{"id":{"repo_id":"embry-riddle","oai_identifier":"oai:commons.erau.edu:db-theses-1215"},"canonical_url":"https://search.dev.ndltd.org/etd/embry-riddle/oai:commons.erau.edu:db-theses-1215","repository":{"repo_id":"embry-riddle","name":"Embry Riddle Aeronautical University","base_url":"https://commons.erau.edu/do/oai/"},"display":{"title":"Optical Emissions Generated During Ionospheric Heating","abstract":"<p>Ionospheric heating, accomplished by transmitting a high-frequency electromagnetic wave into the atmosphere, stimulates a large number of linear and non-linear wave-plasma interactions. One outcome of these interactions is the acceleration of thermal ionospheric electrons, leading to the production of induced optical emissions. Detection of these emissions yields information regarding wave-plasma interactions, which are of fundamental importance in many physical processes, and provides an effective means of remotely sensing ionospheric constituents and dynamics.</p> <p>During an ionospheric heating experiment performed at the High Power Auroral Stimulation facility in Alaska (64.9° N, 146.8° W), a modified Czerny-Turner grating spectrometer acquired high resolution optical spectra of a heated volume. In addition to the already-documented 0(3P) 844.6 nm (excitation energy of 10.99 eV), and 0(5P) 777.4 nm (10.74 eV) emissions, two previously unreported radio-induced optical emissions, 0+ 732-733 nm (18.61 eV), and <em>0(3D°) </em>799.0 nm (12.49 eV), were observed. The experiment utilized a 2.85 MHz, 32 MW effective radiated power, o-mode radio wave, pointed into the magnetic zenith.</p> <p>This thesis presents the first spectroscopic time series observations of a heated volume, showing optical emission modulation by the heater, and summarizes the current state of high-latitude ionospheric heating, with a focus on the generation and detection of optical emissions.</p>","abstract_html":"&lt;p&gt;Ionospheric heating, accomplished by transmitting a high-frequency electromagnetic wave into the atmosphere, stimulates a large number of linear and non-linear wave-plasma interactions. One outcome of these interactions is the acceleration of thermal ionospheric electrons, leading to the production of induced optical emissions. Detection of these emissions yields information regarding wave-plasma interactions, which are of fundamental importance in many physical processes, and provides an effective means of remotely sensing ionospheric constituents and dynamics.&lt;/p&gt; &lt;p&gt;During an ionospheric heating experiment performed at the High Power Auroral Stimulation facility in Alaska (64.9° N, 146.8° W), a modified Czerny-Turner grating spectrometer acquired high resolution optical spectra of a heated volume. In addition to the already-documented 0(3P) 844.6 nm (excitation energy of 10.99 eV), and 0(5P) 777.4 nm (10.74 eV) emissions, two previously unreported radio-induced optical emissions, 0+ 732-733 nm (18.61 eV), and &lt;em&gt;0(3D°) &lt;/em&gt;799.0 nm (12.49 eV), were observed. The experiment utilized a 2.85 MHz, 32 MW effective radiated power, o-mode radio wave, pointed into the magnetic zenith.&lt;/p&gt; &lt;p&gt;This thesis presents the first spectroscopic time series observations of a heated volume, showing optical emission modulation by the heater, and summarizes the current state of high-latitude ionospheric heating, with a focus on the generation and detection of optical emissions.&lt;/p&gt;","abstract_has_math":false,"creators":["Mutiso, Charles Kiumo"],"institution":null,"degree_name":"Master of Science in Space Science","degree_level":"Thesis - Open Access","degree_discipline":"Physical Sciences","degree_department":null,"school":null,"contributors":["John M. Hughes","G. G. Sivjee","Mark Anthony Reynolds"],"advisors":[],"committee_chairs":[],"committee_members":[],"year":2008,"date_issued":"2008-06-01T07:00:00Z","date_published":"2008-06-01T07:00:00Z","updated_at":"2026-07-27T19:25:45Z","subjects":["optical emissions","ionosphere","Astrophysics and Astronomy","Atmospheric Sciences"],"languages":[],"rights":[],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"https://commons.erau.edu/db-theses/154","outbound_label":"Repository record","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor","label":"Contributor","values":["John M. Hughes","G. G. 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One outcome of these interactions is the acceleration of thermal ionospheric electrons, leading to the production of induced optical emissions. Detection of these emissions yields information regarding wave-plasma interactions, which are of fundamental importance in many physical processes, and provides an effective means of remotely sensing ionospheric constituents and dynamics.</p> <p>During an ionospheric heating experiment performed at the High Power Auroral Stimulation facility in Alaska (64.9° N, 146.8° W), a modified Czerny-Turner grating spectrometer acquired high resolution optical spectra of a heated volume. In addition to the already-documented 0(3P) 844.6 nm (excitation energy of 10.99 eV), and 0(5P) 777.4 nm (10.74 eV) emissions, two previously unreported radio-induced optical emissions, 0+ 732-733 nm (18.61 eV), and <em>0(3D°) </em>799.0 nm (12.49 eV), were observed. The experiment utilized a 2.85 MHz, 32 MW effective radiated power, o-mode radio wave, pointed into the magnetic zenith.</p> <p>This thesis presents the first spectroscopic time series observations of a heated volume, showing optical emission modulation by the heater, and summarizes the current state of high-latitude ionospheric heating, with a focus on the generation and detection of optical emissions.</p>"]},{"key":"dc:title","label":"Title","values":["Optical Emissions Generated During Ionospheric Heating"]}]}],"canonical_facts":{"dc:contributor":["John M. Hughes","G. G. Sivjee","Mark Anthony Reynolds"],"dc:creator":["Mutiso, Charles Kiumo"],"dc:description.abstract":["<p>Ionospheric heating, accomplished by transmitting a high-frequency electromagnetic wave into the atmosphere, stimulates a large number of linear and non-linear wave-plasma interactions. One outcome of these interactions is the acceleration of thermal ionospheric electrons, leading to the production of induced optical emissions. Detection of these emissions yields information regarding wave-plasma interactions, which are of fundamental importance in many physical processes, and provides an effective means of remotely sensing ionospheric constituents and dynamics.</p> <p>During an ionospheric heating experiment performed at the High Power Auroral Stimulation facility in Alaska (64.9° N, 146.8° W), a modified Czerny-Turner grating spectrometer acquired high resolution optical spectra of a heated volume. In addition to the already-documented 0(3P) 844.6 nm (excitation energy of 10.99 eV), and 0(5P) 777.4 nm (10.74 eV) emissions, two previously unreported radio-induced optical emissions, 0+ 732-733 nm (18.61 eV), and <em>0(3D°) </em>799.0 nm (12.49 eV), were observed. The experiment utilized a 2.85 MHz, 32 MW effective radiated power, o-mode radio wave, pointed into the magnetic zenith.</p> <p>This thesis presents the first spectroscopic time series observations of a heated volume, showing optical emission modulation by the heater, and summarizes the current state of high-latitude ionospheric heating, with a focus on the generation and detection of optical emissions.</p>"],"dc:identifier":["https://commons.erau.edu/db-theses/154"],"dc:subject":["optical emissions","ionosphere","Astrophysics and Astronomy","Atmospheric Sciences"],"dc:title":["Optical Emissions Generated During Ionospheric Heating"],"thesis:degree_discipline":["Physical Sciences"],"thesis:degree_level":["Thesis - Open Access"],"thesis:degree_name":["Master of Science in Space Science"]},"updated_at":"2026-07-27T19:25:45Z"}