Using qflux to constrain modeled Congo Basin rainfall in the CMIP5 ensemble. Issue 22 (26th November 2016)

• Record Type: Journal Article
• Authors: Creese, A.; Washington, R.
• Is Part Of: Journal of geophysical research. Volume 121:Issue 22(2016)
• Page Start: 13, 415
• Page End: 13, 442
• Publication Date: 2016-11-26
• Subjects: Congo Basin rainfall -- moisture flux -- process‐based evaluation -- CMIP5 -- tropical circulation; Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1002/2016JD025596
• Languages: English
• ISSNs: 2169-897X

Abstract

Abstract: Coupled models are the tools by which we diagnose and project future climate, yet in certain regions they are critically underevaluated. The Congo Basin is one such region which has received limited scientific attention, due to the severe scarcity of observational data. There is a large difference in the climatology of rainfall in global coupled climate models over the basin. This study attempts to address this research gap by evaluating modeled rainfall magnitude and distribution amongst global coupled models in the Coupled Model Intercomparison Project 5 (CMIP5) ensemble. Mean monthly rainfall between models varies by up to a factor of 5 in some months, and models disagree on the location of maximum rainfall. The ensemble mean, which is usually considered a "best estimate" of coupled model output, does not agree with any single model, and as such is unlikely to present a possible rainfall state. Moisture flux (qflux) convergence (which is assumed to be better constrained than parameterized rainfall) is found to have a strong relationship with rainfall; strongest correlations occur at 700 hPa in March–May ( r = 0.70) and 850 hPa in June–August, September–November, and December–February ( r = 0.66, r = 0.71, and r = 0.81). In the absence of observations, this relationship could be used to constrain the wide spectrum of modeled rainfall and give a better understanding of Congo rainfall climatology. Analysis of moisture transport pathways indicates that modeled rainfall is sensitive to the amount of moisture entering the basin. A targeted observation campaign at key Congo Basin boundaries could therefore help to constrain model rainfall. Key Points: Coupled model rainfall climatologies differ by up to a factor of 5 over the Congo Moisture flux convergence is strongly related to rainfall at particular levels in the atmosphere in different seasons Measurements of moisture flux at the basin boundaries could constrain spectrum of model rainfall