Heavy rain over the Indian Ocean and Southeast Asia and the eastern Pacific Ocean is a good indicator that temperatures in central California will reach 100°F in four to 16 days, according to a collaborative research team from the University of California Davis and the Asia-Pacific Economic Cooperation (APEC) Climate Center in Busan, South Korea.
The results were published in Advances in Atmospheric Sciences on April 12, 2019.
The cover image shows links between unusually strong tropical convection and extreme California heat waves. The outgoing longwave radiation anomaly is shaded blue for unusually cold temperatures at the tops of thunderstorms and red where clouds are suppressed and temperatures are unusually warm. Indian Ocean convection is strong on about 1/6 of all days within the two weeks before extreme California heat starts; that convection is measured by the Madden-Julian Oscillation (MJO) phases 2 and 3. Similarly, California heat waves follow convection west of Central America (MJO phases 8 and 1) on nearly 1/3 of those days.
Heat waves are common in the Central California Valley, the 50-mile-wide oval of land that runs 450 miles from just north of Los Angeles up to Redding. The valley is home to half of the nation's tree fruit and nut crops, as well as extensive dairy production, and heat waves can wreak havoc on agricultural production. The dairy industry had a heat wave-induced economic loss of about $1 billion in 2006, for instance. The ability to predict heat waves and understand what causes them could inform protective measures against damage.
We want to know more about how extreme events are created, said Richard Grotjahn, corresponding author on the paper and professor in the Department of Land, Air and Water Resources at the University of California Davis. We know that such patterns in winter are sometimes linked with areas of the tropics where thunderstorms are enhanced; we wondered if there might be similar links during summer for those heat waves.
The scientists analyzed the heat wave data from June through September from 1979 to 2010. The data were collected by 15 National Climatic Data Centers stations located throughout the Valley. From these data, the researchers identified 24 heat waves. They compared these instances to the phases of a large, traveling atmospheric circulation pattern called the Madden-Julian Oscillation (MJO).
The MJO manifests as heavy rain that migrates across the tropical Indian and then Pacific Oceans, and researchers have shown that it influences winter weather patterns.
It's well known that tropical rainfall, such as the MJO, have effects beyond the tropics, said Yun-Young Lee of the APEC Climate Center in Busan, South Korea. She is the paper's first author. So, a question comes to mind: [is] hot weather in the Central California Valley partly attributable to tropical rainfall?
Lee and Grotjahn found that, yes, enhanced rainfall in the tropics preceded each heat wave in specific and relatively predictable patterns. They also found that hot weather in the Valley is most common after more intense MJO activity in the eastern Pacific Ocean, and next most common after strong MJO activity in the Indian Ocean.
The more we know about such associations to large-scale weather patterns and remote links, the better we can assess climate model simulations and therefore better assess simulations of future climate scenarios, Grotjahn said.
This work was supported by the National Science Foundation, the National Aeronautics and Space Administration, the Department of Energy Office of Science, the United States Department of Agriculture's National Institute of Food and Agriculture, and the APEC Climate Center in the Republic of Korea.