Investigating the spread in surface albedo for snow‐covered forests in CMIP5 models. Issue 3 (5th February 2016)

• Record Type: Journal Article
• Authors: Wang, Libo; Cole, Jason N. S.; Bartlett, Paul; Verseghy, Diana; Derksen, Chris; Brown, Ross; von Salzen, Knut
• Is Part Of: Journal of geophysical research. Volume 121:Issue 3(2016)
• Page Start: 1104
• Page End: 1119
• Publication Date: 2016-02-05
• Subjects: surface albedo -- leaf area index -- climate model -- snow cover -- boreal forest -- CMIP5; Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1002/2015JD023824
• Languages: English
• ISSNs: 2169-897X

Abstract

Abstract: This study investigates the role of leaf/plant area index (LAI / PAI) specification on the large spread of winter albedo simulated by climate models. To examine the sensitivity of winter albedo to LAI, we perform a sensitivity analysis using two methods commonly used to compute albedo in snow‐covered forests as well as diagnostic calculations within version 4.2 of the Canadian Atmospheric Model for which PAI is systematically varied. The results show that the simulated albedo is very sensitive to negative PAI biases, especially for smaller PAI values. The LAI and surface albedo of boreal forests in the presence of snow simulated by the Coupled Model Intercomparison Project Phase 5 (CMIP5) models are evaluated using satellite observations. The evaluation of CMIP5 models suggest that inaccurate tree cover fraction due to improper plant functional type specification or erroneous LAI parameterization in some models explains, in part, an observed positive bias in winter albedo over boreal forest regions of the Northern Hemisphere. This contributes to a large intermodel spread in simulated surface albedo in the presence of snow over these regions and is largely responsible for uncertainties in simulated snow‐albedo feedback strength. Errors are largest (+20–40%) in models with large underestimation of LAI but are typically within ±15% when simulated LAI is within the observed range. This study underscores the importance of accurate representation of vegetation distribution and parameters in realistic simulation of surface albedo. Key Points: Large spread of winter albedo is linked to spread in simulated leaf area index Errors in PFT simulation can lead to errors in simulated TCF and LAI Corrections of underestimation in TCF and LAI will likely limit the albedo bias to ±15%