SURFACE TEMPERATURE GRADIENTS AS INDICATORS OF THE POSITION OF THE GULF STREAM
Abstract
The possibility of determining the position of the Gulf Stream from an examination of surface temperature gradients was investigated. A comparison was made of the surface, 100-m, and where possible, 200-m temperatures from 99 BT sections across or well into the Gulf Stream. Agreement between surface and deep temperature gradients was good for the main currents of the Stream from November to May; however, at no season of the year did surface temperature gradients in the slope water inshore of the Gulf Stream reliably reflect those in deep water.
Document Details
- Document Type
- Technical Report
- Publication Date
- Jul 01, 1953
- Accession Number
- AD0016499
Entities
People
- S. L. Strack
Organizations
- Woods Hole Oceanographic Institution