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The Greenland ice sheet: modelling the surface mass balance from GCM output with a new statistical downscaling technique

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Academic year: 2017

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Fig. 1. (a) 10 yr mean precipitation rate (kg m −2 yr −1 ) modelled by Crocus (forced by CNRM- CNRM-CM5.1 atmospheric outputs) against near-surface air temperature in ◦ C (grey dots)
Fig. 2. 10 yr mean snowmelt (kg m −2 yr −1 ) modelled by Crocus (forced by CNRM-CM5.1 atmo- atmo-spheric outputs) against near-surface air temperature in ◦ C (grey dots)
Fig. 3. 10 yr mean sublimation rate ( kg m −2 yr −1 ) modelled by Crocus (forced by CNRM-CM5.1 atmospheric outputs) against near-surface air temperature in ◦ C (grey dots)
Fig. 4. 10 yr mean surface mass balance ( kg m −2 yr −1 ) modelled by Crocus (forced by CNRM- CNRM-CM5.1 atmospheric outputs) against near-surface air temperature in ◦ C (grey dots)
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