Ecology, Climate Change and Related News

Ellie Cohen, President and CEO, Point Blue Conservation Science

Drought and Climate Change

Leave a Comment

 

 

Study connects man-made global warming to ongoing California drought, winter’s polar vortex

Associated Press April 24, 2014 By SETH BORENSTEIN, AP Science Writer WASHINGTON (AP) —   While researchers have sometimes connected weather extremes to man-made global warming, usually it’s not done in real time. Now a study is asserting a link between climate change and both the intensifying California drought and the polar vortex blamed for a harsh winter that mercifully has just ended in many places. The Utah State University scientists involved in the study say they hope what they found can help them predict the next big weird winter. Outside scientists, such as Katharine Hayhoe at Texas Tech University, are calling this study promising but not quite proven as it pushes the boundaries in “one of the hottest topics in climate science today.” The United States just came out of a two-faced winter — bitter cold and snowy in the Midwest and East, warm and severely dry in the West. The latest U.S. drought monitor says 100 percent of California is in an official drought. The new study blames an unusual “dipole,” a combination of a strong Western high pressure ridge and deep Great Lakes low pressure trough. That dipole is linked to a recently found precursor to El Nino, the world-weather changing phenomenon. And that precursor itself seems amplified by a build-up of heat-trapping greenhouse gases, the study says. It’s like a complex game of weather dominos that starts with cold water off China and ends with a devastating drought and memorable winter in the United States, said study author Simon Wang, a Utah State University climate scientist. Wang was looking at colder water off China as a precursor to an El Nino. The colder water there triggers westerly winds in the tropical Pacific. Those westerly winds persist for several months and eventually push warmed up water and air to the central Pacific where an El Nino forms, Wang said. An El Nino is a warming of the central Pacific once every few years, from a combination of wind and waves in the tropics. It shakes up climate around the world, changing rain and temperature patterns. Wang saw the precursors and weather event coming months before federal weather officials issued an official El Nino watch last month. Then Wang noticed the connection between that precursor — cold water off China, Vietnam and Taiwan — and the recent wild winter. He tracked similar combinations of highs and lows in North America. And he found those combination extremes are getting stronger. Wang based his study, soon to be published in the journal Geophysical Research Letters, on computer simulations, physics and historical data. It is not as detailed and doesn’t involve numerous computer model simulations as more formal attribution studies. Still, Wang said his is a proper connection. Wang compared computer simulations with and without gases from the burning of fossil fuels. When he included carbon dioxide from fossil fuel use, he got a scenario over the past few decades that mirrored what has happened, including this past weird winter and other worsening dipole conditions. When he took out the greenhouse gases, the increasing extremes actually went down — not what happened in real life…..

 

Probable causes of the abnormal ridge accompanying the 2013-14 California drought: ENSO precursor and anthropogenic warming footprint

S.-Y. Simon Wang1,2,*, Lawrence Hipps2,  Robert R Gillies1,2 and Jin-Ho YoonGeophysical Research Letters DOI: 10.1002/2014GL059748 ©2014. American Geophysical Union. All Rights Reserved.

Abstract

The 2013-14 California drought was accompanied by an anomalous high-amplitude ridge system. The anomalous ridge was investigated using reanalysis data and the Community Earth System Model (CESM). It was found that the ridge emerged from continual sources of Rossby wave energy in the western North Pacific starting in late summer, and subsequently intensified into winter. The ridge generated a surge of wave energy downwind and deepened further the trough over the northeast U.S., forming a dipole. The dipole and associated circulation pattern is not linked directly with either ENSO or Pacific Decadal Oscillation; instead it is correlated with a type of ENSO precursor. The connection between the dipole and ENSO precursor has become stronger since the 1970s, and this is attributed to increased GHG loading as simulated by the CESM. Therefore, there is a traceable anthropogenic warming footprint in the enormous intensity of the anomalous ridge during winter 2013-14, the associated drought and its intensity.

Leave a Reply

Your email address will not be published. Required fields are marked *

You may use these HTML tags and attributes: <a href="" title=""> <abbr title=""> <acronym title=""> <b> <blockquote cite=""> <cite> <code> <del datetime=""> <em> <i> <q cite=""> <strike> <strong>