“Les petits renards qui détruisent la Vigne du Seigneur Sabaoth”. Innocent III et le Cantique des cantiques

This article examines medieval interpretations of the Song of Songs and their appearance in the correspondence of one of the greatest popes of the High Middle Ages: Innocent III (1198-1216). Innocent III’s depiction of heretics in the south of France as ‘the little foxes which destroy the vineyard of the Lord of Hosts’ was not unprecedented: decades earlier Saint Bernard of Clairvaux had also likened the ‘little foxes’ to heretics in his sermons. Bernard’s renown both as mystical theologian and tireless political advocate of the papacy meant that Innocent is likely to have drawn on such sermons for inspiration when composing his correspondence to the Christian faithful. Innocent’s references to the Song of Songs also provide conclusive evidence that a significant number of his letters have a highly personal flavour and that we really can discern a pope’s own ‘voice’ through his correspondence.

Formation and circulation of the cold intermediate layer in the Gulf of Saint Lawrence

[ 1] The local heat content and formation rate of the cold intermediate layer (CIL) in the Gulf of Saint Lawrence are examined using a combination of new in situ wintertime observations and a three-dimensional numerical model. The field observations consist of five moorings located throughout the gulf over the period of November 2002 to June 2003. The observations demonstrate a substantially deeper surface mixed layer in the central and northeast gulf than in regions downstream of the buoyant surface outflow from the Saint Lawrence Estuary. The mixed-layer depth in the estuary remains shallow (< 60 m) throughout winter, with the arrival of a layer of near-freezing waters between 40 and 100 m depth in April. An eddy-permitting ice-ocean model with realistic forcing is used to hindcast the period of observation. The model simulates well the seasonal evolution of mixed-layer depth and CIL heat content. Although the greatest heat losses occur in the northeast, the most significant change in CIL heat content over winter occurs in the Anticosti Trough. The observed renewal of CIL in the estuary in spring is captured by the model. The simulation highlights the role of the northwest gulf, and in particular, the separation of the Gaspe Current, in controlling the exchange of CIL between the estuary and the gulf. In order to isolate the effects of inflow through the Strait of Belle Isle on the CIL heat content, we examine a sensitivity experiment in which the strait is closed. This simulation shows that the inflow has a less important effect on the CIL than was suggested by previous studies.