Skip to main content Skip to footer unit links
167 posts in Climate Matters

Winter Preview: What Can We Expect?

As many of our readers are likely well aware, there is a high likelihood (between 60 and 65% chance) of a weak El Niño developing during the fall and winter. Sea-surface temperature anomalies are above normal throughout the equatorial Pacific Ocean at the time of this writing (more information in the Climate Outlook below), but the predicted El Niño has been slow to start. 

Read more

Growing Hops in Washington State

Due to the passage of I-502 by Washington state voters in November 2012, legal agricultural production has commenced for a notorious member of the family Cannabacaeae. This highlight is about another member of this family that WA state is known for and that is hops (Humulus lupulus). 

Read more

The Precipitation Winners and Losers in Major League Baseball

Seattle’s rainy reputation is difficult to combat, especially among those that have never lived in the Pacific Northwest. The dry Washington summers are often overlooked. In that context, OWSC was pleased to have recently heard a “rumor” that during the regular baseball season, Seattle is one of the driest cities of those that have a Major League Baseball team. 

Read more

Extreme Precipitation Events in Washington State

There has been a slight upward trend in mean precipitation for Washington state over the last century or so, but this change is marginal from the standpoint of statistical significance.  Readers are encouraged to explore this for themselves using an application on the OWSC website: www.climate.washington.edu/trendanalysis. 

Read more

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. 

Read more
Back to Top