Abstract
Abstract. The spatial variability of near-surface variables and surface energy balance components over the Greenland ice sheet are presented, using the output of a regional atmospheric climate model for the period 1958–2008. The model was evaluated in Part 1 of this paper. The near-surface temperature over the ice sheet is affected by surface elevation, latitude, longitude, large-scale and small-scale advection, occurrence of summer melt and mesoscale topographical features. The atmospheric boundary layer is characterised by a strong temperature inversion, due to continuous longwave cooling of the surface. In combination with a gently sloping surface the radiative loss maintains a persistent katabatic wind. This radiative heat loss is mainly balanced by turbulent sensible heat transport towards the surface. In summer, the surface is near radiative balance, resulting in lower wind speeds. Absorption of shortwave radiation and a positive subsurface heat flux due to refreezing melt water are heat sources for surface sublimation and melt. The strongest temperature deficits (>13 °C) are found on the northeastern slopes, where the strongest katabatic winds (>9 m s−1) and lowest relative humidity (<65%) occur. Due to strong large scale winds, clear sky (cloud cover <0.5) and a concave surface, a continuous supply of cold dry air is generated, which enhances the katabatic forcing and suppresses subsidence of potentially warmer free atmosphere air.
Highlights
The Greenland ice sheet (GrIS) is the largest permanent ice and snow covered area in the Northern Hemisphere
Due to small absorption of shortwave radiation and negative net longwave radiation, the net surface radiation balance is negative, resulting in surface cooling and a stable stratification of the atmospheric boundary layer (Hoch et al, 2007). This cooling of the near-surface air results in a shallow high air pressure system located over central Greenland, which is the primary driving mechanism for the katabatic winds. These persistent katabatic winds prevent humidity to be transported to the central part of the GrIS at low atmospheric levels (Dethloff et al, 2002)
We present a 51-year climatology of the nearsurface parameters wind, temperature, humidity, radiative fluxes and surface energy balance (SEB) components of the GrIS at 11 km resolution, from the regional climate model RACMO2/GR (Van Meijgaard et al, 2008)
Summary
The Greenland ice sheet (GrIS) is the largest permanent ice and snow covered area in the Northern Hemisphere. Due to small absorption of shortwave radiation and negative net longwave radiation, the net surface radiation balance is negative, resulting in surface cooling and a stable stratification of the atmospheric boundary layer (Hoch et al, 2007) This cooling of the near-surface air results in a shallow high air pressure system located over central Greenland, which is the primary driving mechanism for the katabatic winds. We present a 51-year climatology of the nearsurface parameters wind, temperature, humidity, radiative fluxes and surface energy balance (SEB) components of the GrIS at 11 km resolution, from the regional climate model RACMO2/GR (Van Meijgaard et al, 2008).
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