Figure 1 | Scientific Reports

Figure 1

From: Antarctic ice mass variations from 1979 to 2017 driven by anomalous precipitation accumulation

Figure 1

(a) Antarctic accumulated precipitation after removing a linear trend (1979–2017). The linear trend is estimated from the first order polynomial (\({a}_{0}+{a}_{1}t\)) fitting to accumulated precipitation. (b) Map of acceleration rate of accumulated precipitation. Acceleration rates are estimated from the second order polynomial (\({a}_{0}+{a}_{1}t+\frac{1}{2}{a}_{2}{t}^{2}\)) fitting to accumulated precipitation. Figures are created with Generic Mapping Tools (GMT-5.4.5, https://gmt.soest.hawaii.edu/).

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