East Asian summer monsoon (EASM) is one of the most dominant climate systems in East Asia. The anomalous EASM can cause extremely high temperatures, floods or drought. And the El Niño-Southern Oscillation (ENSO), the dominating mode in the tropical Pacific, is the most important factor affecting EASM. Understanding the processes for interannual to interdecadal variability of EASM-ENSO relationship is crucial.
Owing to the limited period of observational data, the related studies of decadal or multidecadal variation of ENSO and EASM have their own drawbacks. Therefore, climate model becomes an important tool.
Using a coupled climate model with a 1000-year simulation, scientists from CAS Institute of Atmospheric Physics investigated the multidecadal variations of the EASM-ENSO interannual relationship.
Schematic representation of the Sea Surface Temperature (sst) anomalies over the Indian Ocean and the western tropical Pacific and western North Pacific anomalous anticyclone (WPAC) in the decaying summer of El Niño events. Credit: Institute of Atmospheric Physics
The EASM-ENSO interannual relationship is found to have experienced multidecadal variations. During periods with a significant ENSO-EASM relationship, the ENSO-related circulation anomalies show a Pacific-Japan (PJ)-like pattern with significant wave activity flux propagating from the tropics to the north in the lower troposphere, and from the mid-latitudes to the south in the upper troposphere.
The resulting ENSO-related precipitation anomalies are more (less) than normal over the East Asia (Western North Pacific) in the decaying summers of El Niño events. In contrast, the circulation and precipitation anomalies are weak over East Asia-western North Pacific during the periods with a weak ENSO-EASM relationship.
"The main reason for the multidecadal variations of ENSO-EASM relationship is the amplitude discrepancy of SST anomalies over the Indo-western Pacific Ocean," says HUANG Gang, the corresponding author of the study. "And the discrepancy, in turn, leads to the intensity difference of the western North Pacific anomalous anticyclone and related climate anomalies over the East Asia-Western North Pacific."
Source: Chinese Academy of Sciences
Featured image: Floods around Bangkok, Thailand on October 24, 2017. Credit: DVIDSHUB
If you value what we do here, create your ad-free account and support our journalism.
Producing content you read on this website takes a lot of time, effort, and hard work. If you value what we do here, select the level of your support and register your account.
Your support makes this project fully self-sustainable and keeps us independent and focused on the content we love to create and share.
All our supporters can browse the website without ads, allowing much faster speeds and a clean interface. Your comments will be instantly approved and you’ll have a direct line of communication with us from within your account dashboard. You can suggest new features and apps and you’ll be able to use them before they go live.
You can choose the level of your support.
Stay kind, vigilant and ready!