We report on an abrupt springtime temperature rise (ASTR) occurring over the Greenland ice cap. The abrupt 12¿--15 ¿C temperature rise typically occurs in May over a 24--36 hour period and is accompanied by a 16--22 hPa pressure rise that begins 2--3 days earlier. The Greenland ASTR is examined using composites of pressure and temperature data from Automatic Weather Stations at Cathy and Kenton for the years 1987 through 1990 and 1992 and 1993. Comparative analysis of the ASTR at coastal weather stations is made and contemporaneous atmospheric circulation variations are examined with gridded hemispheric sea level pressure and 500 hPa data. At the ice cap summit the ASTR is accompanied by an average 360 m rise in 500 hPa geopotential heights, strong surface winds, and high relative humidities. During an ASTR, concomitant air temperatures along the western coast of Greenland and on Baffin Island also rise, but with a magnitude only half that at the ice cap summit. The contemporaneous ASTR pressure rise at coastal stations is of equivalent magnitude to that at the summit and is most prominent at Greenland stations and on Iceland. Evidence is presented that the ASTR is linked to a seasonal readjustment in the regional Atlantic atmospheric circulation in which the westerlies become weakest in May and migrate northward into the Arctic. A meridional flow regime is established with southwesterly flow advecting mild air over Greenland. Blocking highs form over the Atlantic and the surface mean Icelandic low is weak, or replaced by mean high pressure. The nature and timing of the ASTR is important for planning field activities on the Greenland ice sheet. Further study of the ASTR should lead to a better understanding of boundary layer processes over the ice sheet.¿ 1997 American Geophysical Union