What explains the difference in wind direction between the surace and the upper atmosphere in the tropial paific near Hawaii?

The difference in wind direction between the surface and the upper atmosphere in the tropical Pacific near Hawaii is primarily due to the Earth's rotation and the influence of the trade winds. At the surface, the trade winds blow from the east to the west due to the Coriolis effect, while in the upper atmosphere, winds generally move from west to east in the subtropical jet stream. This contrast is also influenced by temperature gradients and the presence of high and low-pressure systems. As a result, these dynamics create a distinct difference in wind patterns at various altitudes.