| Summary: | An analysis ismade of data from 30 Aanderaa recording currentmeters (RCMs) set on ninemoorings located east of Cape Farewell, the southern tip of Greenland. The purpose of the measurements was to allow for the estimation of transport in the deep western boundary current (DWBC) below a depth of about 1500 m. The records commenced in September 2005 and lasted from9.5 to 11.5months.After calibration of the rawdata, 12-h averages of temperature and current were derived and the latter employed to estimate the flow across and along the array direction. The 9.5-month average transport of water colder than 38Cwas found to be 7.8 Sv (1 Sv[13 106 m3 s21) with a standard error of 0.8 Sv. For water denser than su527.85 kg m23, the transport is calculated as 4.5 Sv. Whether either of these values is significantly different fromcomparablemeasurementsmade 500 km upstream cannot be determined. In marked contrast, for su . 27.8 kg m23, the transport is estimated as only 9.0 Sv, smaller than the widely accepted value of 13 Sv for nearby measurements made in 1978. A reevaluation of the calculations and assumptions made then allows one to determine the uncertainty of the earlier estimate and thereby conclude that the difference between the previous and present measurements is significant, that is, that the transport has decreased between 1978 and 2005–06. Aweakening of the transport during the 9.5-month period is also observed, along with a warming and an increase in salinity in the core of the DWBC. These latter changes are shown to be consistent with interannual variability rather than a long-term trend.
|
|---|