grant
Mechanisms of Hydroxyl Energy Transfer in Upper Atmospheric Nightglow
Organization SRI InternationalLocation MENLO PARK, United StatesPosted 1 Apr 2026Deadline 31 Mar 2029
NSFUS FederalResearch GrantScience FoundationCA
Description preview
Earth’s upper atmosphere emanates a faint luminescence known as airglow. This non-thermal radiation occurs at altitudes from about 50 to 300 km and is initiated by solar radiation absorbed by atmospheric constituents. Light emission observed during the day is called dayglow. A plethora of photochemical processes and excitation pathways persist…
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