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Woods Hole Oceanographic Institution

Elizabeth B. Kujawinski

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Projects
» Microbial metabolites in DOM

» DOM in the deep Atlantic Ocean

» Polar Petroleum & dispersants in Gulf oil spill

» Carbon cycle of Greenland Ice Sheet

» Heterotrophy, photochemistry & DOM

» FT-ICR MS in chemical oceanography

» Marine DOM: Microbial Influences

» Protozoa in subterranean estuaries

» Photochemical modifications of DOM


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Maya Bhatia sets up an incubation experiment in a supraglacial lake on the Greenland Ice Sheet in July 2007. (Maya Bhatia, WHOI)


Impact of a warming Arctic on hydrological flow routing and carbon transport from glaciated environments to the ocean

Collaborators:
Matthew A. Charette (WHOI Chemistry); Sarah B. Das (WHOI Geology & Geophysics); Emily Lawson (University of Bristol)

The Greenland Ice Sheet represents the largest expanse of glacial ice in the Northern hemisphere and is capable of contributing significant quantities of meltwater and associated carbon material to the surrounding North Atlantic and Arctic Oceans (IPCC, 2007). However, the potential impact of carbon cycle fluctuations in Greenland and other glaciated environments has been largely neglected in many climate change models. Under climatic warming, these environments may contribute a disproportionately large flux of water and sediment to their surroundings.  Here, we propose a novel multi-disciplinary approach to examine the interdependence of water and carbon cycles through the Greenland Ice Sheet. The primary objectives of this study are to establish a baseline flux of carbon export from glaciated Arctic environments by (1) assessing the timing and routing of meltwater through a large glacial system and (2) characterizing the magnitude, age and biological reactivity of the supraglacial (on the glacier surface) and subglacial (beneath the ice mass) carbon pools. To date, such first order characterization has not been undertaken, yet is requisite information for determining present carbon cycling beneath glaciated areas and the associated impact on the ocean.  By establishing present-day values of meltwater flow and the type of organic carbon present beneath glaciated areas, this study will serve as the needed foundation for broader investigations into the impact of increased meltwater runoff from Arctic glaciated environments to the surrounding marine environments.

Funding: WHOI Arctic Research Initiative

Personnel: Maya Bhatia (graduate student)

Publications:

Bhatia, M. P.+, S. B. Das, M. A. Charette, K. Longnecker+ and E. B. Kujawinski. 2010. Molecular characterization of dissolved organic matter associated with the Greenland ice sheet. Geochimica et Cosmochimica Acta. 74: 3768-3784.

Bhatia, M. P.+, S. B. Das, L. Xu, M. A. Charette, J. L. Wadham, and E. B. Kujawinski. Submitted (May 2012; 1st revisions underway Sept 2012). Organic carbon export from the Greenland ice sheet. Geochimica et Cosmochimica Acta.

Bhatia, M. P.+, S. B. Das, E. B. Kujawinski, P. Henderson, A. Burke, and M. A. Charette. 2011. Seasonal evolution of water source contributions to the subglacial outflow from a land-terminating Greenland ice sheet outlet glacier: Insights from a new isotope-mixing model. Journal of Glaciology. 57: 929-941.

Bhatia, M. P.+, S. B. Das, M. A. Charette, K. Longnecker+ and E. B. Kujawinski. 2010. Molecular characterization of dissolved organic matter associated with the Greenland ice sheet. Geochimica et Cosmochimica Acta.74: 3768-3784.


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