The theory arose in the late 1860s and 1870s as American settlement expanded west of the
Missouri River and across the
100th meridian west. This was the traditional boundary line between the
humid and semi-arid portions of central
North America. Specifically, in the early part of the decade, white settlement had spread into central and western
Nebraska along the
Platte River. Emigrants on the
Oregon Trail began reporting that the land in western Nebraska, previously known for its yellowed, dry vegetation during the summer, had seemingly become green. Out of this evidence, some scientists concluded that the apparent increase in rain was due to the settlement and the effects of cultivation. One of the most prominent exponents of the theory in the United States was
Cyrus Thomas, who was a noted
ethnologist and
entomologist but only an amateur
climatologist at best. After studying the recent history of Colorado, he concluded that the increase in moisture was permanent, and that it coincided exactly with the first settlers' cultivating of the land. Other prominent advocates of the theory were
Ferdinand Vandeveer Hayden, the noted
geographer who had explored and
surveyed parts of the
Rocky Mountains of Colorado;
Samuel Aughey, a professor at the
University of Nebraska; and Charles Dana Wilber, an
amateur scientist and author. Thomas and other climatologists offered a variety of explanations for the theory. A common idea was that the plowing of the
soil for cultivation exposed the soil's moisture to the sky. In addition, newly planted trees and shrubs increased rainfall as well, as did
smoke from
trains, or even the metal in the rails or the telegraph wires. Another hypothesis stated that the increased
vibrations in the
atmosphere due to human activity created additional
clouds, from which rain fell. This idea led to the widespread
dynamiting of the air across the
Great Plains in the 1870s. The theory was widely embraced in its day, not only by scientists, but land speculators and emigrants. Some historians have argued that the theory was embraced readily as an outgrowth of
Manifest Destiny, the idea that the United States had a mission to expand, spreading its form of
democracy and freedom. The theory is regarded as partially responsible for the rapid settlement of the Great Plains in the later 19th century. In
The Great Valleys and Prairies of Nebraska and the Northwest, published in 1881, Charles Dana Wilber wrote: In this miracle of progress, the plow was the unerring prophet, the procuring cause, not by any magic or enchantment, not by incantations or offerings, but instead by the sweat of his face toiling with his hands, man can persuade the heavens to yield their treasures of dew and rain upon the land he has chosen for his dwelling... ...The raindrop never fails to fall and answer to the imploring power or prayer of labor.
William Gilpin, the first territorial governor of
Colorado and an aide to President
Abraham Lincoln, was a proponent of this theory. Gilpin was a strong believer in the idea of Manifest Destiny. One of his books was called
The Mission of the North American People. He strongly promoted western settlement and invoked this theory as one of his reasons
for people to migrate west. Climatologists now understand that increased vegetation and
urbanization can result in increased
precipitation. The effect, however, is local in scope, with increased rainfall typically coming at the expense of rainfall in nearby areas. It cannot result in a climatological change for an entire region. They also understand that the Great Plains had had a wetter-than-usual few seasons while this theory was developed and increasing settlement were both taking place. When normal arid conditions returned,
homesteaders suffered. In 2007,
Richard Raddatz, a
climatologist at the
University of Winnipeg, published results of his studies on the conversion of Canadian
grasslands to cropland. His theory is that, because
corn crops
transpire moisture into the atmosphere at a faster rate than the grass they have replaced, crops can generate storms and intensify the season during which
water can cycle through the atmosphere. Observed trends of Midwest summertime cooling and increased rainfall over the last third of the 20th century have been linked to agricultural practices in the arid Great Plains, in an inversion of the
Dust Bowl scenario. Increased precipitation and humidity may cause the downward trend in Midwestern average daytime highs, since humid air takes more energy to heat to a given temperature than dry air. In turn, the increase in Midwestern rainfall may be driven by the large increase in land under irrigation in the Plains over the 20th century. Irrigation water enters the atmosphere through evaporation and plant transpiration, and then falls as rain over the downwind Midwest. == Australia ==