Fig. 10 | Scientific Data

Fig. 10

From: Profile observations of the Arctic atmospheric boundary layer with the BELUGA tethered balloon during MOSAiC

Fig. 10The alternative text for this image may have been generated using AI.

Reconstruction of measured terrestrial irradiances. The raw irradiance (black line) has a slow response to a box function (blue line). Observations are corrected for the response time of the pyrgeometer using a deconvolution method and then smoothed with a 3 s running mean (red line). The remaining oscillations in the corrected signal result from the Gibbs phenomenon associated with the Fourier transform.

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