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Abstract
Examination of ENSO events and the accumulated precipitation and δ18O values recorded in the Guliya ice core,China,shows that the relationship between the occurrence of ENSO events and the precipitation anomaly in Guliya is significant.In the years of El Nino events,the anomalies of precipitation and δ18O values in the Guliya ice core were negative anomalies,that is,the ENSO events are related to the deficit of precipitation as well as low temperature in the western China.
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Citation
YANG Meixue, YAO Tandong. 2000: CLIMATE ANOMALY RECORDED IN GULIYA ICE CORE AND ENSO EVENTS*. Journal of Meteorological Research, 14(2): 141-146.
YANG Meixue, YAO Tandong. 2000: CLIMATE ANOMALY RECORDED IN GULIYA ICE CORE AND ENSO EVENTS*. Journal of Meteorological Research, 14(2): 141-146.
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YANG Meixue, YAO Tandong. 2000: CLIMATE ANOMALY RECORDED IN GULIYA ICE CORE AND ENSO EVENTS*. Journal of Meteorological Research, 14(2): 141-146.
YANG Meixue, YAO Tandong. 2000: CLIMATE ANOMALY RECORDED IN GULIYA ICE CORE AND ENSO EVENTS*. Journal of Meteorological Research, 14(2): 141-146.
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