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• W2066671645 abstract "Radium‐226 and 228 Ra data are presented for the Western Mediterranean Sea and the NE Atlantic. In the NW Mediterranean Sea, the near‐shore surface waters of the Ligurian Current contain much higher 228 Ra concentrations than surface waters collected in the open Ligurian seawater. The gradient of 228 Ra along a Villefranche ‐ Calvi transect has been used to calculate values of the horizontal eddy diffusion coefficient perpendicular to the flow direction of the Ligurian Current of about 10 6 cm 2 s −1 . The observed decay of 228 Ra, as the Mediterranean Deep Water flows toward the Gibraltar Straits, is in good agreement with the assumption of a rapid turnover of the Mediterranean basin. Concentration profiles of 226 Ra and 228 Ra were measured in the Mediterranean Outflow Water (MOW) off the Gibraltar Straits in the NE Atlantic basin at two stations, 36°30′N ‐ 15°35′W and 36°27′N ‐ 10°35′W. These sites showed the hydrographic characteristics of Meddies (MOW which propagates as eddies in the NE Atlantic) at intermediate depth. At the center of the Meddies, around 1000 m depth, the activity of the short half‐life 228 Ra increases up to 0.9 × 10 −2 disintegrations per minute per liter, higher than usually found in North Atlantic Deep Water. This “young” 228 Ra results from the contact, a few months earlier, of the MOW with the Spanish continental shelf in the vicinity of the Gibraltar Straits. The decay of 228 Ra, used as an internal tracer of water mass motion, leads to a transit time of the Meddy Yseult of less than 1 year since its formation." @default.
• W2066671645 created "2016-06-24" @default.
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• W2066671645 date "1996-02-15" @default.
• W2066671645 modified "2023-10-03" @default.
• W2066671645 title "Radium as internal tracer of Mediterranean Outflow Water" @default.
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• W2066671645 doi "https://doi.org/10.1029/95jc03308" @default.
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