The Silk Road pattern in meteorology is a wave-like teleconnection pattern in the summer propagating eastward under the wave guidance of the upper-tropospheric Asian westerly jet stream. It shows up as alternate southerly and northerly anomalies (or cyclonic and anticyclonic circulation anomalies) along the jet, and is the leading mode of the interannual variability of upper-tropospheric meridional winds. It is interesting that this meteorological teleconnection pattern covers most domains along the ancient Silk Road, and exerts significant influences on climatic anomalies over a broad area of the Eurasian continent.