Michael Trolier

TL;DR: In this paper, the authors performed an inverse deconvolution of both CO2 and delta C-13 observations, using a two-dimensional model of atmospheric transport, and determined the partitioning of the net uptake of CO2 between ocean and land as a function of latitude and time.

TL;DR: In this article, the global surface fluxes of O-18 for vegetation and soils using the SiB2 biosphere model coupled with the Colorado State University general circulation model were calculated, and it was shown that exchange with the canopy produces an isotopic enrichment of CO2, whereas exchange with soils has the opposite effect.

TL;DR: The stable isotopic composition of atmospheric CO2 is monitored via measurements made at the University of Colorado-Institute of Arctic and Alpine Research, using air samples collected weekly by the Global Air Sampling Network of the NOAA Climate Monitoring and Diagnostics Laboratory as mentioned in this paper.

TL;DR: In this paper, the authors used a tracer model to simulate the atmospheric CO2 and found that the shape of the latitudinal profile of the CO2 is determined primarily by the respiration of the land biota, which balances photosynthetic uptake over the course of a year.

TL;DR: In this paper, the product of subject reaction was detected in v'=2 and v' = 3 with full resolution of N', f', λ' sublevels using LIF spectroscopy in the off-diagonal Δv=−2 sequence bands in the region 385-409 nm.