摘要
通过对树木年轮、冰核、珊瑚等的测定和分析获得的古气候记录研究成果, 评述了 E N S O 的演变规律及强度变化特征, 指明了 E N S O 是可查证记录以来就己存在的现象.
By determination and analysis of the tree ring, ice core,and corals,some records of the paleoclimatic records were obtained. The ENSO developing regulation and variation characters of intensity were commented. The results indicate that ENSO has been existing since there was the verifiable record of clmate.
出处
《云南农业大学学报》
CAS
CSCD
1999年第3期323-327,共5页
Journal of Yunnan Agricultural University