Dongyou Wu
Biographic Data
| ID | 7998431 |
|---|---|
| NAME | Dongyou Wu |
| GIVEN NAMES | Dongyou |
| FAMILY NAME | Wu |
| SIGNATURE | WU D |
| AFFILIATIONS | Lanzhou University |
| ORCID | 0000-0001-5946-1280 |
| VERIFIED | Yes |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2021 |
| LATEST PUBLICATION YEAR | 2024 |
| H-INDEX | 0 |
Divergent features of the upper-tropospheric carbonaceous aerosol layer
The upper-tropospheric carbonaceous aerosol layer (TCAL) represents the increase of aerosols in the upper-troposphere. It was first discovered over Asia but was found in this study to also occur over South America and Africa. The TCALs over three regions typically exist during the strong deep convection season, with the Asian, South American, and African TCALs showing peak intensity during July–August, October–December, and November–December, res…
Projection of extreme precipitation induced by Arctic amplification over the Northern Hemisphere
Numerous attempts have been made to understand the connection between extreme weather and Arctic amplification (AA), and it is still disputed whether the mechanism is the elongation and deceleration of planetary-scale waves. In this study, we provide further evidence that the Arctic’s rapid warming is influencing extreme precipitation in the Northern Hermisphere based on observation and model outputs, and elucidate the underlying dynamic mechanis…
No prominent works on this page.
Projection of extreme precipitation induced by Arctic amplification over the Northern Hemisphere
Numerous attempts have been made to understand the connection between extreme weather and Arctic amplification (AA), and it is still disputed whether the mechanism is the elongation and deceleration of planetary-scale waves. In this study, we provide further evidence that the Arctic’s rapid warming is influencing extreme precipitation in the Northern Hermisphere based on observation and model outputs, and elucidate the underlying dynamic mechanis…
Divergent features of the upper-tropospheric carbonaceous aerosol layer
The upper-tropospheric carbonaceous aerosol layer (TCAL) represents the increase of aerosols in the upper-troposphere. It was first discovered over Asia but was found in this study to also occur over South America and Africa. The TCALs over three regions typically exist during the strong deep convection season, with the Asian, South American, and African TCALs showing peak intensity during July–August, October–December, and November–December, res…
Atmospheric sciences (2 works) · Climatology (2 works) · Environmental Science (2 works) · Geography (2 works) · Geology (2 works) · Meteorology (2 works) · Aerosol (1 work) · Air pollution (1 work) · Amplitude (1 work) · Arctic (1 work)