资源环境科技发展态势分析平台

To better understand and quantify the impact of clouds on the Greenland Ice Sheet surface mass balance (SMB), we study the spatiotemporal variability of the cloud radiative effect (CRE). The total CRE is separated in short-term and long-term impacts by performing multiple simulations with the SNOWPACK model for 2001-+2010. The annual total CRE is 16.8 +/- 4.5 W m(-2), reducing the SMB with -157 +/- 3.8 Gt yr(-1). Summer cloud radiative cooling is -6.4 +/- 5.7 W m(-2) in the ablation area, increasing the SMB with 121 +/- 2.2 Gt yr(-1). The annual integrated impact is cloud-reduced SMB of -36 Gt yr(-1). The short-term effect dominates the opposing long-term effects through the albedo-melt feedback. A long-term warming effect decreases the albedo and so preconditions the surface for enhanced (summer) melt. The impact of the CRE, determined by spatial, temporal and initial conditions, explains existing conflicted views on the role of cloud radiation and emphasizes the need for accurate cloud and albedo representations in future studies.