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Melting trends over the Greenland ice sheet (1958–2009) from spaceborne microwave data and regional climate models

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Academic year: 2017

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Fig. 1. (a) Top – daily mean near-surface temperature (in black) observed in summer 2002 at Crawford Point 1 (69.9 ◦ N, 47 ◦ W, 2022 m), 3 m-temperature simulated by the MAR model (in blue), 2 m-temperature simulated by the RACMO2 model (in red) and, the T
Table 2. Abbreviation of the different techniques discussed in the text to detect the melt
Table 4. Correspondence between Eq. (1)-based and RCM-based melt detection. The mean number of GrIS pixels when both RCM and T19H-based algorithms detect melt (RCM = SAT), when RCM detects melt and not the retrieving algorithms (RCM > SAT) and when RCM
Table 5. The same as Table 4 but for ExtXPGR with T19H thsd = 227.5 K.
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