Boundary current a basin (such as the Gulf Stream, a current on the western side of the Atlantic Ocean) are stronger than those on the eastern boundary (such as the California Current, on the eastern side of the Pacific Ocean). Western intensification was first explained by the American oceanographer Henry Stommel. In 1948, Henry Stommel published a paper in "Transactions, American Geophysical Union" titled "The Westward Intensification of Wind-Driven Ocean Currents", in which he used a simple, homogeneous, rectangular ocean model to examine the streamlines and surface height contours for an ocean at a non-rotating frame, an ocean characterized by a constant
Ocean Pier Railway at Atlantic City Ocean Pier Railway at Atlantic City The Ocean Pier Railway at Atlantic City was an electric narrow gauge railway, which ran over the entire length of the Ocean Pier in Atlantic City, about into the ocean. The Ocean Pier at Atlantic City was extended by in 1896/97. At the same time it was widened, and the railway, a fishing platform and several pavilions were built. The gauge of the railway was . At the shore loop the distance between the inner rails was , which necessitated a very sharp curve. The loop at the ocean end was broader and permitted