Synonyms: 
SOLVE 1
SOLVE1
SOLVE I
Associated content: 

First measurements of ClOOCl in the stratosphere: The coupling of ClOOCl and ClO in the Arctic polar vortex

Hydration, dehydration, and the total hydrogen budget of the 1999/2000 winter Arctic stratosphere

Microphysical modeling of the 1999–2000 Arctic winter 2. Chlorine activation and ozone depletion

Microphysical modeling of the 1999–2000 Arctic winter: 1. Polar stratospheric clouds, denitrification, and dehydration

Microphysical modeling of the 1999--2000 Arctic winter: 3. Impact of homogeneous freezing on polar stratospheric clouds

Evidence for the widespread presence of liquid-phase particles during the 1999–2000 Arctic winter

Drdla, K., et al. (2003), Evidence for the widespread presence of liquid-phase particles during the 1999–2000 Arctic winter, J. Geophys. Res., 108, 8318, doi:10.1029/2001JD001127.

Discriminating Types Ia and Ib polar stratospheric clouds in POAM satellite data

Strawa, A., et al. (2002), Discriminating Types Ia and Ib polar stratospheric clouds in POAM satellite data, J. Geophys. Res., 107, 8291, doi:10.1029/2001JD000458.

Molecular velocity distributions and generalized scale invariance in the turbulent atmosphere

Tuck, A. F., et al. (2013), Molecular velocity distributions and generalized scale invariance in the turbulent atmosphere, Faraday Discussions, 130, 181-193, doi:10.1039/b410551f.

Uptake of reactive nitrogen on cirrus cloud particles in the upper troposphere and lowermost stratosphere

Nitric acid condensation on ice: 1. Non-HNO3 constituent of NOY condensing cirrus particles on upper tropospheric

Gamblin, B., et al. (2006), Nitric acid condensation on ice: 1. Non-HNO3 constituent of NOY condensing cirrus particles on upper tropospheric, J. Geophys. Res., 111, D21203, doi:10.1029/2005JD006048.

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