SOLVE

Synonyms

SOLVE 1

SOLVE1

SOLVE I

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.

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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.

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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.

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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.

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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.

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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.

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

Hallar, 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.

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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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SOLVE

National Aeronautics and Space Administration

National Aeronautics and
Space Administration