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Progress in Earth and Planetary Science
Fig. 10 | Progress in Earth and Planetary Science

Fig. 10

From: Diurnal cycle over a coastal area of the Maritime Continent as derived by special networked soundings over Jakarta during HARIMAU2010

Fig. 10

Same as Fig. 9, but for the heat budget. a is for the vertically integrated values of each of the terms in the thermodynamic budget analyses. b to g are in the time–pressure cross section, for b array-scale vertical advection, c array-scale horizontal advection, d Q1, e Q2, f Q1–Q2, and g the array-scale vertical air motion in pressure coordinates (same as Fig. 9e)

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