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SIMULATING THE SENSITIVITY OF MAIZE CROP PROPAGATION
           TO SEASONAL WEATHER CHANGE USING CROPWAT-8
                                         by
                     Ewemoje, T. A. and OKANLAWON, S. A.
      Agricultural and Environmental Engineering Department University of
                               Ibadan, Ibadan, Nigeria.
       Introduction                        • Statistics: Descriptive (Mean), Least
•   Weather influences crop yield and         Square Difference (LSD) and T test.
    quality.                                    Results
•   Global warming has significant impact       Temperature rise has negative
    on agriculture.                             effect on maize yield.
•   Maize production is low under steady        Yield reduction trends were not
    temperature rise without rainfall or        definite due to discrepancy in
    irrigation.                                 temperature variability.
•   CROPWAT was used to model crop              Yield reduction was low under DI
    yield response to weather change.           and high for both CD and NI.
    Objectives                                  No significant difference
•   To simulate temperature changes             (p<0.05) between CD and DI.
    effects on maize crop yield.                Significant differences existed, at
•   To predict the effects of rise in           p < 0.05 between DI and NI, also
                                                between at CD and NI.
    temperature on maize yield.
                                                Coefficient of determination (R2)
•   To investigate appropriate irrigation
                                                is close to 1 therefore model is
    schedule to minimize yield loss.
                                                valid.
                                                Yield reduction was low between
                                                May and September, depicting
                                                better yield during rainy season.
                                                Moisture depletion increases with
                                                temperature and had a low value
                                                at DI irrigation schedule.
    Methods                                      Conclusion
• Study area: Ibadan, Nigeria.                   Weather change is not constant
• Data: Climatic, Soil and Crop.                 phenomenon, its ever changing.
• Irrigation Schedule: No Irrigation (NI),       DI is most preferred under
   Critical Depletion (CD) and Definite          uncertainty in variability of
   Interval (DI).                                weather change.

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Simulating the Sensitivity of Maize Crop Propagation to Seasonal Weather Change

  • 1. SIMULATING THE SENSITIVITY OF MAIZE CROP PROPAGATION TO SEASONAL WEATHER CHANGE USING CROPWAT-8 by Ewemoje, T. A. and OKANLAWON, S. A. Agricultural and Environmental Engineering Department University of Ibadan, Ibadan, Nigeria. Introduction • Statistics: Descriptive (Mean), Least • Weather influences crop yield and Square Difference (LSD) and T test. quality. Results • Global warming has significant impact Temperature rise has negative on agriculture. effect on maize yield. • Maize production is low under steady Yield reduction trends were not temperature rise without rainfall or definite due to discrepancy in irrigation. temperature variability. • CROPWAT was used to model crop Yield reduction was low under DI yield response to weather change. and high for both CD and NI. Objectives No significant difference • To simulate temperature changes (p<0.05) between CD and DI. effects on maize crop yield. Significant differences existed, at • To predict the effects of rise in p < 0.05 between DI and NI, also between at CD and NI. temperature on maize yield. Coefficient of determination (R2) • To investigate appropriate irrigation is close to 1 therefore model is schedule to minimize yield loss. valid. Yield reduction was low between May and September, depicting better yield during rainy season. Moisture depletion increases with temperature and had a low value at DI irrigation schedule. Methods Conclusion • Study area: Ibadan, Nigeria. Weather change is not constant • Data: Climatic, Soil and Crop. phenomenon, its ever changing. • Irrigation Schedule: No Irrigation (NI), DI is most preferred under Critical Depletion (CD) and Definite uncertainty in variability of Interval (DI). weather change.