03 · formed机理与大气环流 About 8 min read (2810 words) · Back to Wiki Index

How Do El Niño and La Niña Affect Typhoons? Understanding the Seasonal Pattern

Key SummaryIn El Niño years, typhoons tend to form farther east, reach greater intensity, and experience more Fujiwara interactions; in La Niña years, they tend to form farther west and make more landfalls in China. An analysis of the relationship between ENSO and the typhoon season.

What Is ENSO?

ENSO (El Niño–Southern Oscillation) is the periodic warming and cooling of sea-surface temperatures in the central and eastern equatorial Pacific: abnormally warm waters indicate El Niño, while abnormally cool waters indicate La Niña. It generally occurs in a cycle every 2–7 years. It is the most important climate background influencing the overall character of a typhoon season.

Typhoon Characteristics in El Niño Years

  • Formation farther east and south: As warm water shifts eastward, more typhoons are "born" over the open ocean east of Guam
  • Longer journey at sea → greater intensity: A longer journey over the ocean allows more energy to be absorbed, resulting in a noticeably higher proportion of super typhoons
  • Fewer landfalls in China overall: After forming farther east, typhoons are more likely to turn toward Japan and South Korea
  • Higher probability of the Fujiwara effect (interaction between two typhoons): Simultaneous existence of multiple typhoons over the open ocean is more common

Typhoon Characteristics in La Niña Years

  • Formation farther west: A higher proportion of locally formed typhoons appear over the South China Sea and waters east of the Philippines
  • Shorter development period and warning window: Because they form close to shore, only two or three days may elapse between formation and landfall
  • A higher proportion of landfalls in China: A stronger, farther-westward subtropical high often steers typhoons westward toward southern China
  • Autumn typhoons combined with cold air carry a greater risk, potentially resulting in more severe rainstorm-related disasters

Some Classic Seasonal Patterns

YearBackgroundTyphoon Season Characteristics
1997Super El NiñoTen super typhoons formed throughout the year, with formation locations notably farther east
2018El Niño developingRemote-ocean super typhoons such as MANGKHUT occurred frequently
2020La NiñaAn unusual "typhoon-free" period occurred over the western Pacific in July, while numerous typhoons clustered and made landfalls in China in August
2021La NiñaTyphoons such as IN-FA moved westward and made landfalls in eastern China, bringing extreme rainfall

How Can ENSO Help with Typhoon Season Preparedness?

ENSO provides only a probabilistic background, not a definitive forecast: El Niño years can still feature severe typhoons making landfall in China, while La Niña years can also produce dominant super typhoons over the open ocean. The appropriate approach is to pay close attention during El Niño years to the potential turning paths of super typhoons over the open ocean, particularly their impact on shipping and island travel. During La Niña years, preparedness should focus on the risks of rapid formation near the coast and successive landfalls by multiple typhoons.