The El Niño – Southern Oscillation correlates well with cloud-to-ground lightning in the following summer in China
Large-scale circulation anomalies are a key factor in the transportation of water vapour and changes in climate.
For tropical and subtropical regions, an atmospheric circulation field not only determines the characteristics of the weather situation but also influences the atmospheric circulation in the middle and high latitudes, as well as the global climate, through the transport of energy and angular momentum.
At the same time, whilst lightning can serve as a global tropical ‘thermometer’ and an indicator of water vapour in the upper troposphere, the driving role of the circulation situation for it needs to be further analysed.
In a paper, Professor Xiushu Qie and Dr Mingyi Xu from the Key Laboratory of Middle Atmosphere and Global Environment Observation, Institute of Atmospheric Physics, Chinese Academy of Sciences, attempt to address this issue.
They present new evidence for El Niño – Southern Oscillation (ENSO) correlating well with following-summer cloud-to-ground lightning in China.
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Firstly, the time-lagged correlation between monthly cloud-to-ground lightning anomalies over China’s land areas (2010 – 2020) and the Oceanic Niño Index (the main index for tracking the oceanic part of ENSO) was analysed.
Qie explained: “Interestingly, the correlation coefficients, which were statistically significant at the 90% confidence level, revealed good correlation between ENSO and subsequent cloud-to-ground lightning in China.
In addition, the ENSO phenomenon – especially La Niña events – correlate well with subsequent cloud-to-ground lightning flashes in land areas of China.
“When the sea surface temperature anomaly caused by ENSO is more obvious, the spatial distribution characteristics of cloud-to-ground lightning are also more obvious.”
When the sea surface temperature of the east Pacific Ocean and Indian Ocean warms abnormally and the sea surface temperature of the northwest Pacific becomes abnormally cold, a cyclonic circulation is stimulated over the Yellow Sea, East China Sea, and tropical west Pacific region of China, thereby enhancing the easterly wind on the north side and the westerly wind on the south side, bringing water vapour from the northwest Pacific to north China and northeast China.
Affected by the abnormally high pressure, the corresponding cloud-to-ground lightning activities in north China and northeast China are weak.
However, the water vapour then moves southwards, where it converges with water vapour derived from the Bay of Bengal in south China, and ascending motion strengthens here, thus enhancing the cloud-to-ground lightning activity of this area.
As the water vapour continues to move southwards, the water vapour divergence and descending motion in southern Guangdong give rise to weak cloud-to-ground lightning activities there.
Xu added: “Therefore, the ENSO phenomenon might serve as a climatic driver of subsequent cloud-to-ground lightning activity occurring over the land areas of China.”
The research is published in Atmospheric and Oceanic Science Letters.
Image: Double-termination negative cloud-to-ground lightning captured by high-resolution camera (Binzhou, China). © Key Laboratory of Middle Atmosphere and Global Environment Observation (LAGEO), IAP, CAS, Beijing, China.