Due to both bottom - boundary layer friction and interior adjustment,
this coastal current anomaly facilitates the movement of warmer deep water upward onto the continental shelf and toward the coast (see Figure).
The sea level anomaly creates an along - shelf geostrophic
coastal current anomaly, which is particularly strong on the western side of the Peninsula.
Not exact matches
Such as wildfire feedback,
coastal erosion, weather / atmospheric
anomalies, seasonal changes, species adaptation, ocean
currents etc..