Hunt n' Fish wrote:
Thank you very much Capt Len and the rest of you for offering such a great "How To" here. I appreciate it.
Jigalow wrote:
Halfseas wrote:
The warmer, salinate/ heavier gulf water will push under the cooler, desalinated/ lighter Labrador current water.
sorry but this part doesn't make sense to me. I've always understood the warm water floats on top of the colder water, you're saying it's the other way around?
Yes, colder water is denser than warm water and would, under normal circumstances, be lower in the column, but the pertinent part of the discussion you missed was:
Halfseas wrote:
The warmer, salinate/ heavier gulf water will push under the cooler, desalinated/ lighter Labrador current water.
Saltwater is denser than freshwater. Even warm saltwater is denser than cold freshwater. So apparently Gulf Stream water has a higher salinity (maybe due to more evaporation in the Southern climates?) than the Northern surface currents, and is more dense, and pushes under the cold water?
The most dense water in the world occurs where the ice caps form, and take the fresh water out of the sea to form ice, and the excess salt and extremly cold waters sink to the ocean bottom and form currents much like the surface warm water currents and bring nutrient rich upwellings when they collide with sea mounts, etc.
Chris
Thanks Chris
Because of the driving force a warm eddy creates that pushes north, along with the depth and size of the warm eddy, warm water can be driven under the cold water only to eventually rise to the surface up on the flats inside the 100 fathom line. This water can pop up 2 to 10 miles inshore of the 100. KEEP YOUR EYES OPEN FOR LIFE inside the shelf and watch the water for color, & temp.
This post edited by CaptLen 05:44 PM 05/11/2008