Continental
scale precipitation variations.
Not exact matches
On decadal time
scales, annual streamflow
variation and
precipitation are driven by large -
scale patterns of climate variability, such as the Pacific Decadal Oscillation (see teleconnections description in Climate chapter)(Pederson et al. 2011a; Seager and Hoerling 2014).
As discussed in the Climate chapter, large -
scale atmospheric circulation patterns connected to changes in sea - surface temperatures strongly influence natural
variations in
precipitation and temperature (e.g., Cayan et al. 1999; Mantua and Hare 2002).
For example, deficiencies remain in the simulation of tropical
precipitation, the El Niño - Southern Oscillation and the Madden - Julian Oscillation (an observed
variation in tropical winds and rainfall with a time
scale of 30 to 90 days).
southern oscillation a large -
scale atmospheric and hydrospheric fluctuation centered in the equatorial Pacific Ocean; exhibits a nearly annual pressure anomaly, alternatively high over the Indian Ocean and high over the South Pacific; its period is slightly variable, averaging 2.33 years; the
variation in pressure is accompanied by
variations in wind strengths, ocean currents, sea - surface temperatures, and
precipitation in the surrounding areas
A set of long, nearly complete daily
precipitation series for Alaska spanning the latter half of the 20th century has been analyzed for seasonal relationships between
variations in mean, heavy, and extreme
precipitation and large -
scale atmospheric circulation
variations at interannual, decadal, and secular timescales.