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The Arctic Oscillation and Pacific Northwest Weather

The Arctic Oscillation (AO), also known as the Northern Annular Mode (NAM), is an important element of the variability in the weather and climate of the Northern Hemisphere. It relates fundamentally to the state of the flow at northern latitudes, with the positive phase associated with a strong, axisymmetric polar vortex and the negative phase associated with a weak polar vortex, allowing for more prominent large-scale ridges and troughs for the whole hemisphere. 

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Western WA Heat Waves

As we enter the summer months, it is timely to discuss a research paper that was recently published in the Journal of Applied Meteorology and Climatology (Bumbaco et al. 2013). OWSC collaborated with the Oregon Climate Service at Oregon State University to examine the historical record of heat waves occurring west of the Cascade Mountains in both Washington and Oregon. 

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A Review of Winter 2012-2013

During September and October 2012, seasonal forecasts were indicating an increased likelihood of a drier and warmer winter than usual in Washington State due to the projected development of an El Niño in the tropical Pacific Ocean. 

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