Lably
Skip to content

2017 California floods

2017 regional natural disaster event

  • 7 min read
  • 3 chapters

Related on Lably

Through Groundwater

The flooding occurred at the end of one of California's worst droughts on record, and much of the state was unprepared to handle the huge volume of rain and snow. The precipitation helped to refill surface water supplies, including many major lakes and reservoirs, but had limited impact on groundwater reserves. Governor Jerry Brown declared the drought officially over on April 4, 2017.

Background

The high-amplitude ridge off the West Coast that characterized the 2011–17 California drought, dubbed the "Ridiculously Resilient Ridge", was replaced by a persistent presence of anomalous troughs affected California. Another feature in the 2013–2015 winters was the extreme temperature contrast between a warm western U.S. and a cold eastern continent. These anomalous temperature and circulation patterns were referred to as the North American winter “dipole”. The dipole basically describes the wintertime stationary waves over North America, which contribute to the mean temperature difference between the climatologically warmer western U.S. and colder eastern half. Therefore, an amplification of the stationary wave would enhance such a temperature difference, like in the 2013-2015 winters, while a weakening of the stationary wave would reverse the situation, like in the 2016–2017 winter. Indeed, in winter 2016–2017 this dipole was apparently reversed.

Sign in to keep reading

2 more chapters are free with a Lably account.

More in Earth science