The North Atlantic is a peculiarly convective ocean. The convective renewal of intermediate
and deep waters in the Labrador Sea and Greenland/Iceland Sea both contribute …

A synthesis and review of the physical oceanography of the GIN Sea (Greenland, Iceland
and Norwegian Seas) is presented. An accompanying bibliography is included from 1972 …

Salinity stratification is critical to the vertical circulation of the high‐latitude ocean. We here
examine the control of the vertical circulation in the northern seas, and the potential for …

The evidence for the Little Ice Age, the most important fluctuation in global climate in
historical times, is most dramatically represented by the advance of mountain glaciers in the …

The widespread freshening of the upper 500–800m layer of the northern North Atlantic,
which this paper describes, represents one of the most persistent and extreme variations in …

This paperback edition is sold subject to the condition that it shall not, by way of trade or
otherwise, be lent, resold, hired out, or otherwise circulated without the publisher's prior …

Abstract The North Atlantic Oscillation (NAO) and Southern Oscillation (SO) are compared
from the standpoint of their association with Northern Hemisphere winter mean distributions …

We revisited the “Great Salinity Anomaly” of the 1970s (GSA'70s; Dickson et al., 1988) and
documented the newly identified “Great Salinity Anomaly” of the 1980s (hence termed …

Salient features of the long‐term variation of surface air temperature for India as a whole and
for different regions of the country have been presented. Temperature data at 73 fairly …

Cai, W., J. Syktus, HB Gordon, and S. O'Farrell, 1997: Response of a global coupled ocean–
atmosphere–sea ice climate model to an imposed North Atlantic high-latitude freshening. J …