Sentence examples for convergence lines from inspiring English sources

b ΔEPT distribution and surface wind convergence lines.

According to Fig. 18c, lightning strokes were distributed over the topographic 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.

In Fig. 11b, strong wind convergence lines (divU ≤−20[×10−5/s]) are expressed by solid lines, while weak convergence lines (−20[×10−5/s] < divU ≤ −10[×10−5/s]) are expressed by dashed lines.

Additionally, due to northwesterly winds blowing over the Sea of Japan, topographic convergence lines were formed along the coastline.

Additionally, topographic convergence lines formed along the Tohoku and Hokuriku coastline, while ΔEPT was smaller than in previous periods.

According to Fig. 11c, lightning strokes were distributed along the convergence line at the cold front.

In addition, a strong convergence line was formed along the Tohoku coastline in connection with the topographic effects described above in the type A case study.

Additionally, the gradient of ΔEPT across the convergence line was significantly large, indicating that a boundary existed between the stable air mass and the unstable air mass.

Figure 14c shows that lightning strokes were concentrated over the unstable air mass (ΔEPT ≥0 K) and along the topographic convergence line in the coastal areas of the Tohoku district rather than over the weak convergence line along the cold front.

Since SK and SJ cyclones take the northernmost course of all cyclone types, the strong wind convergence line on the cold front may not reach the more southern Hokuriku district.