Page 71 - James Rodger Fleming - Fixing the sky
P. 71

and winter storms, are driven by steam power. Heated by the Sun, a column of
                   moist air rises, allowing the surrounding air to rush in. As the heated air ascends,
                   it cools and its moisture condenses, releasing its latent heat (this is the “steam
                   power”)  and  producing  rain,  hail,  or  snow.  Espy  emphasized,  correctly,  the
                   importance of knowing the quantity of vapor in the air, “for it is from the latent
                   caloric [or heat] contained in the vapor that all the force of the wind in storms is
                   derived. It is only when the dew-point is high that there is sufficient steam power
                   in the air to produce a violent storm; for all storms are produced by steam power.”
                                                                                9
                   His theory was well received by many scientists of his time, including a commit-
                   tee of the French Academy of Sciences chaired by François Arago. The convective
                   theory is now an accepted part of meteorology, and for this discovery Espy is
                   well regarded in the history of science.
                     Espy  strayed  from  the  scientific  mainstream  when  he  promoted  his  idea
                   that significant rains of commercial importance for agriculture and navigation
                   could be generated by cutting and burning vast tracts of forest. He believed the
                   heat and smoke from these fires would create huge columns of hot air, produc-
                   ing clouds and triggering precipitation, much like the effects of volcanic erup-
                   tions. He listed five scientific reasons why setting large fires should produce rain:
                   (1)  experiments  showed  that  expanding  air  cools  dramatically,  and  (2)  under
                   certain conditions of high humidity forms both a visible cloud and significant
                   amounts of precipitation; (3) chemical principles indicated that the “caloric of
                   elasticity” (a venerable term for latent heat) released in the condensation of this
                   vapor is immense, equal to about 20,000 tons of anthracite coal burned on each
                   square mile of cloud extent. Espy’s convective theory further held that (4) this
                   release of heat would keep the cloud buoyant, lower the barometer, and “cause
                   the air to rush inward on all sides toward the center of the cloud and upward in
                   the middle, thus continuing the process of condensation of vapor, formation of
                                           10
                   cloud, and generation of rain.”  Espy derived his final point empirically by col-
                   lecting observations and testimonials to the effect that (5) air does indeed rush
                   inward on all sides toward the center of the region where a great rain is falling
                   and upward into the cloud.
                     Espy explained that three things can prevent rains from accompanying great
                   fires: (1) winds, (2) excessive moisture, and (3) stability of the upper levels of the
                   atmosphere. He released small balloons and tracked their flight in order to get
                   a sense of the winds, and he used a hygrometer to measure atmospheric mois-
                   ture and estimate its changes with height. Stability was more of a problem, for as
                   he observed, in the present state of science, the levity of an upper stratum of air
                   could not always be known. Correspondents, friends, and even a congressman
                   laughed at Espy when they heard of his proposal to make rain, but he assured


            54  |  rain makerS
   66   67   68   69   70   71   72   73   74   75   76