Complete evaluation of air-sea heat exchange and vertical ocean temperature structure by Claudio Iturra
Enter parameters and calculate to see comprehensive heat flux analysis
Direct heat transfer due to temperature differences between air and sea surface, enhanced by wind speed and atmospheric stability
Heat transfer through evaporation/condensation, strongly dependent on humidity gradients and wind conditions
Shortwave radiation penetration, affected by cloud cover, solar angle, and water turbidity in coastal areas
Thermal radiation exchange between ocean surface and atmosphere, influenced by cloud cover and atmospheric moisture
Coastal oceans exhibit unique heat exchange patterns due to: