Luke D Oman
Biographic Data
| ID | 7154430 |
|---|---|
| NAME | Luke D Oman |
| GIVEN NAMES | Luke D |
| FAMILY NAME | Oman |
| SIGNATURE | OMAN L D |
| AFFILIATIONS | Goddard Space Flight Center |
| ORCID | 0000-0002-5487-2598 |
| VERIFIED | Yes |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2015 |
| LATEST PUBLICATION YEAR | 2018 |
| H-INDEX | 0 |
Tropospheric jet response to Antarctic ozone depletion
The Southern Hemisphere (SH) zonal-mean circulation change in response to Antarctic ozone depletion is re-visited by examining a set of the latest model simulations archived for the Chemistry-Climate Model Initiative (CCMI) project. All models reasonably well reproduce Antarctic ozone depletion in the late 20th century. The related SH-summer circulation changes, such as a poleward intensification of westerly jet and a poleward expansion of the Ha…
Impact of future nitrous oxide and carbon dioxide emissions on the stratospheric ozone layer
The atmospheric levels of human-produced chlorocarbons and bromocarbons are projected to make only small contributions to ozone depletion by 2100. Increases in carbon dioxide (CO _2 ) and nitrous oxide (N _2 O) will become increasingly important in determining the future of the ozone layer. N _2 O increases lead to increased production of nitrogen oxides (NO _x ), contributing to ozone depletion. CO _2 increases cool the stratosphere and affect o…
No prominent works on this page.
Impact of future nitrous oxide and carbon dioxide emissions on the stratospheric ozone layer
The atmospheric levels of human-produced chlorocarbons and bromocarbons are projected to make only small contributions to ozone depletion by 2100. Increases in carbon dioxide (CO _2 ) and nitrous oxide (N _2 O) will become increasingly important in determining the future of the ozone layer. N _2 O increases lead to increased production of nitrogen oxides (NO _x ), contributing to ozone depletion. CO _2 increases cool the stratosphere and affect o…
Tropospheric jet response to Antarctic ozone depletion
The Southern Hemisphere (SH) zonal-mean circulation change in response to Antarctic ozone depletion is re-visited by examining a set of the latest model simulations archived for the Chemistry-Climate Model Initiative (CCMI) project. All models reasonably well reproduce Antarctic ozone depletion in the late 20th century. The related SH-summer circulation changes, such as a poleward intensification of westerly jet and a poleward expansion of the Ha…
Atmospheric and Environmental Gas Dynamics (2 works) · Atmospheric chemistry and aerosols (2 works) · Atmospheric Ozone and Climate (2 works) · Atmospheric sciences (2 works) · Environmental Science (2 works) · Ozone (2 works) · Ozone Depletion (2 works) · Ozone layer (2 works) · Stratosphere (2 works) · Atmospheric Circulation (1 work)