It is on the grounds outlined in this chapter that students of the subject believe that ultimately large areas of the “desert” may be reclaimed by means of dry-farming.  The real question before the dry-farmer is not, “Is the rainfall sufficient?” but rather, “Is it possible so to conserve and use the rainfall as to make it available for the production of profitable crops?”

CHAPTER III

DRY-FARM AREAS—­RAINFALL

The annual precipitation of rain and snow determines primarily the location of dry-farm areas.  As the rainfall varies, the methods of dry-farming must be varied accordingly.  Rainfall, alone, does not, however, furnish a complete index of the crop-producing possibilities of a country.

The distribution of the rainfall, the amount of snow, the water-holding power of the soil, and the various moisture-dissipating causes, such as winds, high temperature, abundant sunshine, and low humidity frequently combine to offset the benefits of a large annual precipitation.  Nevertheless, no one climatic feature represents, on the average, so correctly dry-farming possibilities as does the annual rainfall.  Experience has already demonstrated that wherever the annual precipitation is above 15 inches, there is no need of crop failures, if the soils are suitable and the methods of dry-farming are correctly employed.  With an annual precipitation of 10 to 15 inches, there need be very few failures, if proper cultural precautions are taken.  With our present methods, the areas that receive less than 10 inches of atmospheric precipitation per year are not safe for dry-farm purposes.  What the future will show in the reclamation of these deserts, without irrigation, is yet conjectural.

Arid, semiarid, and sub-humid

Before proceeding to an examination of the areas in the United States subject to the methods of dry-farming it may be well to define somewhat more clearly the terms ordinarily used in the description of the great territory involved in the discussion.

The states lying west of the 100th meridian are loosely spoken of as arid, semiarid, or sub-humid states.  For commercial purposes no state wants to be classed as arid and to suffer under the handicap of advertised aridity.  The annual rainfall of these states ranges from about 3 to over 30 inches.

In order to arrive at greater definiteness, it may be well to assign definite rainfall values to the ordinarily used descriptive terms of the region in question.  It is proposed, therefore, that districts receiving less than 10 inches of atmospheric precipitation annually, be designated arid; those receiving between 10 and 20 inches, semiarid; those receiving between 20 and 30 inches, sub-humid, and those receiving over 30 inches, humid.  It is admitted that even such a classification is arbitrary, since aridity does not alone depend upon the rainfall, and even under such