The flow of water through the straits of Dover, related to wind and differences in sea level

Abstract

The difference in electric potential between the water on opposite sides of the English Channel, as recorded on a telephone cable running from St Margaret’s Bay to Sangatte, has been used to measure the mean flow of water through the Straits of Dover. The records were calibrated by means of the tidal currents, which were know from previous measurements. A p.d. of 1 V corresponds to a current of about 140 cm /s (2.75 knots), the exact calibration depending on the electrical conductivity o f the sea water and having a seasonal variation. Continuous records were obtained during the 15-month period from February 1953 to June 1954. For 4 months, from November 1953 to March 1954, similar records were also obtained on an other cable, crossing the southern North Sea from Aldeburgh to Domburg. Fluctuations due to the Earth currents associated with geomagnetic disturbances occurred from time to time, but did not usually cause any difficulty in in terpretin g the records. The residual flow, after eliminating the tidal currents, has been correlated with the local wind in the Straits and the difference in sea level between the eastern p a rt of the English Channel and the southern part of the North Sea, as determined from tide-gauge records. The tidal currents and elevations were eliminated, approximately, by taking means of 25 hourly readings centred at noon, for each day of the period covered by the observations. The greatest daily rates of flow recorded w ere 79 cm/s (T53 knots) towards the north-east on 1 November 1953 an d 77 cm /s (T49 knots) towards the south-w est on 3 January 1954. F or three periods of un usually strong flow, namely, 19 to 24 September 1953, 26 October to 8 November 1953, and 1 to 6 January 1954, a more detailed analysis was made, eliminating the tidal effects by a method previously used in the analysis of storm surges. The results show the existence of ‘current surges’, the peaks of which lag by up to 6 h behind the corresponding max im a in the wind stress or surface gradient producing them . An attempt has been made to relate the empirical results to the dynamics of flow through the Straits. On the assumption that the 25 h means can be regarded as referring to steady-state conditions, values o f 4-5 x 10<super>-3</super> for the w ind-stress coefficient y<super> 2</super> an d 3-8 x 10<super>-3</super> for the bottom friction coefficient k have been deduced. These rather high values may be due, in part, to the steady-state assumption not being justified. The general features of the current surges are consistent with the dynamical treatment.