Physics
Scientist
National Center for Atmospheric Research, Boulder, Colo.
Energy exchange and temperature of aerosols in the earth's atmosphere /0-60 km/
Equilibrium temperatures of small particles in the earth's upper atmosphere /50-110 km/
Equilibrium temperatures of spherical ice particles in the upper atmosphere and implications for noctilucent cloud formation
On the origin of noctilucent clouds: Extraterrestrial dust and trapped water molecules.
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