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. Author manuscript; available in PMC: 2020 Nov 16.
Published in final edited form as: Bull Am Meteorol Soc. 2019 Aug 28;100(8):1511–1528. doi: 10.1175/BAMS-D-18-0100.1

Fig. 2.

Fig. 2.

Flight strategies employed by a single Twin Otter aircraft in previous aerosol–cloud field investigations (dashed green and purple lines), in contrast to the comprehensive plan for ACTIVATE using a dual-aircraft approach (red lines). Relevant parameters that are typically needed for analysis are shown where they are measured, with some values integrated over cloud depth and others as a function of altitude [i.e., f(z)]: LWP = liquid water path, WVP = water vapor path, ΔZ = cloud thickness, τ = cloud optical depth, CTH = cloud-top height, Na = subcloud aerosol concentration, w = cloud base updraft velocity, R = rain rate, Nd = cloud droplet concentration, re = drop effective radius, σa = vertically resolved remote sensing parameters such as aerosol extinction coefficient, T = temperature, q = humidity, u/υ = wind components. Variables in blue and black are measured via remote sensing and in situ techniques, respectively; note though that T(z), q(z), u(z), and υ(z) are measured with dropsondes released from the higher aircraft.