A "Rise," with dry air, and cold increasing in summer, indicates wind from northward; and if rain has fallen, better weather is to be expected. A "Rise," with moist air and a low temperature, indicates wind and rain from northward. A "Rise," with southerly wind, indicates fine weather. A STEADY BAROMETER, With dry air and a seasonable temperature, indicates a continuance of very fine weather. A FALLING BAROMETER. A "Rapid" fall indicates stormy weather. A "Rapid" fall, with westerly wind, indicates stormy weather from northward. A "Fall," with a northerly wind, indicates storm, with rain and hail in summer, and snow in winter. A "Fall," with increased moisture in the air, and the heat increasing, indicates wind and rain from southward. A "Fall," with dry air, and cold increasing (in winter), indicates snow. A "Fall," after very calm and warm weather, indicates rain with squally weather. =27. Causes which may bring about a Fall or a Rise in the Barometer.=[3]--As heat produces rarefaction, a sudden rise of temperature in a distant quarter may affect the weight of the atmosphere over our heads, by producing an aerial current outwards, to supply the place of the lighter air which has moved from its former position; in which case the barometer will fall. Now such a movement in the atmosphere is likely to bring about an intermixture of currents of air of different temperatures, and from this intermixture rain is likely to result. On the other hand, as cold produces condensation, any sudden fall of temperature causes the column of air over the locality to contract and sink to a lower level, whilst other air rushes in from above to supply the void; and, accordingly, the barometer rises. Should this air, as often happens, proceed from the north, it will contain in general but little moisture; and hence, on reaching a warmer latitude, will take up the vapour of the air, so that dry weather will result. It is generally observed, that wind causes a fall in the instrument; and, indeed, in those greater movements of the atmosphere which we denominate storms or hurricanes, the depression is so considerable as to forewarn the navigator of his impending danger. It is evident, that a draught of air in any direction must diminish the weight of the column overhead, and consequently cause the mercury in the barometer to sink. The connection, therefore, of a sinking of the barometric column with rain is frequently owing to the wind causing an intermixture of the aerial currents which, by their motion, diminish the weight of the atmosphere over our heads; whilst a steady rise in the column indicates the absence of any great atmospheric changes in the neighbourhood, and a general exemption from those causes which are apt to bring about a precipitation of vapour.