Seasonal Mixing Processes in an Arctic Fjord System

摘要: Abstract Studies of water movement in the Aafardlikavsâ/Qaumarujuk fjord system West Greenland have barn carried out order to understand mine tailings discharged into Agfardlikavsâ Fjord. Observations are explained terms resonance internal tide, deep convection associated with sea ice growth, and basin exchange occurring at time breakup early summer. Mixing processes dominated by these events, illustrating limitations any seasonal description based on conventional diffusive processes.