Acronym: OCB-023
Program: Ocean Carbon & Biogeochemistry [OCB]
URL: Project Web Site
Start date:
End date:
Geolocation: North Atlantic
Description:

from www.us-ocb.org

We lack a clear understanding of how the subpolar North Atlantic carbon sink responds to climate change, despite the fact that this is a region of significant mean carbon uptake (Sabine et al. 2004). The vast majority of carbon cycle observations are of surface ocean pCO2, with strong seasonal to interannual timescale variability. This variability makes it difficult to distinguish trends, though several authors have tried (Lefevre et al. 2004, Omar and Olsen, 2006, Corbiere et al. 2007, Thomas et al. 2007). Numerical models are now able to capture a significant amount of physical and biogeochemical variability (Lima and Doney, 2004), and need to be used, in conjunction with data, to assess carbon cycle trends. In this project, I will use a North Atlantic regional model with newly-available data to ask: (1) How well can a physical-biogeochemical model capture in-situ observations of surface ocean pCO2 in the North Atlantic? (2) Has there been a trend in the subpolar North Atlantic carbon sink in recent decades? (3) If trends are not yet notable, how much sampling will be required to distinguish trends from variability?

In the educational component, I will enhance the climate curriculum at UW-Madison and train high school teachers in climate and climate modeling, with a focus on carbon-climate interactions. Central to these efforts will be the EdGCM, a user-friendly version of the NASA GISS climate model. Curriculum will be designed to enhance the EdGCM experience by including carbon cycle investigations. The ultimate goal of this effort is to enhance climate and carbon cycle science literacy in the general public through UW-Madison and high school graduates.

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More information about project Modeling the carbon cycle and climate: Ocean processes to global predictions
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