Morphological classification of microtidal sand and gravel beaches

A new classification of microtidal sand and gravel beaches with very different morphologies is presented below. In 557 studied transects, 14 variables were used. Among the variables to be emphasized is the depth of the Posidonia oceanica. The classification was performed for 9 types of beaches: Type 1: Sand and gravel beaches, Type 2: Sand and gravel separated beaches, Type 3: Gravel and sand beaches, Type 4: Gravel and sand separated beaches, Type 5: Pure gravel beaches, Type 6: Open sand beaches, Type 7: Supported sand beaches, Type 8: Bisupported sand beaches and Type 9: Enclosed beaches. For the classification, several tools were used: discriminant analysis, neural networks and Support Vector Machines (SVM), the results were then compared. As there is no theory for deciding which is the most convenient neural network architecture to deal with a particular data set, an experimental study was performed with different numbers of neuron in the hidden layer. Finally, an architecture with 30 neurons was chosen. Different kernels were employed for SVM (Linear, Polynomial, Radial basis function and Sigmoid). The results obtained for the discriminant analysis were not as good as those obtained for the other two methods (ANN and SVM) which showed similar success.

Castles in the sand: Mali and the demise of the EU’s Common Security and Defence Policy. CEPS Commentary, 28 January 2013

The threat posed by the crisis in Mali is direct, multidimensional and without regard to geographical proximity or historical and colonial heritage, writes Giovanni Faleg. France’s solitary intervention in Mali and the EU’s absence there raise two important questions for the future of the EU’s supposedly ‘Common’ Security and Defence Policy. The first has to do with the crisis itself; its nature and the threat posed by the terrorist groups and militias that are being countered by French armed forces. The second concerns the causes and implications of yet another example of the EU’s inability to take responsibility for security matters in its neighbourhood and beyond.

Vanishing lines in the sand – Why a new map of the Middle East is necessary. CEPS Commentary, 1 October 2013

As the stalemate in Syria drags on, territorial divisions in the country are becoming more entrenched and the civil war is spreading to Syria’s neighbours; aggravating long-standing sectarian divisions in the whole region. In the view of Steven Blockmans, a lasting agreement cannot be reached in the Middle East if world powers stick to infamous 1916 Sykes-Picot Agreement in which France and the UK secretly dealt with what came to be called the ‘Syria Question’. Any way out of the quagmire will require a grand bargain – one that establishes a new order in the whole region and draws borders accordingly.

Heads buried in the sand: member states block solutions to the refugee crisis. EPC Commentary, 15 September 2015

Yesterday’s meeting of Interior Ministers demonstrated that the EU’s asylum and immigration policy remains incomplete. This is mainly due to the member states’ inability to plan ahead, their reluctance to adopt binding common rules – considered as a violation of their sovereignty – and their central position in the implementation of EU rules.

Stricter regulation boosts exports: the case of Maximum Residue Levels in pesticides

Constructing an original panel on Maximum Residue Levels (MRLs) in pesticides for 50 countries over 2006-2012, this paper studies the effect of heterogeneity in MRL regulation on bilateral trade. We find evidence of regulatory heterogeneity diminishing trade at the extensive margin when the exporter faces more stringent regulation abroad, suggesting compliance costs in entering the destination market. Significantly, however, we also find strong evidence of regulatory heterogeneity increasing trade at the intensive margin for exports coming from countries that set the strictest standards, alluding to the positive informative effect of such regulation.

Clay mineralogy of carbonate-rich sediments of ODP Leg 101 sites

The insoluble residues of samples from ODP Sites 626 and 627 can be subdivided into four groups: (1) illite, 7 A minerals, quartz and feldspar; (2) smectite and zeolite (clinoptilolite); (3) palygorskite and in places sepiolite; and (4) glauconite and pyrite. Whereas group 1 is clearly terrigenous and group 4 authigenic, group 2 is most probably authigenic, as indicated by its abundance in samples with small insoluble residues and its appearance in SEM photographs. Group 3 is authigenic in Albian peritidal dolomite and possibly terrigenous in middle Miocene slumps and debris flows. Smectite crystallinity increases with age. This increase, however, is less pronounced in the Bahamian carbonate-rich samples than in the carbonate-poor silts south of Guatemala (DSDP Leg 84, Sites 569 and 570, the only comparable investigation) as far as can be judged from such a small number of samples.