Profile for Charles Jackman
| Title: | Physical Scientist |
|---|---|
| Affiliation: | NASA |
| Contact: |
E-mail Code 613.3 NASA Goddard Space Flight Center GREENBELT, MD 20771 Office Phone: 301-614-6053 Fax: 301-614-5903 |
Publications
Damiani, A., B. Funke, D. R. Marsh, M. Lopez Puertas, M. L. Santee, L. Froidevaux, S. Wang, C. H. Jackman, T. von Clarmann, A. Gardini, R. R. Cordero, and M. Storini (2012). Impact of January 2005 solar proton events on chlorine species.. Atmos. Chem. Phys., 12, 4159-4179 .
doi:10.5194/acp-12-4159-2012
Swartz, W. H, R. S. Stolarski, L. D. Oman, E. L. Fleming, and C. H. Jackman (2012). Middle atmosphere response to different descriptions of the 11-yr solar cycle in spectral irradiance in a chemistry-climate model. J. Atmos. Chem. Phys, 12, 5937-5948.
doi:10.5194/acp-12-5937-2012
Fleming, E. L., C.H. Jackman, R.S. Stolarski, and A.R. Douglass (2011). A model study of the impact of source gas changes on the stratosphere for 1850-2100. Atmos. Chem. Phys., 11, 8515-8541.
10.5194/acp-11-8515-2011
Funke, B., A. Baumgaetner, M. Calisto, T. Egorova, C.H. Jackman, J. Kieser, A. Krivolutsky, M. Lopez-Puertas, D. B. Marsh, T. Reddmann, E. Rozanov, S.-M. Salmi, M. Sinnhuber, G. P. Stiller, P. T. Verronen, S. Versick, T. von Clarmann, T. Y. Vyushkova, T. Wieters, and J. M. Wissing (2011). Composition changes after the “Halloween” solar proton event: the High-Energy Particle Precipitation in the Atmosphere (HEPPA) model versus MIPAS data intercomparison study. Atmos. Chem. Phys., 11, 9089-9139.
doi:10.5194/acp-11-9089-2011
Jackman, C.H., D. R. Marsh, F. M. Vitt, R. G. Roble, C. F. Randall, P. F. Bernath, B. Funke, M. Lopez-Puertas, S. Versick, G. P. Stiller, A. J. Tylka, and E. L. Fleming (2011). Northern hemisphere atmospheric influence of the solar proton events and ground level enhancement in January 2005. Atmos. Chem. Phys., 11, 6153-6166.
10.5194/acp-11-6153-2011
Carlon N. R., D. K. Papanastasiou, E. L. Fleming, C.H. Jackman, P. A. Newman, and J. B. Burkholder (2010). UV absorption cross sections of nitrous oxide (N2O) and carbon tetrachloride (CCl4) between 210 and 350 K and the atmospheric implications. Atmos. Chem. Phys., 10(13), 6137-6149.
doi:10.5194/acp-10-6137-2010