Jack Pymble refuses to help export firearms illegally from Australia to New Guinea. A mobster threatens him—Jack accidentally kills the man, and suddenly he's on the run. Mysterious Susan Carter convinces Pymble to fight back. Infatuated by her sexuality, he agrees. There's an arms dealer's meeting—their only opportunity to untangle the mess—in New Guinea, thousands of miles away... Chased by both the mob and the cops, they go for it, using motorcycles, a coach, a stolen car, a prawn trawler and a helicopter. They burst open a plot to seize vast mineral resources...but will they die before they can talk? Genre: Thriller/Suspense Don't miss the sequel: TRAPPING JUDAS [A PROFILE THREE THRILLER]

In the sequel to PROFILE THREE, find out what Susan Carter and newly-trained agent Jack Pymble get tangled up in when they take on their next assignment.The world of heroin trafficking seethes with money and sadism. Penetrating that scene with the intent of breaking open just a small part of it is a difficult, frightening, dangerous job. It's also astonishingly complicated. Discover just how complicated it can be as an operation across the Top End of Northern Australia slowly develops. Don't miss the first incredible book: PROFILE THREE [A PROFILE THREE THRILLER]

The long shore current maximum observed in the trough of a barred beach during the nearshore dynamics experiment DELILAH at Duck, North Carolina, is not predicted by present theory. The simplest longshore curren models balance cross-shore changes in the alongshore wave momentum (radiation stress) with the alongshore bottom shear stress. Waves break over the bar, reform in the trough and again break on the foreshore resulting in changes in the radiation stress, which predicts two jets, one over the bar and the other at the foreshore, which does not agree with the observed current maximum in the trough. The advection of the momentum of the longshore current by mean cross-shore currents as a source of momentum mixing is investigated. The longshore current is strongest toward the surface and decreasing to zero at the bottom. The cross-shore mean current has an onshore transport in the wave crest/trough region and an offshore transport beneath (undertow). The net interaction can induce significant lateral mixing of the alongshore momentum of the mean currents, which is shown using a simplified three- dimension model of nearshore currents to explain much of the differences with observations.

Atlases accompany 1885-1891, 1894,1895, 1897-1904.