The omega equation method based on an equivalent isobaric geopotential heig
ht in sigma coordinates has been used to retrieve the precipitation over Gr
eenland. This approach is designed to accurately represent the topographic
effects of the Greenland Ice Sheet on atmospheric motion and precipitation.
The 11 year mean precipitation from 1985 to 1996 over all of Greenland is
376 mm yr(-1), which is close to the long-term mean precipitation of 346 mm
yr(-1) estimated from glaciological data. The precipitation over all of Gr
eenland shows that the largest value in 1986 is 472 mm yr(-1) and the small
est value in 1995 is 309 mm yr(-1). The major interannual variability of th
e atmospheric circulation in the North Atlantic can be represented by the v
ariation of the North Atlantic Oscillation (NAO) index, which is most prono
unced during winter. It is found that if the NAO index increases, the total
precipitation over Greenland decreases, and vice versa. The correlation co
efficient between these two series for 1985-1995 is -0.75. The mean precipi
tation over southern Greenland, where the majority of precipitation falls,
is more closely related to the NAO index in winter, and their correlation c
oefficient is -0.80. This relationship can be understood from the composite
maps of sea level pressure and Greenland precipitation for the high and lo
w index months. During months of high NAO index values, the Icelandic Low i
s strong. During months of low NAO index values, the monthly mean low is lo
cated to the southwest of Greenland over the Labrador Sea. Precipitation am
ounts over the southeast coast of Greenland are about 100 mm larger during
the low NAO index months than the high NAO index months. Precipitation over
all of Greenland during the low NAO index months is higher. There are sign
ificant downward trends in annual precipitation from 1985-1995 for all of G
reenland and its southern and central west coastal regions, amounting to ab
out 3% per year.