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英国气象学家吉尔伯特 · 沃克爵士在19世纪末通过计算大气压力、气温和降雨量的时间序列之间的相关性，首次注意到了遥相关。它们是理解气候变化的基石，因为它们表明气候变化并非完全随机的。
英国气象学家吉尔伯特 · 沃克爵士在19世纪末通过计算大气压力、气温和降雨量的时间序列之间的相关性，首次注意到了遥相关。它们是理解气候变化的基石，因为它们表明气候变化并非完全随机的。
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]].