION OF THE SUN FOR THE YEAR 1899.
Table 89.
DURATION OF ASTRONOMICAL TWILIGHT. (Interval between sunrise or sunset
and the time when the true position
of the sun's center is i8°
below the horizon.)
NORTH LATITUDE. Date.
0°
Jan.
Feb.
h.
m.
I
I
14
II 21
I
14
I
I
13
I
12 II I 10
May
June
July
m,
I
I
12 12
I
I
m.
li.
m.
h.
m.
h.
m
h,
m,
h.
m.
I
II
I
I
I
IS I 18 I 22 I 24 I 26 I 28 I 3° I 33 I 17 I 21 I 23 I 25 I 27 I 29 I 32 I 24 I 26 I 28 I 31 13 I 16 I 20
h.
m,
I
41 39 38
I
I
II I 14 I 17 II I IS I 18 12 I 16 I 20
I
I
09
I
I
10
I
I
II
I
I
I
II 21
I I
12I1 13 13 I 14 13I1 IS
I
I
14]
16
I
II 21
I
iS|i 17 IS
I
I
I
I
I
II 21
I I
I I
23 I 25 I 27 I 30 I 33 I 27 I 30 I 33 I 36
I
32
39
I
24
I
24 27
I
29
I
I
36
I
I
27
I
3°
I
33
I
36
I
43
I
I
30
I
33
I
I
40
I
48
1
I
I
32
I
36
I
36 39
I
43
I
S4 2
23
I
28
I
41
I
I
I
I
44
I
I
I
29 29
38 40
I
I
iS 36 37
I
24 24
I
41
I
45
I
46 49 50
17 16
I
24
I
29
I
I
I
44 41
I
I
40 38
I
23 I 28 21 I 26
I
36 3S 32
I
I
I
36
I
39
I
19 iS 16
I
14
IS 14 13
I
I
IS
I
13 12
I
14
I
13 I 12
I
Sept. I II 21
I
I
10 09 09
Oct. I
I
09
I
II
I
I
I
I
I
I I
21.
I
II I
I
43
I
53
2
00
39 37
I
48 44
I
I
I
49
I
I
41
I
45
I
54 5°
33 33 33
I
36 36 36
I
39 39
I
48
I
43 43
I
I I
40
I
44
138
I
49
40
I
I
52
I
42
I
I
46 47 49
I
I
41 43 46
I
I
55
44 45 45
I
47 49 49
I
52
I
I
53 54
I
57 59 59
I
30
I
I
I
22
I
24
I
27
I
3°
I
33
I
I I
I
21 22
I
I I I
28 28 28
3° 30
I
I
I
I
I
40
I
I
41 41
I
12 12 I 12
I
13
I
13
I
I
I
14
I
21
I
II 21
I
I
14 14 15
I
15 16
22 22
I
I
I
IS
I
I
19
I
I I
26
I
I
27 28 28
I
I
33
I
I
31 32
I
32
I
34 iS
I
I
I
29
I
I
36 30
I
Smithsonian Tables.
215
I
I
34 36 38
I I
I
I
I
I
25 26
I
31
II 21
I
I
12 2 23 2 40 2 18 2 31
I
27 I 29 I 32 23 25 17 I 24 I 26 I 28 I 30 I 33 18 I 20 I 24 I 26 I 28 I 30 I 32 I 35 I
I
I
I
I
2
I
27
I
01 2 10 2 20 lo 2 20 2 35 20 2 35 2 58
39 36 34
I
36
II I
2
02
I
I
2
54 01 2 10
I
20
I
1
2
2
I
I
54
54
44 39 36
20
2
1
48 43
I
I
48 54 01
I
1 54 54 2 00 01 2 08
I
I
36 33
25 25 26
49
1
I
40
I
I
10
I
I
44
2
I
23 23 24
43 48
48 48 50
01
36 ii
I
40
I
2
I
I
I
I
I
I
I
21 21 22
36 39 43
I
I
48
33 30
I
I
43 43 45
I
I
I
I
I
I
39 39 41
I
07
I
19 19
I
36 36 37
I
2
27 24
I
I
I
2
30
I
40
49 48
I
59 54
I
16 16 16
52
I
I
I
02
I
I
I
I
47 45 44
I
I
24 22
I
I
39 37 36
2
13 I 17 I 21 I 23 I 25 I 27 I 30 I 33 I 13 I 16 I 20 I 22 I 24 I 26 I 29 I 31
13 13 13
43 41
I
I
59 57 54
55 52
I
I
I
I
h,
I
49 46 43
I
49
I
I
49 47 45
52 1 59 2 07 2 18 2 31 2 54 55 2 02 2 12 2 23 2 40 3 II 56 2 03 2 13 2 25 2 44 3 19
I
10 10
I
22 24 26
I
I
I
I
I
I
41
I
II 21
I
I
I
I
I
m,
S3 52
I
33
I
I
m.
h.
h.
I
II I 13 I 16 I 20 I 21 I 23 I 25 I 28 I 30 I 33 I 09 I 10 I 13 I 16 I 19 I 21 I 23 I 25 I 28 I 30 I 33 I og I 10 I 13 I 16 I 20 I 22 I 24 I 26 I 29 I 31 I 34
lO
14
50
I
m.
45 43
h.
I
I
I
Dec.
h.
18. I
36 34
I
I
Nov.
m.
21 I 26 I 28 I 29 I 31 I 34 I 37 I I I 21 I 2S I 27 I 29 I 31 I 33 I 36 I 17 I 20 I 23 I 2S I 28 I 30 I 32 I 34 I
II 21
Aug.
h.
h.
IS 14 13
I
II 21
Apr.
h.
I
II 21
I
Mar.
10° 20° 25° 30° 32° 34° 36° 38° 40° 42° 44° 46° 48°
36 37 38
I
I
I
I
2 10 2 20 2 35 54 2 01 2 10 2 20 48 I 54 2 01 2 09
I I
I
I
I
Table 90.
DURATION OF CIVIL TWILIGHT. (Interval between sunrise or sunset is
and the time when the true position of the sun's center 6° below the horizon.) [Minutes.]
Table 91
RELATIVE INTENSITY OF SOLAR RADIATION, A/lean
Date.
intensity / for 24 liours of solar radiation on a liorizontal surface at the top of tlie atmospliere and tlie solar constant ^, in terms of tKe mean solar constant ^o.
Table 92.
RELATIVE AMOUNTS OF SOLAR RADIATION RECEIVED ON A HORIZONTAL SURFACE DURING THE YEAR AT DIFFERENT LATITUDES,
MISCELLANEOUS TABLES.
Weight
in grams of a cubic centimeter of air:
English measures
— Temperature term Humidity term;
auxiliary table
.
.
Table
95
Table
96
Table
97
Table
98
Table
99
Humidity and pressure terms, combined
Metric measures
—
Temperature term
Humidity term; auxiliary
table
.
.
Humidity and pressure terms, com-
Table 100
bined
Atmospheric water-vapor
lines in the visible
Atmospheric water-vapor bands
spectrum
in the infra-red
.
.
spectrum
Transmission percentages of radiation through moist
air
.
.
.
.
Table
10 i
Table
102
Table
103
International Meteorological Symbols
Table 104
International Cloud Classification
Table
Beaufort Weather Notation
Table 106
List of meteorological stations
Table
105
107
Table 95.
WEIGHT
IN
CRAMS OF ONE CUBIC CENTIMETER OF
Temperature term:
Jj
= I
I
AIR.
0.00129305 Fahrenheit temperatures. {t —32°)'
+0.0020389
cubic centimeter of dry air at the temperature 32° F.
and pressure 760 mm., under the
standard value of gravity and sea-level, weighs 0.00129305 gram.
Temperature.
Table 96.
WEIGHT
IN
GRAMS OF ONE CUBIC CENTIMETER OF
Humidity term: Values e
= Vapor pressure
in inches.
of
0378
e.
Auxiliary to Table 97. (See Tables 69
Temperature by normal hydrogen thermometer.
DewPoint.
AIR.
and
70.)
Table 97.
WEIGHT
IN
CRAMS OF ONE CUBIC CENTIMETER OF
Humidity and pressure terms combined:
r5,,
B= h.
Barometric pressure in inches; e
=
= 29.921
= Vapor
AIR.
——
29.921
pressure in inches.
WEIGHT
IN
TT
.jv and J . I.J Humidity pressure terms combined:
* r-
So
B= h.
Table 97. AIR.
CRAMS OF ONE CUBIC CENTIMETER OF
Barometric pressure in inches;
e
^
=
= Vapor
—
= 5-o.378e =
29.921
29.921
pressure in inches.
Table 98.
WEIGHT
IN
CRAMS OF ONE CUBIC CENTIMETER OF
Temperature term: I
5;
^^^
=
—
^-
^~1-
AIR.
Centigrade temperature.
cubic centimeter of dry air at the temperature o° C. and pressure 760 mm., under the standard value of gravity and sea-level, weighs 0.00129305 gram.
t.
WEIGHT
IN
GRAMS OF ONE CUBIC CENTIMETER OF Temperature term. {Continued.)
\.
Table 98. AIR.
Table 100.
WEIGHT
IN
CRAMS OF ONE CUBIC CENTIMETER OF
Humidity and pressure terms combined
:
—"= '
h
5—0.378,?
760
760
B^ Barometric pressure in mm. ^= Vapor pressure in mm. ;
h.
AIR.
Table 100,
WEIGHT
IN
CRAMS OF ONE CUBIC CENTIMETER OF AIR. S h =B — 0.378^
Humidity and pressure terms combined
B^ Barometric pressure in mm. h.
mm.
;
^
:
— = -7-
-j
= Vapor pressure in mm.
Table 100.
WEIGHT
IN
GRAMS OF ONE CUBIC CENTIMETER OF
AIR.
Table
ATMOSPHERIC WATER-VAPOR LINES Wave
lengths
Angstroms.
in
5292 3-5296.0 5861.8-5870.0. 5870.864.
5871.3-58760
Number of
Wave
Intensity.
.
4?
.
.
7
CO CO I
.
CO
...
5876.338 5876.6-5879.4 ... 5879.820.. 5879.945 5S80. 7-588 CO ... 5881.147. 5881.320. 5882.084 5882.2-58832.... 5884 120. 58S4. 4-5885. 8 5886.193.. 5886.560 5886.6-5886.9 ... 5887.445 5887,880 5888.056.
I
.
00 1 I
.
5920395
I
5920.776 5921.3-5922.6 5922.735 5922.9-5923.4
I
.
o
.
2
5932998
I
5933.2-5940.2 5940.640 5941.091 5941.290 5941.470 5941.845 5942.500 5942.635 5942 789 5944.5305944-945
.
2
5945.4-59-15 5
.
00
3 2
00 I
o 4
5891878..
3
.
o I
o
5896710
.
5897.047 5897.3-5898-2 589S.378. 5898.6-5899.0 ... 5899-215 5899.752.. •
4 00 2
00 2
5900 135.. 5900.260 5900 6-5901.5 5901.682. 5902.238 5902.363 5903 035 5903 748 5903-9-590" -7 5908 070 5908.425
4
CO 6 000
.
I
000
.
t
.
13
5909 668
00 I I
5909213
3
00
.
I
5,910.398
5910.5-5910.9 5910.987 5911.1-5912.9... 59r3.2i2 5914 430
00 2
00 ,
7
00 I
o 2
3
6
4 coo 2
000 2
CO
5892.608 5893.268 5893.725 5894.6-5896.6
5
00
5889.303..
•
.
5928510
5888920..
.
.
I
5929.0-5931.2. 5932.306
5890.100 5890.4-5890.9 5891 398 5891.720..
I
00 4 000
2
00
5889855..
I
592.3.865
5 3
.
sity.
line".
5924.040 5924.490 5924.975 5925.220 5926.835
o
.
Inten-
5
I
•
ber of
00 5
.
01
I
5915.146 5915 650 59'5 840 5916.0-5918.2. 5918.635. 5919.175 5919 276 5919.860
o o
Num-
lengths
in Angstroms.
lines.
.
IN
1
THE VISIBLE SPECTRUM.
5 2
14
I
00 5
000 2
oco I
3 I
I
00
5945.865 5946.223..... 5946-864 5947-062 5947.283 5947-6-5949-2 5949.390 5949.8-5954.6 5955.170 5956.0-5956.6 5958.098 5958.460 5961.6-5966 6 5966.885 5967-540 5968.058 5968.280 5968.495 5969.2-5970.9 5971 557 5975 33°. 5976.694 5977.252 5977.6-6479.7 .
229
000
I
3
000 I
2
000 2
00 I
000 I I
00 I
00 2
000
,
2
00 I I
•
00 I
73
000
Table 101.
ATMOSPHERIC WATER-VAPOR LINES Wave in
lengths
Angstroms.
6480.285.. 6480.4-64S3.3 6483.468.. 6483.6-6490 9. 6491 015.. .
.
.
.
6493.1-64935....
Number of
THE VISIBLE SPECTRUM.
Wave
Intensity.
in
lines.
Num-
lengths
ber of
Angstroms.
lines.
Intensity.
000
I
6941. 260. 6941 475- •• 6942. 402. . 6942, 630. 6944. 060..
00
6947 ,782...
5
6947. 863. 6949 240. 6949 310... 6951 010. 6953 828.
00
6954.0-6955 9 6956 660 \. 6956 746/.
00 4
6959' 704. 6961, .515- • 6964, 812...
3
6971, 135.--
o
6977 .715.
3
.
I
4
0000 I
II 2
I
2 I
.
000
3
.
6494.725.-
I
6496 082 6497.8-6514.5.... 6514.956.. 6516 oSo 6516.750.. 6516.855.. 65I7-3-65I9-4 6519.682. 6522.1-6523.9 6524.080 6526.0-6530 8 6532 595. 6534.172.. 6534.8-6542.6 6544.140.. 6546.0-6547.9. .. 6548.855
I
.
2
00
I I
.
2
I
.
000
.
I
2
00
I
.
I
ooco I
.
000 I
2
000
.
I
6552865.. 6554 025
00? I
I?
00 I
o
7011, 7016, 7016, 7023, 7027, 7027,
000 2
-
I
6985 .220..
3
o 3 I
2 I
o 2
o 2
o
7005.3-7010
I
.
.
6981 ,722..
6998. 978.. 6999. 223... 7004, 575 •• • 7004, 995- ••
O
.
I
6990 632... 6993 776... 6994 360...
I
6556.30S.. 6557-4-6558 4..-. 6560 800. 6563-7-6569.0 6572.330,. 6575-085 65S0. 4-6929. 6. 6934-075 6937 9576938.520.. 6939 875 6940.436..
4
6986, 833. • 125... 6989 ,237...
2
00
.
.
IN
2 I
2
590-. 330675-. 770.. 213.. 740..
I
3 2
o 2
Table 102.
ATMOSPHERIC WATER-VAPOR BANDS
IN
THE INFRA-RED SPECTRUM.
The infra-red ban-^s may perhaps be composed
Name of band.
Wave- Transmislengths,
sion coefficient a.
numerous fine lines which the holographic apparatus does not separately distinguish. Wide bands of very great atmospheric watervapor absorption are found in the infra-red spectrum as follows of
:
0,718 0.814 P
Ixiii,
xx> 5°
arc into into arc
19s
xx, 51 xxu, 57 xxii, 58
mean, at apparent noon Radiation, solar, relative intensity of, for 24 hours at top of atmosphere Ixvii, 217 Ixviii, 218 during year at surface of the earth transmission percentages of, through moist air, Ixxi, 231 Rainfall, conversion of depth of, into gallons and tons Ixiii, 195 Reaumur, conversion to Approximate Absolute, Cenxii, 2-4 tigrade and Fahrenheit Reduction, of barometer to xxxiv-xxxviii, 129standard gravity xxx-xxxiv, 86standard temperature of psychrometric observations, Ivii-lx, 172English Ivii-lxi, 186 Metric Ixii, 194of snowfall measurements xxxii, li, lii, Regnault, treatise cited Rehtive humidity, Ix, 183-: English Metric Ixi, 192Relative intensity of solar radiation. .Ixvii-lxviii, 217Rode, Danish, value of XXV Rotch, A. L., work cited
Rowland, work cited Rubens and Aschinass, treatise cited Ruthe, Prussian, value of Norwegian, value of
Ixxi
48
comparison of Approximate Absolute, Centi-
grade, Fahrenheit,
xxii,
...
58 48
through moist -Ixxi,
air
231
Ixvh, 215
Twilight, duration of astronomical duration of civil
bivii,
216
Vapor, aqueous, pressure of,
English Metric pressure
160-164 165-168
lii-lv,
.lii-lv,
by psychrometric
observations,
English
Ix,
172-182 186-191
Iv-lvii,
169-170
lix,
Metric
;
pressure decrease with altitude, for mountain stations specific gravity
weight of Vara, values of,
Ixi,
48 48 48 229-230
Mexican Spanish Versta or Werst, value of Visible spectrum, water vapor lines in ._
194
Iv-lvi
_
Ixxi,
231
Sagene, Russian, value of Scales,
mean solar into sidereal sidereal into mean solar ToisS, value of Transmission percentages of radiation
and Reaumur
xii-xiii,
2-4
Sea-level,
reduction of temperature to, English
Metric Seconds, conversion of decimals of a day into into arc into decimals of a day into decimals of an hour reduction for, sidereal or solar time Sidereal time, conversion to mean solar Simpson, Dr. G. C, work cited Sky, relative illumination intensity, at sunset at end of civil twilight Snowfall, weight corresponding to depth of water Ixii,
XXX, 82 xxx, 83 xxi, 56 xx, 51 xxi, 56 xxi, 57 xxii, xxii,
58 58
xxv 218 218
194-igs
liii Waals, J. D. van der, work cited Water, vapor of (see Aqueous) Ixxii, 236 Weather, state of, Beaufort symbols for Weight, of saturated aqueous vapor. Iv-lvii, 169 Cubic foot .Iv-lvii, 170 Cubic meter in grams, of a cubic centimeter of air, Ixix-lxx, 220-223 English Ixix-lxx, 224-228 Metric 48 Werst or versta, value of xxiv-xxix, 64-79 Wind tables Wind, mean direction by Lambert's formula xxv-xxvii, 71-76 true direction and velocity at sea, determina-
xxv tion of xxvii-xxix, 77-79 gradient, velocity of radius of critical curvature, .xxvii-xxix, 77-7Q xxiv-xxv, 70 scale, Beaufort's xxiv, 64 synoptic conversion of velocities .
Year, days into decimals tropical, length of
of,
and angle
xx, 52-s5_ xxii
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