Mémoire numérisé par la Direction des bibliothèques de l'Université de Montréal.

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In 1981, the United States Supreme Court delivered a landmark ruling in Upjohn Co. v. United States. The decision made clear that the protections afforded by the attorneyclient privilege apply to internal corporate investigations. This piece examines the fundamental tenets of Upjohn, discusses some recent challenges to the applicability of privilege to materials gathered during internal investigations, and considers the manner in which the international nature of modern internal investigations adds complexity and uncertainty to the field.

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Information from business emails is often very important for investigating breaches of rules or for court proceedings. However, strict legal requirements apply to the analysis and inspection of emails. The following overview sets out these requirements and describes the risks resulting from failure to comply with them, while focusing primarily on more recent court rulings. The article also shows how employers can effectively mitigate or avoid legal risks when monitoring emails. One of the main focuses of the overview is on recommended actions to take in practice and a checklist for preparing for and implementing access to business email accounts.

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It gives us great pleasure to introduce you to our second edition of the Compliance Elliance Journal (CEJ).

Mémoire numérisé par la Division de la gestion de documents et des archives de l'Université de Montréal.

The observed summertime drying over Northern Central India (NCI) during the latter half of the twentieth century is not reproduced by the Coupled Model Intercomparison Project Phase 5 (CMIP5) model ensemble average. At the same time, the spread between precipitation trends from individual model realizations is large, indicating that internal variability potentially plays an important role in explaining the observed trend. Here we show that the drying is indeed related to the observed 1950–1999 positive trend of the Pacific Decadal Oscillation (PDO) index and that the relationship is even stronger for a simpler index (S1). Adjusting the CMIP5-simulated precipitation trends to account for the difference between the observed and simulated S1 trend increases the original multimodel average NCI drying trend from −0.09 ± 0.31 mm d−1 (50 years)−1 to −0.54 ± 0.40 mm d−1 (50 years)−1. Thus, our estimate of the 1950–1999 NCI drying associated with Pacific decadal variability is of similar magnitude as our previous CMIP5-based estimate of the drying due to anthropogenic aerosol. The drying (moistening) associated with increasing (decreasing) S1 can partially be attributed to a southeastward (northwestward) shift of the boundary between ascent and descent affecting NCI. This shift of the ascent region strongly affects NCI but not Southeast Asia and south China. The average spread between individual model realizations is only slightly reduced when adjusting for S1 as smaller-scale variability also plays an important role.