NOAA/WDS Paleoclimatology - Himalayan 400 Year Spring Jet Stream Latitude Reconstruction

Since the 1980s, the subtropical jet stream has generally moved poleward, but its behavior varies by region and season. Here we examine the interannual variability and trends in the latitudinal position of the spring subtropical jet over the Himalayas. During the modern period (1948 to 2018), the spring (MAM) jet is typically anchored immediately south of the Himalayas, but has rarely (in 1956, 1971, 1984 and 1999) moved poleward to pass over Kyrgyzstan and northwest China. A tree-ring reconstruction of the jet's latitude indicates such poleward excursions may have become more frequent after 1950 but it is not clear whether that behavior is unprecedented within the past four centuries. These insights into the behavior of the Himalayan subtropical jet may improve seasonal weather forecasts for the region and provide a target for climate simulations to test whether the recent spate of excursions is unusual and due to anthropogenic warming.