Open AccessEvidence of nitric acid uptake in warm cirrus anvil clouds during the NASA TC4 campaign
Author(s) -
Scheuer Eric,
Dibb Jack E.,
Twohy Cynthia,
Rogers David C.,
Heymsfield Andrew J.,
Bansemer Aaron
Publication year - 2010
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2009jd012716
Subject(s) - cirrus , ice cloud , troposphere , atmospheric sciences , mixing ratio , environmental science , aerosol , radiative transfer , geology , meteorology , physics , quantum mechanics
Uptake of HNO 3 onto cirrus ice may play an important role in tropospheric NO x cycling. Discrepancies between modeled and in situ measurements of gas‐phase HNO 3 in the troposphere suggest that redistribution and removal mechanisms by cirrus ice have been poorly constrained. Limited in situ measurements have provided somewhat differing results and are not fully compatible with theory developed from laboratory studies. We present new airborne measurements of HNO 3 in cirrus clouds from anvil outflow made during the Tropical Composition, Cloud, and Climate Coupling Experiment (TC4). Upper tropospheric (>9 km) measurements made during three flights while repeatedly traversing the same cloud region revealed depletions of gas‐phase HNO 3 in regions characterized by higher ice water content and surface area. We hypothesize that adsorption of HNO 3 onto cirrus ice surfaces could explain this. Using measurements of cirrus ice surface area density and some assumptions about background mixing ratios of gas‐phase HNO 3 , we estimate molecular coverages of HNO 3 on cirrus ice surface in the tropical upper troposphere during the TC4 racetracks to be about 1 × 10 13 molecules cm −2 . This likely reflects an upper limit because potential dilution by recently convected, scavenged air is ignored. Also presented is an observation of considerably enhanced gas‐phase HNO 3 at the base of a cirrus anvil suggesting vertical redistribution of HNO 3 by sedimenting cirrus particles and subsequent particle sublimation and HNO 3 evaporation. The impact of released HNO 3 , however, appears to be restricted to a very thin layer just below the cloud.