The examination of John Owen late of New Jersey brought before me Jeremiah Langhorne ..., 1725

Title from first line of text.

Programming EU External Action Post-Lisbon: New Opportunities or Business as Usual?

Over 90% of the external relations budget of the EU is processed through its external financial instruments. With the Lisbon Treaty and the creation of the new European External Action Service (EEAS), the institutional architecture of these instruments was significantly reformed. This contribution analyses strategic programming both pre- and post-Lisbon, identifies ‘winners’ and ‘losers’, and examines the potential of the new provisions to increase the coherence of EU external action. The examination shows that the instruments can be categorised into three groupings: ‘the big three’ comprising the bulk of funding characterised by joint programming and responsibilities; the ‘Commission-only’ instruments where all powers remain with the Commission; and the ‘EEAS-led rest’ in which the High Representative and the EEAS play a strong role but only have limited financial resources available. The new system calls for strong coordination of all involved actors in order to make it work. Findings of a case study on the Instrument for Stability reveal, however, that so far the establishment of the EEAS has not made a substantial impact on strategic programming in its first two years.

An historical sketch of the College of New Jersey.

Mode of access: Internet.

Beach changes at Long Beach Island, New Jersey, 1962-73 /

Beach profile line data collected from 32 profile sites along Long Beach Island, New Jersey. A total of 2,158 profile line surveys were examined, using empirical eigenfunction analysis and other measures of beach variability. Most profile lines have shown an accretionary trend since 1962 with rates between 2.3 and 0.24 meter per year in spite of erosion estimates due to sea level rise on the order of 0.68 meter per year. A great deal of variability in profile line change takes place along the beach, increasing from north to south, due to the location of profile lines relative to structures and offshore linear shoals. Detailed closely spaced profile lines taken over a year in a groin field near the north end of the island indicate littoral transport directions shift from north to south. Evidence of a littoral transport node near the north end of the groin field has been found. Net transport of the node is toward the south, but the rate could not be established due to lack of adequate wave data. Profile line variability within groin cells shows that single profile lines are not sufficient to determine the net change within a cell. The design of future beach monitoring studies should consider coastal structures, offshore bathymetry, the method of analysis, and the scales of processes under study. A coastal storm in November 1968 moved the MSL back as much as 22 meters; however, the beach recovered without artificial measures. The offshore bathymetry shows a series of shoreface-connected linear shoals at several locations along the island. Limited data show that these have remained stable and that most beach variability takes place in water shallower than 3 meters.

Beach changes at Atlantic City, New Jersey (1962-73) /

"March 1981."

Sand resources on the inner continental shelf off the central New Jersey coast /

"October 1982."

Conventional and advanced sewer design concepts for dual purpose flood and pollution control : a preliminary case study, Elizabeth, New Jersey /

Mode of access: Internet.

Rules of the District court of the United States for the district of New Jersey ; general, admiralty, bankruptcy, adopted January 1, 1933.

Mode of access: Internet.