The associated precipitation anomalies include above - average totals in the Gulf of Alaska extending into the Pacific Northwestern United States, and below - average totals over the upper Midwestern United States.
Not exact matches
To name just a few of the climate impacts of the annular modes: the NAM is
associated with large
anomalies in surface temperatures and
precipitation across North American and Eurasia, in the distribution of sea - ice throughout the Arctic, in sea - surface temperatures over the North Atlantic, and in the spatial distribution ozone in the lower stratosphere.
Interannual NAO and
associated SAT and
precipitation anomalies.
In particular, a stronger southern center - of - action of the NAO (i.e., a stronger high pressure
anomaly) and a northward shift of the SLP dipole nodal line is
associated with greater
precipitation deficits over southern and central Europe; and a southward shift of the nodal line accompanied by stronger anomalous westerly flow across northern Europe and Russia favors enhanced
precipitation and warming in these regions (Fig. 4).
The large interannual to decadal hydroclimatic variability in winter
precipitation is highly influenced by sea surface temperature (SST)
anomalies in the tropical Pacific Ocean and
associated changes in large - scale atmospheric circulation patterns [16].
Vector wind analyses were computed to explain the composite seasonal
precipitation anomaly results in terms of different circulation patterns
associated with these two wet groups.