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 (March-April-May) 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 that 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 t...
The tropical easterly jet (TEJ) is a prominent atmospheric circulation feature observed during the A...
The tropical easterly jet (TEJ) is a prominent atmospheric circulation feature observed during the A...
Long-term changes in upper-tropospheric jet latitude, altitude, and strength are assessed using five...
In this study, 40-yr ECMWF Re-Analysis (ERA-40) data are used for the description of the seasonal cy...
In this study, 40-yr ECMWF Re-Analysis (ERA-40) data are used for the description of the seasonal cy...
This study presents a 5-yr climatology of 7-day back trajectories started from the Northern Hemisphe...
The westerly jet (WJ) is an important component of atmospheric circulation, which is characterized b...
The westerly jet (WJ) is an important component of atmospheric circulation, which is characterized b...
The tropics are expanding poleward at about 0.5∘ per decade in observations. This poleward expansio...
This is the final version. Available on open access from Springer via the DOI in this recordThe trop...
During the summer monsoon the upper tropospheric subtropical anticyclone of Asia is centred over SE ...
The intensity and location of the westerly jet (WJ) in the mid-latitudes of the Northern Hemisphere ...
The westerly jet (WJ) in the upper troposphere, an important atmospheric circulation system, is crit...
A new jet stream description, defined as the geostrophic streamline of maximum average velocity is p...
The westerly jet (WJ) in the upper troposphere, an important atmospheric circulation system, is crit...
The tropical easterly jet (TEJ) is a prominent atmospheric circulation feature observed during the A...
The tropical easterly jet (TEJ) is a prominent atmospheric circulation feature observed during the A...
Long-term changes in upper-tropospheric jet latitude, altitude, and strength are assessed using five...
In this study, 40-yr ECMWF Re-Analysis (ERA-40) data are used for the description of the seasonal cy...
In this study, 40-yr ECMWF Re-Analysis (ERA-40) data are used for the description of the seasonal cy...
This study presents a 5-yr climatology of 7-day back trajectories started from the Northern Hemisphe...
The westerly jet (WJ) is an important component of atmospheric circulation, which is characterized b...
The westerly jet (WJ) is an important component of atmospheric circulation, which is characterized b...
The tropics are expanding poleward at about 0.5∘ per decade in observations. This poleward expansio...
This is the final version. Available on open access from Springer via the DOI in this recordThe trop...
During the summer monsoon the upper tropospheric subtropical anticyclone of Asia is centred over SE ...
The intensity and location of the westerly jet (WJ) in the mid-latitudes of the Northern Hemisphere ...
The westerly jet (WJ) in the upper troposphere, an important atmospheric circulation system, is crit...
A new jet stream description, defined as the geostrophic streamline of maximum average velocity is p...
The westerly jet (WJ) in the upper troposphere, an important atmospheric circulation system, is crit...
The tropical easterly jet (TEJ) is a prominent atmospheric circulation feature observed during the A...
The tropical easterly jet (TEJ) is a prominent atmospheric circulation feature observed during the A...
Long-term changes in upper-tropospheric jet latitude, altitude, and strength are assessed using five...