10 
B.  Helland-Hansen. 
[No.  15 
Fig.  1.  The  stations  in  the  Sondmure  Piords  and  in  the  Norwegian  Sea.  (The 
bottoni-lines  in  fathoms). 
from  the  Sule  Fiord.  The  locality  of  the  different  stations  will  be 
seen  trom  the  chart  (hg.  1).  In  the  upper  portion  of  the  Hjo rund 
Fiord  observations  were  taken  during  the  course  of  4 hours  on 
the  alternoon  of  the  3rd  July.  High  water  occurred  at  9 o’clock 
in  the  evening  or  a little  later.  During  the  rise  of  the  tide  the 
veloeities  increased  at  one  meter  below  the  surfaee  (0  p.m.  about 
7 c:n./gec.  aiid  10  p.m.  nearly  10  cm./g^,.  );  tlie  movement  was  out- 
wards  the  whole  time.  At  5 meters  the  opposite  was  found  to  be 
the  case;  the  water  howed  inwards  during  the  ilse  of  the  tide  and 
with  decreasing  veloeities  (at  (i  offloek  15  cm.  per  second  and  at 
