• Reineman, B. D., Lenain L. , Statom N. M. , and Melville W. K. , 2013: Development and testing of instrumentation for UAV-based flux measurements within terrestrial and marine atmospheric boundary layers. J. Atmos. Oceanic Technol., 30, 12951319.

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CORRIGENDUM

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  • 1 Scripps Institution of Oceanography, and Department of Mechanical and Aerospace Engineering, University of California, San Diego, La Jolla, California
  • | 2 Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California
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In the final processing of Reineman et al. (2013), the appearance of Fig. 17 on p. 1313 was inadvertently altered. Figure 17 appears below as it was meant to be shown.

Sample time series of variables measured by the ScanEagle Flux payload, at an altitude of 32.4 ± 3.1 m AGL over the Potomac River on 13 Apr 2012, showing (a) vertical wind; (b) water vapor concentration, as measured by the krypton hygrometer; and (c) temperature, as measured by the optical sensor (low-pass filtered with a 4-Hz-cutoff Butterworth filter). Positive correlation

In the final processing of Reineman et al. (2013), the appearance of Fig. 17 on p. 1313 was inadvertently altered. Figure 17 appears below as it was meant to be shown.

Sample time series of variables measured by the ScanEagle Flux payload, at an altitude of 32.4 ± 3.1 m AGL over the Potomac River on 13 Apr 2012, showing (a) vertical wind; (b) water vapor concentration, as measured by the krypton hygrometer; and (c) temperature, as measured by the optical sensor (low-pass filtered with a 4-Hz-cutoff Butterworth filter). Positive correlation

In the final processing of Reineman et al. (2013), the appearance of Fig. 17 on p. 1313 was inadvertently altered. Figure 17 appears below as it was meant to be shown.

Sample time series of variables measured by the ScanEagle Flux payload, at an altitude of 32.4 ± 3.1 m AGL over the Potomac River on 13 Apr 2012, showing (a) vertical wind; (b) water vapor concentration, as measured by the krypton hygrometer; and (c) temperature, as measured by the optical sensor (low-pass filtered with a 4-Hz-cutoff Butterworth filter). Positive correlation

In the final processing of Reineman et al. (2013), the appearance of Fig. 17 on p. 1313 was inadvertently altered. Figure 17 appears below as it was meant to be shown.

Sample time series of variables measured by the ScanEagle Flux payload, at an altitude of 32.4 ± 3.1 m AGL over the Potomac River on 13 Apr 2012, showing (a) vertical wind; (b) water vapor concentration, as measured by the krypton hygrometer; and (c) temperature, as measured by the optical sensor (low-pass filtered with a 4-Hz-cutoff Butterworth filter). Positive correlation

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