Abstract
Two temperature sections across the track of Typhoon Shirley (September 1965) in the vicinity of the Kuroshio are shown. The first is based on observations made less than a week before the storm and the second within two days after its passage. The comparison shows: (1) maximum cooling of more than 3°C directly under the eye of the storm; (2) upwelling of 20–25 m on the seaward side of the eye but very little on the inshore side; (3) a slight increase in the depth of the mixed layer; and (4) some evidence that upwelling continued for at least a day after the storm passed. Heat loss to the atmosphere is estimated at 1000 to 3000 cal/cm2. DOI: 10.1111/j.2153-3490.1969.tb00454.x

This publication has 2 references indexed in Scilit: