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Luke D Oman

Biographic Data

ID7154430
NAMELuke D Oman
GIVEN NAMESLuke D
FAMILY NAMEOman
SIGNATUREOMAN L D
AFFILIATIONSGoddard Space Flight Center
ORCID0000-0002-5487-2598
VERIFIEDYes
TOTAL WORKS2
TOTAL CITATIONS0
WORKS AS AUTHOR2
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2015
LATEST PUBLICATION YEAR2018
H-INDEX0
  • Tropospheric jet response to Antarctic ozone depletion

    Open Access•Seok‐Woo Son, Bo-Reum Han et al.•ARTICLE•Environmental Research Letters•2018

    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

    Open Access•Richard S Stolarski, A R Douglass et al.•ARTICLE•Environmental Research Letters•2015

    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

    Open Access•Richard S Stolarski, A R Douglass et al.•ARTICLE•Environmental Research Letters•2015

    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

    Open Access•Seok‐Woo Son, Bo-Reum Han et al.•ARTICLE•Environmental Research Letters•2018

    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)

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