macd
Well-Known Member
Anyone who's experienced a blow in the Mediterranean will know how rapidly the seas build, and how frighteningly steep they can quickly become.
I've never encountered a convincing argument as to why this should be so, but recently noticed an observation in the pilot book for Corsica and N Sardinia. In it the author, John Marchment, writes that:
"...the sea is much saltier than the Atlantic Ocean, which increases the surface tension and the surface wind effect...this surface tension effect also helps to account for the incredibly swift build-up of seas". He goes on to include their steepness as part of the same process.
I was a little sceptical of this and consulted Cap'n Google. All I was able to come up with was that surface tension is indeed a factor in the generation of 'capillary waves', but these are typically less than 2cm in length (such as cat's paws?). The process of generating larger waves goes way beyond this, and no measure of surface tension seems to figure in it.
Any thoughts?
I've never encountered a convincing argument as to why this should be so, but recently noticed an observation in the pilot book for Corsica and N Sardinia. In it the author, John Marchment, writes that:
"...the sea is much saltier than the Atlantic Ocean, which increases the surface tension and the surface wind effect...this surface tension effect also helps to account for the incredibly swift build-up of seas". He goes on to include their steepness as part of the same process.
I was a little sceptical of this and consulted Cap'n Google. All I was able to come up with was that surface tension is indeed a factor in the generation of 'capillary waves', but these are typically less than 2cm in length (such as cat's paws?). The process of generating larger waves goes way beyond this, and no measure of surface tension seems to figure in it.
Any thoughts?