PMCs and the Water Frost Point in the Arctic Summer Mesosphere

• Main Authors: Stevens, Michael H., Conway, Robert R., Englert, Christoph R., Summers, Michael B., Grossmann, Klaus U., Gusev, Oleg A.
• Other Authors: NAVAL RESEARCH LAB WASHINGTON DC E O HULBURT CENTER FOR SPACE RESEARCH
• Format: Text
• Language: English
• Published: 2001
• Subjects: Atmospheric Physics; Meteorology; *MESOSPHERE; *CLOUDS; *TEMPERATURE; *FROST; SUPERSATURATION; CRYOGENICS; ATMOSPHERES; TELESCOPES; INFRARED SPECTROMETERS; SPECTROGRAPHS; WATER VAPOR; BRIGHTNESS; HIGH RESOLUTION; DENSITY; ARCTIC REGIONS; REPRINTS; *PMC(POLAR MESOSPHERIC CLOUD); *ARCTIC SUMMER MESOSPHERE; *WATER FROST POINT; MAHRSI(MIDDLE ATMOSPHERE HIGH RESOLUTION SPECTROGRAPH INVESTIGATION); CRISTA(CRYOGENIC INFRARED SPECTROMETERS AND TELESCOPES FOR THE ATMOSPHERE); Arctic
• Online Access: http://www.dtic.mil/docs/citations/ADA526399; http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA526399

In August, 1997 the Middle Atmosphere High Resolution Spectrograph Investigation (MAHRSI) obtained vertical profiles of OH number density and polar mesospheric cloud (PMC) brightness by scanning the limb up to 71 deg N while the Cryogenic Infrared Spectrometers and Telescopes for the Atmosphere (CRISTA) obtained co-located vertical profiles of temperature. MAHRSI OH densities are converted to water vapor using a one-dimensional model that assumes photochemical equilibrium. By combining water vapor profiles with CRISTA temperatures we map the frost point both vertically and horizontally in the Arctic summer mesosphere. Our data show that supersaturation can exist between 80-87 km suggesting that growth of ice particles is limited to these altitudes. Additionally, we find that not only is supersaturation an insufficient condition for a PMC but also that PMCs can exist in apparently unsaturated air. Published in Geophysical Research Letters, v28 n23 p4449-4452, 1 Dec 2001. Paper number 2001GL013598.