Estimation of Strong Wind Distribution on the Korean Peninsula for Various Recurrence Periods: Significance of Nontyphoon Conditions

<div>Simulated wind vector and surface temperature fields in the innermost WRF model domain at 24:00 UTC on October 22, 2006 (a), and wind rose diagram for the strong wind event observed at the Daegwallyeong ASOS (b).</div>

Advances in Meteorology

fig10

Figure 10

Figure 10: Estimation of Strong Wind Distribution on the Korean Peninsula for Various Recurrence Periods: Significance of Nontyphoon Conditions 