The effects of rainfall structure and atmospheric circulation variability o
n streamflow in the Alzette River basin (Grand Duchy of Luxembourg, Europe)
were investigated. Evidence is presented regarding the local-scale sensiti
vity of the Alzette River basin to large-scale changes in atmospheric circu
lation. Since the 1950s, there has been a marked increase in the contributi
on of the westerly component of atmospheric circulation to rainfall. These
changes in atmospheric circulation are on a par with an increase in rainfal
l intensity and duration, which has induced a significant increase in the w
inter maximum daily storm Row in the Alzette River basin since the 1970s.