The mean dynamic topography (MDT, in cm) of the world’s oceans in the highest resolution ever achieved from space-based data. MDT is calculated by taking the mean sea-surface height measured by satellites like Envisat, and subtracting the gravity model from GOCE. Red areas show where water levels are above the surface of the gravity model, while blue depicts areas where the water is below. From this, scientists calculated the speed of ocean currents.