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Filtering by: Funding statement C.R.S., C.A.W. and K.S. were supported by the US National Science Foundation grant ATM-0910766. C.A.W. was additionally supported through NASA Terrestrial Ecology award NNX10AR68G (2N041). B.E.L. was supported by AmeriFlux (the Office of Science (BER), US Department of Energy (DE-FG02-04ER63917 and DE-FG02-04ER63911)). K.T.P.U. was supported by the US National Science Foundation grant F1137306/MIT subaward 5710003122 to the University of California, Davis.

Reduction in carbon uptake during turn of the century drought in western North America

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Schwalm, Christopher R., Williams, Christopher A., Schaefer, Kevin, Baldocchi, Dennis D., Black, T. Andrew, Goldstein, Allen H., Law, Beverly E., Oechel, Walter C., Paw U, Kyaw Tha, and Scott, Russel L.

Abstract:

Fossil fuel emissions aside, temperate North America is a net sink of carbon dioxide at present¹⁻³. Year-to-year variations in this carbon sink are linked to variations in hydroclimate that affect net ecosystem productivity³,⁴. The severity and incidence of climatic extremes, including drought, have increased as a result of climate warming⁵⁻⁸....

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supported by the US National Science Foundation grant F1137306/MIT subaward 5710003122 to the University of

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Reduction in carbon uptake during turn of the century drought in western North America

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