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Fig. 3 | Progress in Earth and Planetary Science

Fig. 3

From: Precision and convergence speed of the ensemble Kalman filter-based parameter estimation: setting parameter uncertainty for reliable and efficient estimation

Fig. 3

Cold pool and radar reflectivity of the simulated squall line in the nature run: a Hovmöller diagram of potential temperature at the lowest model level; b–d snapshots of radar reflectivity, where (b) T = 6 h; (c) T = 18 h; and (d) T = 24 h. The three red line segments in (a) correspond to the times and locations of (b–d)

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