Synonyms: 
SOLVE 1
SOLVE1
SOLVE I
Associated content: 
SOLVE

Nitric acid condensation on ice: 2. Kinetic limitations, a possible ‘‘cloud clock’’ for determining cloud parcel lifetime

Gamblin, B., et al. (2007), Nitric acid condensation on ice: 2. Kinetic limitations, a possible ‘‘cloud clock’’ for determining cloud parcel lifetime, J. Geophys. Res., 112, D12209, doi:10.1029/2005JD006049.

Measurements of large stratospheric particles in the Arctic polar vortex

Brooks, S. D., et al. (2003), Measurements of large stratospheric particles in the Arctic polar vortex, J. Geophys. Res., 108, 4652, doi:10.1029/2002JD003278.

Multiple Axis Resonance Fluorescence Chemical Conversion Detector for ClO and BrO

Vacuum ultraviolet radiation produced in a low pressure plasma discharge lamp is used to induce resonance scattering in Cl and Br atoms within a flowing sample. ClO and BrO are converted to Cl and Br by the addition of NO such that the rapid bimolecular reaction ClO + NO → Cl + NO2 (BrO + NO → Br + NO2) yields one halogen atom for each halogen oxide radical present in the flowing sample. Three detection axes are used to diagnose the spatial (and thus temporal) dependence of the ClO (BrO) to Cl (Br) conversion and to detect any removal of Cl (Br) following its formation. A double duct system is used both to maintain laminar flow through the detection region and to step the flow velocity in the detection region down from free stream (200 m/sec) to 20 m/sec in order to optimize the kinetic diagnosis.

Instrument Type: 
Fluorescence
Measurements: 
ClO, BrO
Aircraft: 
ER-2 - AFRC, WB-57 - JSC, DC-8 - AFRC
Point(s) of Contact: 
James Anderson (PI)

Evidence for inertia gravity waves forming polar stratospheric clouds over Scandinavia

Dörnbrack, A., et al. (2002), Evidence for inertia gravity waves forming polar stratospheric clouds over Scandinavia, J. Geophys. Res., 107, 8287, doi:10.1029/2001JD000452.

Quantifying the rate of heterogeneous processing in the Arctic polar vortex with in situ observations of OH

Hanisco, T. F., et al. (2002), Quantifying the rate of heterogeneous processing in the Arctic polar vortex with in situ observations of OH, J. Geophys. Res., 107, 8278, doi:10.1029/2000JD000425.

In situ observations of HO2 and OH obtained on the NASA ER-2 in the high-ClO conditions of the 1999/2000 Arctic polar vortex

Hanisco, T. F., et al. (2002), In situ observations of HO2 and OH obtained on the NASA ER-2 in the high-ClO conditions of the 1999/2000 Arctic polar vortex, J. Geophys. Res., 107, 8283, doi:10.1029/2001JD001024.

Interaction between dynamics and chemistry of ozone in the setup phase of the Northern Hemisphere polar vortex

Kawa, S. R., et al. (2003), Interaction between dynamics and chemistry of ozone in the setup phase of the Northern Hemisphere polar vortex, J. Geophys. Res., 108, 8310, doi:10.1029/2001JD001527.

Measurements of ice water content in tropopause region Arctic cirrus during the SAGE III Ozone Loss and Validation Experiment (SOLVE)

Hallar, A. G., et al. (2004), Measurements of ice water content in tropopause region Arctic cirrus during the SAGE III Ozone Loss and Validation Experiment (SOLVE), J. Geophys. Res., 109, D17203, doi:10.1029/2003JD004348.

Large and unexpected enrichment in stratospheric 16 13 18 O C O and its meridional variation

Yeung, L. Y., et al. (2009), Large and unexpected enrichment in stratospheric 16 13 18 O C O and its meridional variation, Proc. Natl. Acad. Sci., 106, 11496-11501, doi:10.1073/pnas.0902930106.

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