[12]. The Aneroid Barometer: How to Buy and How to Use it. By a Fellow of the Meteorological Society. Post free for six stamps, from any bookseller or optician.
The height of mountains may also be determined by the temperature at which water boils, as this depends on the pressure of the atmosphere, and according to Deschanel, “just as we can determine the boiling-point of water when the external pressure is given, so if the boiling-point be known we can determine the external pressure,” and as this varies with the elevation above sea-level, the boiling-point of water also varies.
These facts induced Wollaston to attempt the determination of heights of mountains by an apparatus which he called the Barometric Thermometer, subsequently modified by Regnault and called a Hypsometer, but now more generally known as a Boiling-point Thermometer.
33.
Boiling-point
Thermometer.
Scale about 1/3.
A portable form of boiling-point thermometer is shown at Fig. 33, which is much used by Alpine travellers, and forms a trustworthy check on the aneroid and barometer.
| Boiling-point of Water for pressure in next col. | Barometer at lower Station. | BAROMETER AT UPPER STATION.—INCHES. | |||||||||||||||
| In. | 30 | 29 | 28 | 27 | 26 | 25 | 24 | 23 | 22 | 21 | 20 | 19 | 18 | 17 | 16 | 15 | |
| 213·78 | 31 | 859 | 873 | 889 | 905 | 921 | 939 | 957 | 977 | 998 | 1020 | 1043 | 1068 | 1095 | 1124 | 1155 | 1188 |
| 212·13 | 30 | .... | 888 | 904 | 920 | 937 | 955 | 974 | 994 | 1015 | 1038 | 1062 | 1087 | 1115 | 1144 | 1176 | 1210 |
| 210·43 | 29 | .... | .... | 919 | 936 | 953 | 971 | 991 | 1012 | 1033 | 1056 | 1081 | 1107 | 1135 | 1165 | 1198 | 1233 |
| 208·67 | 28 | .... | .... | .... | 952 | 970 | 989 | 1009 | 1028 | 1051 | 1075 | 1100 | 1127 | 1156 | 1187 | 1220 | 1257 |
| 206·87 | 27 | Factor A. | 988 | 1007 | 1028 | 1050 | 1073 | 1097 | 1122 | 1150 | 1180 | 1211 | 1246 | 1283 | |||
| 205·01 | 26 | .... | .... | .... | .... | .... | 1027 | 1048 | 1070 | 1093 | 1118 | 1145 | 1173 | 1203 | 1236 | 1271 | 1309 |
| 203·09 | 25 | .... | .... | .... | .... | .... | .... | 1069 | 1092 | 1116 | 1141 | 1169 | 1198 | 1229 | 1262 | 1299 | 1338 |
| 201·11 | 24 | .... | .... | .... | .... | .... | .... | .... | 1115 | 1140 | 1166 | 1194 | 1224 | 1256 | 1290 | 1327 | 1367 |
| 199·05 | 23 | .... | .... | .... | .... | .... | .... | .... | .... | 1164 | 1191 | 1220 | 1251 | 1284 | 1319 | 1358 | 1399 |
| 196·92 | 22 | .... | .... | .... | .... | .... | .... | .... | .... | .... | 1218 | 1248 | 1280 | 1314 | 1350 | 1390 | 1433 |
| 194·71 | 21 | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | 1278 | 1310 | 1346 | 1383 | 1424 | 1469 |
| 192·41 | 20 | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | 1343 | 1380 | 1419 | 1461 | 1507 |
| 190·00 | 19 | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | 1416 | 1457 | 1500 | 1548 |
| 187·50 | 18 | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | Factor A | .... | 1497 | 1542 | 1592 | |
| 184·87 | 17 | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | 1588 | 1639 |
| 182·10 | 16 | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | .... | 1690 |
| 179·20 | 15 | ||||||||||||||||
| Height in 1,000 feet. | Factor D. additive. | Latitude. | Factor C. | Mean Temperature. | Factor B. |
| 2 | 5 | 0° | †2·7 | 10° | 0·951 |
| 4 | 11 | 10 | †2·5 | 20 | 0·973 |
| 6 | 17 | 20 | †2·0 | 30 | 0·996 |
| 8 | 23 | 30 | †1·4 | 40 | 1·018 |
| 10 | 30 | 40 | †0·6 | 50 | 1·040 |
| 12 | 37 | 45 | 0·0 | 60 | 1·062 |
| 14 | 44 | 50 | -0·5 | 70 | 1·084 |
| 16 | 52 | 60 | -1·3 | 80 | 1·127 |
| 18 | 60 | 70 | -2·0 |