Fig. 18

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Spectral response of Euclid’s wide imaging bands. For comparison we show the Gaia bands that we used – among others – for photometric calibration of the VIS IE-band, and the atmospheric transmission that limits the ground-based Y, J, H, and Ks bands, for a precipitable water vapour level of 1.0 mm from Rothman et al. (2013). Considerable colour terms may arise for individual sources when transforming fluxes in the wide Euclid bands to fluxes in other photometric systems.
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