Cl. Douglas et al., AGROCLIMATIC ZONES FOR DRYLAND WINTER-WHEAT PRODUCING AREAS OF IDAHO,WASHINGTON, AND OREGON, Northwest science, 66(1), 1992, pp. 26-34
There is a need to develop a series of "zones" to facilitate technolog
y transfer within the Intermountain Northwest. Six agroclimatic zones
have been delineated based on three climatic and soil parameters impor
tant in growing winter wheat: soil depth, mean annual precipitation, a
nd cumulative growing degree from 1 January through 31 May. Thus each
zone, regardless of the state in which it is located, has similar soil
and climatic conditions. There are uncultivated areas within each zon
e that are not identified but if farmed would be farmed like other par
ts of the same zone. The zones provide a common basis for identifying
areas where successful exchange of practices, experience, and knowledg
e between and among producers, researchers, extension, and Soil Conser
vation Service personnel will most likely occur. Management decisions
that produce desired results in one zone in one zone in one state will
probably succeed in that same zone in any other state. Conservation p
ractices and erosion control techniques should be similar within but n
ot between zones.