Estimating Greenland surface melt is hampered by melt induced dampening of temperature variability
he positive degree-day (PDD) model provides a particularly simple approach to estimate surface melt from land ice based solely on air temperature. Here, we use a climate and snow pack simulation of the Greenland ice sheet (Modèle Atmosphérique Régional, MAR) as a reference, to analyze this scheme in...
| Published in: | Journal of Glaciology |
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| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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INT GLACIOL SOC
2018
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| Subjects: | |
| Online Access: | https://epic.awi.de/id/eprint/48079/ https://epic.awi.de/id/eprint/48079/1/estimating_greenland_surface_melt_is_hampered_by_melt_induced_dampening_of_temperature_variability.pdf https://www.cambridge.org/core/journals/journal-of-glaciology/article/estimating-greenland-surface-melt-is-hampered-by-melt-induced-dampening-of-temperature-variability/B043A6CE2D469695FB1795FA16998715 https://hdl.handle.net/10013/epic.2916e229-d755-4a5c-a301-61ab4ab8d587 |
| Summary: | he positive degree-day (PDD) model provides a particularly simple approach to estimate surface melt from land ice based solely on air temperature. Here, we use a climate and snow pack simulation of the Greenland ice sheet (Modèle Atmosphérique Régional, MAR) as a reference, to analyze this scheme in three realizations that incorporate the sub-monthly temperature variability differently: (i) by local values, (ii) by local values that systematically overestimate the dampened variability associated with intense melting or (iii) by one constant value. Local calibrations reveal that incorporating local temperature variability, particularly resolving the dampened variability of melt areas, renders model parameters more temperature-dependent. This indicates that the negative feedback between surface melt and temperature variability introduces a non-linearity into the temperature – melt relation. To assess the skill of the individual realizations, we hindcast melt rates from MAR temperatures for each realization. For this purpose, we globally calibrate Greenland-wide, constant parameters. Realization (i) exhibits shortcomings in the spatial representation of surface melt unless temperature-dependent instead of constant parameters are calibrated. The other realizations perform comparatively well with constant parametrizations. The skill of the PDD model primarily depends, however, on the consistent calibration rather than on the specific representation of variability. |
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