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Teleconnections were first noted by the British meteorologist Sir Gilbert Walker in the late 19th century, through computation of the correlation between time series of atmospheric pressure, temperature and rainfall. They served as a building block for the understanding of climate variability, by showing that the latter was not purely random.

Teleconnections were first noted by the British meteorologist Sir Gilbert Walker in the late 19th century, through computation of the correlation between time series of atmospheric pressure, temperature and rainfall. They served as a building block for the understanding of climate variability, by showing that the latter was not purely random.

19世纪末 ，英国气象学家吉尔伯特·沃克爵士在计算大气压力、气温和降雨量时间序列数据之间的相关性时，首次注意到了遥相关现象。遥相关现象表明气候变化并不是完全随机的，而是相互影响的，遥相关成为理解气候变异的关键。

 

19世纪末 ，英国气象学家吉尔伯特·沃克爵士在计算大气压力、气温和降雨量时间序列数据之间的相关性时，首次注意到了遥相关现象。

Indeed, the term [[El Niño–Southern Oscillation]] (ENSO) is an implicit acknowledgment that the phenomenon underlies variability in several locations at once. It was later noticed that associated teleconnections occurred all over North America, as embodied by the [[Pacific–North American teleconnection pattern]].

Indeed, the term [[El Niño–Southern Oscillation]] (ENSO) is an implicit acknowledgment that the phenomenon underlies variability in several locations at once. It was later noticed that associated teleconnections occurred all over North America, as embodied by the [[Pacific–North American teleconnection pattern]].