Map climatic features as the long-term mean values (of atmospheric pressure, temperature, humidity, total precipitation, and so forth) to connect points with equal values of the feature in question—for example, isobars for pressure, isotherms for temperature, and isohyets for precipitation. Isoamplitudes are drawn on maps of amplitudes (for example, annual amplitudes of air temperature—that is, the differences between the mean temperatures of the warmest and coldest month). Isanomals are drawn on maps of anomalies (for example, deviations of the mean temperature of each place from the mean temperature of the entire latitudinal zone). Isolines of frequency are drawn on maps showing
Atmospheric railway by atmospheric pressure. The train consisted of ten carriages (including that to which the piston is attached) and its weight was upward of fifty tons. At seven and a half minutes past two the train left the point of rest at the Dartmouth Arms, and at eight and three-quarter minutes past, the piston entered the valve, when it immediately occurred to us that one striking advantage of the system was the gentle, the almost imperceptible, motion on starting. On quitting the station on locomotive lines we have frequently experienced a "jerk" amounting at times to an absolute "shock" and sufficient