North Atlantic Oscillation: verschil tussen versies
|Regel 47:||Regel 47:|
[[Category:Climate changeand ]]
Huidige versie van 22 jul 2019 om 15:57
The North Atlantic Oscillation (NAO) is a weather phenomenon in the North Atlantic Ocean of fluctuations in the difference of atmospheric pressure at sea level (SLP) between the Icelandic Low and the Azores High .
Through fluctuations in the strength of the Icelandic low and the Azores high, the North Atlantic Oscillation controls the strength and direction of westerly winds and location of storm tracks across the North Atlantic. A permanent low-pressure system over Iceland (the Icelandic Low) and a permanent high-pressure system over the Azores (the Azores High) control the direction and strength of westerly winds into Europe. A large difference in the pressure at the two stations (a high index year, denoted NAO+) leads to increased westerlies and, consequently, cool summers and mild and wet winters in Central Europe and its Atlantic facade. In contrast, if the index is low (NAO-), westerlies are suppressed, northern European areas suffer cold dry winters and storms track southwards toward the Mediterranean Sea. This brings increased storm activity and rainfall to southern Europe and North Africa .
The NAO exhibits considerable interseasonal and interannual variability, and prolonged periods (several months) of both positive and negative phases of the pattern are common (Fig. 1). The wintertime NAO exhibits clusters of positive and negative NAO winters (Fig.2). Data analysis techniques have revealed a weak 8-year periodicity.