In OND, we do see a highly significant association between EQL rains and evolutionary phases of IOD, with a positive phase IOD leading to more precipitation in EQL.
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Perspectives on CMIP5 model performance in the Nile River headwaters regions.
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The first mode of variability exhibits a positive trend (Figure 5 (a)) that can be associated with pan‐tropical increases in SST (Figure 6 (a)).