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  • Other Sources  (3)
  • 2010-2014  (3)
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  • 1
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    The Eastern Mediterranean Transient (2014)
    AGU (American Geophysical Union) | Wiley
    In:  In: The Mediterranean Sea. , ed. by Borzelli, G. L. E., Gačić, M., Lionello, P. and Malanotte‐Rizzoli, P. Geophysical Monograph Series, 202 . AGU (American Geophysical Union), Wiley, Washington, pp. 75-83.
    Details
    Publication Date: 2020-08-03
    Description: The eastern Mediterranean transient (EMT) was caused by a combination of high‐salinity waters intruding into the Aegean Sea and the two particularly strong winters of 1991–1992 and 1992–1993. The approach in this chapter is to search for specific signatures in the historic hydrographic observations, which date back to 1910. To deal with the problem that up into the 1950s the data not only are of limited precision but also have gaps of about 20 years, it is advantageous to consider the fact that the evolution of the actual EMT is rather well documented over a similar time span. The chapter begins by outlining the characteristics of the current EMT. Thereafter, a selection of suitable hydrographic observations among the available historic data is provided to compare these with signatures expected from the evolution of the actual EMT.
    Type: Book chapter , PeerReviewed
    Format: text
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  • 2
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    Deep water formation, the subpolar gyre, and the meridional overturning circulation in the subpolar North Atlantic (2011)
    Elsevier
    In:  Deep Sea Research Part II: Topical Studies in Oceanography, 58 (17-18). pp. 1819-1832.
    Details
    Publication Date: 2020-08-05
    Description: On interannual to decadal times scales, model simulations suggest a strong relationship between anomalies in the deep water formation rate, the strength of the subpolar gyre, and the meridional overturning circulation in the North Atlantic. Whether this is valid, can only be confirmed by continuous, long observational time series. Several measurement components are already in place, but crucial arrays to obtain time series of the meridional volume and heat transport in the subpolar North Atlantic are still missing. Here we summarize the recent developments of the deep water formation rates and the subpolar gyre transports. We discuss how existing observational components in the subpolar North Atlantic could be supplemented to provide long-term monitoring of the meridional heat and volume transport. Through a combined analysis of observations and model results the temporal and spatial scales that had to be covered with instruments are discussed, together with the key regions with the highest variability in the velocity and temperature fields.
    Type: Article , PeerReviewed
    Format: text
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  • 3
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    The Eastern Mediterranean Transient: evidence for similar events previously? (2014)
    AGU (American Geophysical Union) | Wiley
    In:  In: The Mediterranean Sea: Temporal variability and spatial patterns. Geophysical Monograph Series, 202 . AGU (American Geophysical Union), Wiley, Washington, USA, pp. 75-83.
    Details
    Publication Date: 2015-09-28
    Type: Book chapter , PeerReviewed
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