Figure 5. Simulated outputs of three-stage linear model for the Midui glacier based on (a) sole effect of precipitation and (b) sole effect of temperature on glacier changes. The gradual changes in the form of anomaly were presented as simulation of mass balance, thickness change, flux change, and length (solid as simulated and dotted as observed) from 1385 to 2017 in both (a) and (b)

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Three-stage Linear Model Simulation of Midui Glacier since Little Ice Age (LIA)

Sadrish Dabadi, Shalik Ram Sigdel, Nita Dyola, Munawar Ali

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