Interannual variability in climate and anthropogenic emissions has determined the observed year-to-year surface ozone fluctuations over the United States,and separating these two drivers is a question
It is generally accepted that the persistent blocking situation in high latitudes and the quasi-stationary front in Southern China(SC)were responsible for the long-persisting of the snowstorm over SC
The impact of surface sensible heating over the Tibetan Plateau(SHTP)on the western Pacific subtropical high(WPSH)with and without the air–sea interaction was investigated in this study.Data analysis