1 Introduction
Oil exploration in the deep Gulf of Mexico is vulnerable to hazards due to strong currents at the fronts of highly nonlinear warm-core eddies [38]. The dynamics in the Gulf of Mexico are indeed dominated by the powerful northward Yucatan Current flowing into a semi-enclosed basin. This current forms a loop, called the Loop Current, that exits through the Florida Straits, and in turn merges with the Gulf Stream. At irregular intervals, the loop current sheds large eddies that propagate westward across the Gulf of Mexico. This eddy shedding involves a rapid growth of nonlinear instabilities [3], and the occasional eddy detachment and reattachment make it very difficult to clearly define, identify, monitor, and forecast an eddy shedding event [2], [4], [11]. A selected time step of an ocean forecasting ensemble computed for the Gulf of Mexico is visualized via the mean surface of the ensemble (center). for a more detailed inspection of the entire distribution of the surfaces comprising the ensemble, we provide two linked views. the first linked view (left) shows a histogram of depth positions of the surfaces at a selected spatial position and time step. The second linked view (right) is a time-series view that depicts a glyph for each time step at the selected position. the horizontal line corresponds to a chosen critical sea level, where each glyph's color depicts the risk corresponding to how much of the distribution is above that critical level