Melting trends over the Greenland ice sheet (1958–2009) from spaceborne microwave data and regional climate models
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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](https://thumb-eu.123doks.com/thumbv2/123dok_br/18446229.363752/5.892.130.761.127.903/surface-temperature-observed-crawford-temperature-simulated-temperature-simulated.webp)
![Table 2. Abbreviation of the different techniques discussed in the text to detect the melt](https://thumb-eu.123doks.com/thumbv2/123dok_br/18446229.363752/6.892.140.748.549.714/table-abbreviation-different-techniques-discussed-text-detect-melt.webp)
![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](https://thumb-eu.123doks.com/thumbv2/123dok_br/18446229.363752/7.892.87.808.200.746/table-correspondence-detection-number-algorithms-detects-retrieving-algorithms.webp)
![Table 5. The same as Table 4 but for ExtXPGR with T19H thsd = 227.5 K.](https://thumb-eu.123doks.com/thumbv2/123dok_br/18446229.363752/8.892.128.770.133.241/table-table-extxpgr-t-h-thsd-k.webp)
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