Drought -- National Drought Mitigation Center
Title
Exploring the Potential for Using ENSO Forecasts in the U.S. Corn Belt
Document Type
Article
Date of this Version
October 1996
Interannual climate variability poses the greatest risk that farmers face.
Until recently, seasonal climate forecasts have been weak and therefore rarely
observed by farmers in making management decisions. Farm management is
generally based on long-term mean expectations of climate and crop responses
to local edaphic conditions. Currently, significant progress is being
made in the skill level of predictions of seasonal to interannual climate,
primarily because of new understanding of the teleconnections between
ocean circulation and atmospheric processes. The El Niño/Southern Oscillation
(ENSO) refers to fluctuations in both sea-surface temperatures (SSTs) in
the eastern equatorial Pacific and in sea-level pressures in the southern Pacific
at a time scale of roughly 3 to 7 years. Using ocean circulation models, we are
now able to forecast the SST anomaly up to a year in advance with an 80%
level of accuracy (Latif et al., 1994). Thus, associated climate phenomena
may be predicted with a high degree of skill using this tool.
Given the strong relationship between crop growth and climate, this
predictability carries significant implications for improved efficiency of
agricultural production (Adams et al., 1995; Sonka et al., 1986). In some
regions, the teleconnection between climate and ENSO has been well
established. In others, however, the relationship is only now being elucidated.
Thus, the spatial extent of the potential for use of ENSO forecasts is not well
defined. We are developing a methodology that uses analysis of historical
climate and crop data as well as models of crop growth and farm management
to explore the extent of ENSO impacts and implications for using forecasts
in agricultural management.
Based on the few studies that have been done, there is indication of a
significant link between ENSO and climate in the midwestern United States.
Using reconstruction from white oak tree rings in Iowa going back to 1640,
Cleveland and Duvick (1992) showed a strong correlation with the Southern
Oscillation Index, one indicator of the ENSO phase. Handler (1984) used
yield data from the major Corn Belt states going back to 1868 and a
classification scheme ranking event intensity. He found a strong relationship,
with El Niño years associated with positive maize yield anomalies and La
Niña with negative anomalies. Our current work extends the analysis of the
U.S. Corn Belt, with the objective of testing the potential for using long-range
ENSO/climate forecasts to increase profit margins and decrease risk for
maize farmers in the United States.

Comments
Published in Drought Network News October 1996. Published by the International Drought Information Center and the National Drought Mitigation Center, School of Natural Resources, University of Nebraska – Lincoln.