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A meteorological overview of the TC4 mission

Pfister, L., et al. (2010), A meteorological overview of the TC4 mission, J. Geophys. Res., 115, D00J12, doi:10.1029/2009JD013316.

Remote sensing of radiative and microphysical properties of clouds during TC4: Results from MAS, MASTER, MODIS, and MISR

Observations and modeling of ice cloud shortwave spectral albedo during the Tropical Composition, Cloud and Climate Coupling Experiment (TC4)

Planning, implementation, and first results of the Tropical Composition, Cloud and Climate Coupling Experiment (TC4)

Microphysical and radiative properties of tropical clouds investigated in TC4 and NAMMA

Lawson, P., et al. (2010), Microphysical and radiative properties of tropical clouds investigated in TC4 and NAMMA, J. Geophys. Res., 115, D00J08, doi:10.1029/2009JD013017.

Evidence of nitric acid uptake in warm cirrus anvil clouds during the NASA TC4 campaign

Scheuer, E., et al. (2010), Evidence of nitric acid uptake in warm cirrus anvil clouds during the NASA TC4 campaign, J. Geophys. Res., 115, D00J03, doi:10.1029/2009JD012716.

Advanced Whole Air Sampler

32 samples/flight (ER-2); 50 samples/flight (WB57); 90 samples/flight (Global Hawk)

Updated control system with remote control capability

Fill times
–14 km 30 – 40 sec
–16 km 40 – 50 sec
–18 km 50 – 60 sec
–20 km 100 – 120 sec (estimated)

Analysis in UM lab: GC/MS; GC/FID; GC/ECD

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Rosemount Icing Detector

The RICE is a magnetostrictive oscillation probe with a sensing cylinder 6.35 mm in diameter and 2.54 cm in length. Ice buildup on the sensing cylinder causes the frequency of oscillation to change, which can be related to the rate of ice accretion and hence the cloud liquid water content (LWC). When approximately 0.5 mm of ice has accumulated, a heater melts the ice, which is shed into the air stream. The heater cycle is approximately 5 s, and the cylinder normally requires an additional 5–10 s to cool down to a temperature where it can begin accreting ice again.

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