Fig. 1.
Cross sections across an 80 km wide sea gulf at 60°N. Calm ( V g=0), cold, clear sky December day,+20 h simulation. Δx=2 km, SST = + 1 °C, z 0=0.1 mm at the sea.
Table 1. The maximum u, v and w at the indicated heights, T2m at the coast and far inland as the function of the initial surface temperature T s, from a calm case + 20 h simulation with SST of 1 °C.
Fig. 2.
As Fig. 1 but for (u g, v g)=(2, 0) ms−1 ( V g from left to right).
Fig. 3.
As Fig. 1 but for (u g, v g)=(6, 0) ms−1.
Fig. 4.
As Fig. 1 but for (u g, v g)=(0, 10) ms−1 ( V g into the figure plane), z 0=1 mm at the sea.
Fig. 5.
As Fig. 4 but for (u g, v g)=(2, 9.8) ms−1.
Fig. 6.
Sea level pressure (dashed lines, hPa), 500 hPa heights (solid lines, gpm) and SYNOP observations from 7 December 1998 12UTC over the Gulf of Bothnia (between Sweden and Finland) and the Gulf of Finland (along 60°N). The location of Gävle, Sweden is marked.
Fig. 7.
As Fig. 5 but for a gulf 120 km wide.
