Temporal variability of the descent of high-altitude NOXinferred from ionospheric data

Author:

Clilverd Mark A.1,Seppälä Annika2,Rodger Craig J.3,Thomson Neil R.3,Lichtenberger János4,Steinbach Péter5

Affiliation:

1. Physical Sciences Division; British Antarctic Survey; Cambridge UK

2. Earth Observation; Finnish Meteorological Institute; Helsinki Finland

3. Department of Physics; University of Otago; Dunedin New Zealand

4. Space Research Group; Eötvös University; Budapest Hungary

5. MTA-ELTE Research Group for Geoinformatics and Space Sciences; Budapest Hungary

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference32 articles.

1. Relationships between precipitating auroral zone electrons and lower thermospheric nitric oxide densities: 1998-2000;Baker;J. Geophys. Res.,2001

2. ELF and VLF radio waves;Barr;J. Atmos. Sol. Terr. Phys.,2000

3. Global observations of nitric oxide in the thermosphere;Barth;J. Geophys. Res.,2003

4. Stellar occultation technique for atmospheric ozone monitoring: GOMOS on Envisat;Bertaux;Earth Obs. Q.,2000

5. First results on GOMOS/Envisat;Bertaux;Adv. Space Res.,2004

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