Fig. 9From: Maritime continent coastlines controlling Earth’s climateExamples of a frequency power spectra (at a coastal land station in Bengkulu (04°S, 102°E), southwestern coast of Sumatera); b, c 10 day-mean land (Bengkulu)/marine (RV Mirai, approximately 50 km SW from Bengkulu) atmospheric temperature diurnal cycles below 1 km altitude; and d their difference, obtained during 8–18 December 2015. The abscissas of b−d are in UT (= LT−7 h). Details of the observations are described in Yokoi et al. (2017) and Wu et al. (2018)Back to article page