Research Article
Convective Cold Pool Associated with Offshore Propagation of Convection System over the East Coast of Southern Sumatra, Indonesia
Figure 7
(a) Time series of daily accumulation of rainfall from BMKG station during December 30, 2020–January 2, 2021. (b) A map of the 3 station data locations. (c) Comparison of simulated diurnal rainfall (mm h−1) at D03 (1 km) resolution with GSMaP satellite. Rainfall over seaside (landside) from GSMaP (WRF) is denoted as Sea1 (Sea2) and Land1 (Land2), respectively. (d) The landside and seaside area denoted for area averaged over 105–105.8°E 5.5–5°S (black box) and 105.8–106.5°E; 5.5–5°S (red box) of the eastern coastal region of South Sumatra. The average diurnal cycle is composited from January 1 to January 2, 2021. (e) Diurnal rainfall observed by radar reflectivity (dBZ) height-time cross section of radar reflectivity (dBZ) over X (105.85°E, 5.15°S as a center area of Lampung at January 1, 2021.