Gu Wei, chief forecaster of the National Climate Center, said that the sea temperature index for the first half of August has broken through 2.5℃, but according to the relevant national standards, the current sliding average has not reached the threshold of a super event, and currently no super El Niño event has officially formed. The National Climate Center predicts that sea surface temperatures in the equator Middle East and Pacific will continue to fluctuate and rise, reaching the peak of this event from November to December this year. The current warming trend is obvious. The peak of the 3-month sliding average is likely to exceed the 2.5℃ mark, forming a super strong El Niño event and becoming the strongest since observations were recorded. Monitoring by the National Climate Center shows that since summer, China's climatic characteristics reflect the typical effects of the El Niño development stage: the east has two rainy zones in the north and south. The torrential rain process was extensive and strong, the falling areas overlapped, and the disasters were compounded; the typhoon was active and intense, and wind and rain affected for a long time.

Gu Wei, chief forecaster of the National Climate Center, said that the sea temperature index for the first half of August has broken through 2.5℃, but according to the relevant national standards, the current sliding average has not reached the threshold of a super event, and currently no super El Niño event has officially formed. The National Climate Center predicts that sea surface temperatures in the equator Middle East and Pacific will continue to fluctuate and rise, reaching the peak of this event from November to December this year. The current warming trend is obvious. The peak of the 3-month sliding average is likely to exceed the 2.5℃ mark, forming a super strong El Niño event and becoming the strongest since observations were recorded. Monitoring by the National Climate Center shows that since summer, China's climatic characteristics reflect the typical effects of the El Niño development stage: the east has two rainy zones in the north and south. The torrential rain process was extensive and strong, the falling areas overlapped, and the disasters were compounded; the typhoon was active and intense, and wind and rain affected for a long time.