Climatology and the problems of western grasslands

Sixty years after Coronado, Don Juan de Onate wrote the first reasonably good description of the High Plains. He was near the present site of Wichita, Kansas, in 1601, when he arrived a t a large rancheria, or temporary Indian camp, containing more than 5000 souls. Onate's account expressed wonderment at the great extent of the level land, a t the numerous small streams bordered with luxuriant groves of trees, and, of course, at the large number of buffalo.

We shall never see the wonderland of the blossoming prairie which he described as follows: Grazing for the horses "had been lacking for several days, as there had been none for many leagues, for the fields there were covered with flowers of a thousand different kinds, so thick that they choked the pasture " (1, p. 256).

We who fly from Chicago to Denver in a few hours cannot get the same view of the western grasslands as those who, with rifle or sword in hand, moved at the rate of 10 to 15 miles a day.

The tall- and short-grass prairies of the West comprise more than 700,000 square miles in the United States alone, not to mention the great prong extending northward into Canada. Such an area represents nearly a quarter of the United States. There are areas other than prairie where grass is an important natural resource. Among these should be mentioned the grass openings in woodland and along the borders of desert shrub associations in the plateau and basin-and-range provinces. So considered, the western grassed areas constitute even a larger proportion of our country.

This vast domain has problems commensurate in complexity with its geographic scope, and these are in part related to the changes which have occurred since settlement. I shall attempt to state the most important current problems as I see them, and then will discuss briefly the role of the climatologist in their solution.