Research Article

Wind Climate in Kongsfjorden, Svalbard, and Attribution of Leading Wind Driving Mechanisms through Turbulence-Resolving Simulations

Figure 3

The climatological probability of wind directions in Ny-Ålesund from the IGRA data archive for four seasons: winter (a), spring (b), summer (c), and autumn (d). The black bars correspond to the probability of the surface winds, and the white bars to the winds at the 700 hPa pressure level.
568454.fig.003a
(a)
568454.fig.003b
(b)
568454.fig.003c
(c)
568454.fig.003d
(d)