Fig. 11From: Spatial distribution of cold-season lightning frequency in the coastal areas of the Sea of JapanComparisons of divU and ΔEPT with lightning frequency distribution for case A. a Surface wind and divU distribution. b ΔEPT distribution and surface wind convergence lines. Strong wind convergence lines (divU ≤−20[×10−5/s]) are shown as solid lines, while weak convergence lines (−20[×10−5/s] < divU ≤ −10[×10−5/s]) are shown as dashed lines. c Composite maps of lightning frequency distribution, wind convergence lines, and regions where ΔEPT exceeds 10 K (highlighted in pink)Back to article page