Having analyzed a global grid temperature anomaly data set and some sea lev
el pressure data during the last century, we round the following facts. Fir
stly, the annual temperature change with a warming trend of about 0.6 degre
esC / 100 years in the tropical area over Indian to the western Pacific Oce
ans was most closely correlated to the glob:ll mean change. Therefore, the
temperature change in this area might serve as an indicator of global mean
change at annual and longer time scales. Secondly, a cooling of about -0.3
degreesC / 100 years occurred over the northern Atlantic. Thirdly, a two-wa
ve pattern of temperature change, warming over northern Asia and northweste
rn America and cooling over the northern Atlantic and the northern Pacific,
occurred during the last half century linked to strengthening westerlies o
ver the northern Atlantic and the weakening Siberian High. Fourthly. a rema
rkable seasonal difference occurred over the Eurasian continent, with cooli
ng (warming) in winter (summer) during 1896-1945. and warming (cooling) in
winter (summer) during 1946-1995. The corresponding variations of the North
Atlantic Oscillation and the Southern Oscillation were also discussed.