Tranzition Zone Chlorophyll Front
The North Pacific Transition Zone Chlorophyll Front (TZCF) is a dynamic, basin-wide feature characterized by rapidly changing chlorophyll concentrations, temperature, and nutrients, marking a boundary between subtropical and subarctic phytoplankton communities, and influencing marine ecosystems and fisheries.
Here's a more detailed explanation:
- The TZCF is a zone of surface convergence where cool, vertically mixed, high chlorophyll water on the north side sinks beneath warm, stratified, low chlorophyll water on the south side.
- It spans the east-west extent of the North Pacific and moves seasonally northward and southward within the North Pacific Transition Zone between 30°N and 45°N.
- In the fall and winter, the TZCF moves southward, potentially due to strong winds moving nutrients across the boundary between gyres.
- In the spring, winds lessen and nutrient transport southward is reduced, causing the TZCF to move northward, reaching its most northerly position in the summer.
- In the fall and winter, the TZCF moves southward, potentially due to strong winds moving nutrients across the boundary between gyres.
- The TZCF is an important ecological and economic demarcation in the Northern Pacific, associated with migrating predators like tuna, loggerhead turtles, and squid.
- Changes in its position can alter the spatial distribution of marine animals.
- The TZCF supports enhanced phytoplankton net community production.
- The TZCF is an important ecological and economic demarcation in the Northern Pacific, associated with migrating predators like tuna, loggerhead turtles, and squid.
- The front is easily monitored with ocean color satellite remote sensing. Ongoing research continues to advance our understanding of the physics and biology of the TZCF.
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