In order to better understand the general tidal features in the venturi-shaped area between Zhenhai and Shenjiamen in the northern coastal region of Zhejiang Province in the East China Sea

the tidal data were obtained from both the three permanent tide stations of Zhenhai

Dinghai and Shenjiamen

and four temporary tide stations of Mamu

Chuanshan

Guoju and Liuheng

along with the current speed being observed at Luotou Waterway. Results from harmonic analysis show that: (1) The area was dominated by shallow water tides with irregular semi-diurnal features

and the smallest tidal range occurred in the area near a crossing line between Zhenhai and Dinghai stations

indicating that a tidal node existed in the southern Hangzhou Bay; (2) Formulae

$$ H_{S_2 } /H_{M_2 } > 0.4 $$ and $$ g_{M_2 } - (g_{K_1 } + g_{O_1 } ) $$ =270° (where H and g are harmonic constants)

could be used as judging criteria for high and low tidal level diurnal inequalities; (3) The duration difference between ebb and flood tides could be roughly assessed by the ratio of $$ H_{M_4 } vs. H_{M_2 } $$ ; and the larger the ratio is

the bigger the duration difference is. At the same time

the duration period could be assessed by $$ 2g_{M_2 } - g_{M_4 } $$

the epoch difference between M 2 and M 4 tidal constituents. If $$ 2g_{M_2 } - g_{M_4 } $$ <180°

then the ebb duration is longer than the flood duration; if 180°< $$ 2g_{M_2 } - g_{M_4 } $$ <360°

the result is reversed; (4) Taking Dinghai station as a center point

the highest tidal levels and the average high tidal levels

as well as the average tidal ranges at all stations became higher and larger both southeastwards and northwestwards

while the lowest tidal levels and the average low tidal levels appeared to be lower both southeastwards and northwestwards; and (5) The tidal patterns were not all in line with the tidal current patterns. As a conclusion

the smallest tidal range occurred in the narrow part of the venturi-shaped area. Along the both sides of the area

the highest tidal level and tidal range became higher and larger

while the lowest tidal level became lower with the increase of the distance from the narrow throat area. This is somehow different from the theory that the tidal level increases gradually when it moves towards the top narrow area of a V-shaped bay or estuary.