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Li-li Yu results 96 · Newest (Page 1/4, per page 25)
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Journal: Climate Dynamics ×Author: Li-li Yu ×Clear All Filters
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Climate Dynamics · 2026 · Vol. 64 · Issue 3 · Springer
Long-term changes in upper-air wind speed remain substantially uncertain due to the spatial and temporal sparseness of radiosonde observations. This study estimates wind speed trends at six tropospheric pressure levels (850–200 hPa) over land using global IGRA radiosonde records and six reanalysis datasets. Radiosonde observations indicate a general increase in upper troposphere over the past four decades, except Australia. In...
Climate Dynamics · 2024 · Vol. 62 · Issue 8 · Springer
A Stratospheric Northern Annular Mode (SNAM) phase-based composite analysis reveals that continental Cold Air Outbreaks (CAOs) can occur during both positive and negative SNAM events. CAOs tend to occur over Asia, characterized by a meridional-dipole surface temperature anomaly pattern (cold midlatitudes and warm high-latitudes) when the SNAM index is decreasing or the stratospheric polar vortex is weakening, but over North Am...
Climate Dynamics · 2024 · Vol. 62 · Issue 8 · Springer
An accurate understanding of the current and future water cycle over the Third Pole is of great societal importance, given the role this region plays as a water tower for densely populated areas downstream. An emerging and promising approach for skillful climate assessments over regions of complex terrain is kilometer-scale climate modeling. As a foundational step towards such simulations over the Third Pole, we present a mult...
Climate Dynamics · 2024 · Vol. 62 · Issue 5 · Springer
This study used observed rainfall, ERA5 reanalysis, and CMIP6 model datasets to investigate the interdecadal variation and underlying mechanism of persistent heavy rainfall (PHR) over the Huaihe River Basin (HRB) in China during July–August, and to examine the role of the Atlantic Multidecadal Oscillation (AMO) in modulating such rainfall. The results indicate that PHR over the HRB exhibited a marked interdecadal variation. Th...