As the epic El Nino of 2015-2016 continues to fade, this is a good time to analyze what impact it had on the multiyear drought across the western United States. Many Westerners were excited by the prospect of significant rain and snow that the strong episode of El Nino had been expected to bring during the fall and winter months. Although it did have a positive impact on parts of the drought-stricken west coast, it could have been more beneficial.
The U.S. Drought Monitor
Index Map from last October showed how extensive the drought conditions were in
the western United States. Since the
late fall and winter months are when the western United States expects to see additional
rainfall and snowfall, that’s a good benchmark to show how extensive the
drought conditions were prior to the arrival of the El Nino-influenced rainy
season.
Fast forward to the
current Drought Monitor Index map and you can see there was significant
improvement in the Pacific Northwest, which experienced a dramatic reduction in
the expanse of drought conditions. While
some dry conditions currently exist in parts of Oregon and Montana, the extreme
drought conditions are gone.
There is a simple way to
look at the impact the El Nino-influenced winter season of 2015-2016 had in
this by comparing the rainfall between this past winter and the previous,
non-El Nino winter of 2014-2015. From November 1, 2014
through May 31, 2015, Seattle, Washington had a rainfall deficit of 2.72”,
while from November 1, 2015 through April 30, 2016, Seattle had a rainfall
surplus of 11.35”. That’s a net swing of
more than 14 inches of rain in just one year.
Meanwhile, Portland, Oregon, had a rainfall deficit of 5.41” from
November 1, 2014 through May 31, 2015, while they had a rainfall surplus of
9.21” from November 1, 2015 through April 30, 2016. That’s a difference of more than 14.5 inches
of rain during the same period. Such a
dramatic difference between a non-El Nino season and a strong-El Nino winter
shows what an impact the El Nino event had.
Areas farther south
weren’t as lucky though. While San
Francisco had a rainfall surplus of less than one inch from November 1, 2015
through April 30, 2016, the cities of Los Angeles and San Diego have actually
seen larger rainfall deficits this winter compared to the 2014-2015 winter
season. That explains why the drought
conditions virtually disappeared in the Pacific Northwest while much of
California and Nevada remain in extreme to exceptional drought conditions.
The significant El Nino
episode this past winter helped enhance the precipitation in parts of the
western United States, but it didn’t bring the entire west coast the rainfall
it so desperately needs. The
southwestern United States can expect to see some isolated rainfall during the
summer monsoon season, but no widespread rainfall is on the horizon. That’s not good news as the dry summertime
heat builds across the desert regions of interior California and the
southwestern United States. Serving to
foreshadow the upcoming summer, Phoenix, Arizona saw its first 100-degree
temperature of 2016 this past week when it was 102 degrees on May 4.
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