Dry-Farming : A System of Agriculture for Countries under a Low Rainfall — John Shaqi
Dry-Farming : A System of Agriculture for Countries under a Low RainfallWidtsoe, John Andreas
Science
Dry-Farming : A System of Agriculture for Countries under a Low Rainfall
Widtsoe, John Andreas
Dry farming
The total annual precipitation is directly influenced by the land
topography, especially by the great mountain ranges. On the east of
the Rocky Mountains is the sub-humid district, which receives from
20 to 30 inches of rainfall annually; over the Rockies themselves,
semiarid conditions prevail; in the Great Basin, hemmed in by the
Rockies on the east and the Sierra Nevadas on the west, more arid
conditions predominate; to the west, over the Sierras and down to
the seacoast, semiarid to sub-humid conditions are again found.
Seasonal distribution of rainfall
It is doubtless true that the total annual precipitation is the
chief factor in determining the success of dry-farming. However, the
distribution of the rainfall throughout the year is also of great
importance, and should be known by the farmer. A small rainfall,
coming at the most desirable season, will have greater
crop-producing power than a very much larger rainfall poorly
distributed. Moreover, the methods of tillage to be employed where
most of the precipitation comes in winter must be considerably
different from those used where the bulk of the precipitation comes
in the summer. The successful dry-farmer must know the average
annual precipitation, and also the average seasonal distribution of
the rainfall, over the land which he intends to dry-farm before he
can safely choose his cultural methods.
With reference to the monthly distribution of the precipitation over
the dry-farm territory of the United States, Henry of the United
States Weather Bureau recognizes five distinct types; namely: (1)
Pacific, (2) Sub-Pacific, (3) Arizona, (4) the Northern Rocky
Mountain and Eastern Foothills, and (5) the Plains Type:--
_"The Pacific Type.--_This type is found in all of the territory
west of the Cascade and Sierra Nevada ranges, and also obtains in a
fringe of country to the eastward of the mountain summits. The
distinguishing characteristic of the Pacific type is a wet season,
extending from October to March, and a practically rainless summer,
except in northern California and parts of Oregon and Washington.
About half of the yearly precipitation comes in the months of
December, January, and February, the remaining half being
distributed throughout the seven months--September, October,
November, March, April, May, and June."
_"Sub-Pacific Type.--_The term 'Sub-Pacific' has been given to that
type of rainfall which obtains over eastern Washington, Nevada, and
Utah. The influences that control the precipitation of this region
are much similar to those that prevail west of the Sierra Nevada and
Cascade ranges. There is not, however, as in the eastern type, a
steady diminution in the precipitation with the approach of spring,
but rather a culmination in the precipitation."
Public-domain text, read in full here on John Shaqi.
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