These are based on the full set of moving tie points that are tracked from week to week throughout the entire basin of the Arctic Ocean. The initial spacing of the tie points, at fall freeze-up, is 5 km. This initial grid, consisting of approximately half a million 5 x 5 km cells, then moves and deforms with the ice cover. Therefore these products are "Lagrangian": they are computed following the same tie points or cells. The number following each product is the size in megabytes of the weekly data set.
These are interpolated from the basic products to a fixed, 50 km grid. Therefore these products are "Eulerian": they apply to fixed regions of space. The number following each product is the size in megabytes of the weekly data set.
For more details, see Sections 4 and 5 of the RGPS Description by Ron Kwok.
For technical questions about RGPS products, contact Ron Kwok.