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Near-term impact of climate variability on yam rot incidence over a humid tropical region: projections in CORDEX-Africa scenarios

Published online by Cambridge University Press:  05 April 2021

Ugochukwu K. Okoro*
Affiliation:
Atmospheric Physics Group, Department of Physics, Imo State University, Owerri, Nigeria
Jacinta N. Akalazu
Affiliation:
Department of Plant Science and Biotechnology, Imo State University, Owerri, Nigeria
Nobert C. Nwulu
Affiliation:
Atmospheric Physics Group, Department of Physics, Imo State University, Owerri, Nigeria
*
Author for correspondence: Ugochukwu K. Okoro, E-mail: uknac23@yahoo.com
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Abstract

The global population is projected to be enormous by the mid-21st century, whereas, most essential crops being sustained by the rain-fed agriculture are threatened by climate change. Therefore, the study investigated the projected near-future effect of rainfall variability on rot incidence and yam production in humid tropical Nigeria. Production data from the Food and Agriculture Organization and the Nigeria National Bureau of Statistics showed the significant increasing trend in the annual yam output. The field survey conducted in 2018 showed that the maximum percentage of rot incidence occurred in July. Climate Research Unit observational rainfall data from 1979 to 2018 showed the nonsignificant trend in the interannual rainfall variability; however, it showed low variability and a significant decreasing trend in the July rainfall. A pathogenicity test on yam samples confirmed rot by fungi, bacteria and nematodes as virulent pathogens, whereas, the nutritional qualities of the rotted yams were indicated. Monthly rainfall and rot incidence showed positive correlation (r = 0.84, significant at 99% from t-test). The positive characteristic impact values indicated that increase (decrease) in the monthly rainfall corresponds to increase (decrease) in the magnitude of monthly percentage rot incidence. Thus, the significantly decreasing rainfall reduced the quantity of rot incidence and consequently increased the annual yam production for the period. Selected CoOrdinated Regional Downscaling EXperiment-Africa models and the ensemble mean showed a good measure of agreement with observational rainfall in the historical experiments. The efficiencies of the bias-corrected outputs in the representative concentration pathway (RCP) 4.5 and 8.5 indicated improved ‘reasonable’ performances. Bias-corrected projections of the July rainfall showed an increasing trend in both the RCPs, which indicate a potential increase in rot incidence and the consequent decline in annual yam production. The findings are imperative in sustaining the global food supply.

Information

Type
Research Paper
Copyright
Copyright © The Author(s), 2021. Published by Cambridge University Press
Figure 0

Fig. 1. Humid tropical Nigeria (delineated below thin horizontal line) indicating the selected state locations with their annual rainfall (mm) climatological mean from 1979 to 2018 (solid squares), and the three agroecological zones, respectively (shaded).

Figure 1

Table 1. List of the CORDEX-Africa models, their descriptions and references

Figure 2

Fig. 2. Time series of (a) FAO national annual yam production (tons) output for Nigeria from 1979 to 2018, and (b) NBS annual yam production (tons) data for the states from 1995 to 2006.

Figure 3

Fig. 3. Monthly percentage (%) of yam rot incidence from January to December 2018. The error bars indicate the s.d. of the percentage rot incidence in each month, respectively.

Figure 4

Table 2. Average population of the pathogenic fungi isolates from the rotted tubers expressed in CFU per 10 ml of water

Figure 5

Table 3. Average population of the pathogenic bacteria isolates from the rotted tubers expressed in CFU per 10 ml of water

Figure 6

Table 4. Average population density of pathogenic nematode species extracted from the peel of the rotted tubers

Figure 7

Table 5. Average percentage (%) composition from proximate analysis on 1 g sample of each yam

Figure 8

Fig. 4. 12-month SPI of the annual rainfall at the locations and the areal average, respectively. Inserted at the top left corner of each panel is the Sen's slope of the trends.

Figure 9

Fig. 5. Temporal trends of CRU monthly rainfall from 1979 to 2018 at the locations and the areal average, respectively. The Sen's slope (▴ = increase; ● = no trend; ▾ = decrease) values (mm yr−1) of the trends are indicated, whereas, the levels of significance (+ at α = 0.05; ++ at  α = 0.01; +++ at  α = 0.001) are shown. The Sen's slope value (mm yr−1), its significance level, and the CV value (%) for the areal average of each month, respectively, is indicated at the bottom right corner of each panel.

Figure 10

Table 6. Statistical relationship between the monthly percentage (%) yam rot incidence and the monthly rainfall

Figure 11

Table 7. Statistical performance of the historical outputs (1979–2005) in simulating the CRU monthly rainfall variability and the annual rainfall temporal trends

Figure 12

Fig. 6. Temporal trends of July rainfall simulations in historical output from the models and the ensemble mean, and the CRU for the same period. The Sen's slope (▴ = increase; ● = no trend; ▾ = decrease) values (mm yr−1) of the trends are indicated, whereas, the level of significance (+ at  α = 0.05) is shown. The Sen's slope value (mm yr−1) for the areal average of each month is indicated at the bottom right corner of each panel.

Figure 13

Table 8. Statistical performance of the bias corrected RCP 4.5 and RCP 8.5 outputs, respectively, in simulating the CRU monthly rainfall variability and the annual rainfall temporal trends from 2006 to 2018

Figure 14

Table 9. Projected 12-month SPI of annual rainfall temporal trends from 2019 to 2050 in the bias corrected outputs of RCP 4.5 and RCP 8.5 experiments, respectively

Figure 15

Fig. 7. Projected trends of July rainfall in RCP 4.5 from the models and the ensemble mean from 2019 to 2050. The Sen's slope (▴ = increase; ● = no trend; ▾ = decrease) values (mm yr−1) of the trends are indicated, whereas, the level of significance (+ at  α = 0.05) is shown. The Sen's slope value (mm yr−1) for the areal average of each month is indicated at the bottom right corner of each panel.

Figure 16

Fig. 8. Projected trends of July rainfall in RCP 8.5 from the models and the ensemble mean from 2019 to 2050. The Sen's slope (▴ = increase; ● = no trend; ▾ = decrease) values (mm yr−1) of the trends are indicated, whereas, the level of significance (+ at  α = 0.05) is shown. The Sen's slope value (mm yr−1) for the areal average of each month is indicated at the bottom right corner of each panel.