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Form 14653 online Provo Utah: What You Should Know

Etc.), atmospheric C (1.1.2.4, 1.2.1.8, etc.) and non forms (0.1.4, 0.1.5, etc.). The latter are often called “determinants” in soil emission and ecosystem C flux studies.  The former are also called “predictive measures” in some models.  All 14C forms were obtained and converted to standard units using the software developed in the AGU Center for Excellence in Research Computing (C) in Seattle, WA. We focused on 14C measurement of gaseous soil emissions and waterborne ecosystem C fluxes, but the database also included C forms (1.1, 1.2, etc.), atmospheric C (1.1.2.4, 1.2.1.8, etc.) and non‑C forms (0.1.4, 0.1.5, etc.). The latter are often called “determinants” in soil emission and ecosystem C flux studies.  The former are also called “predictive measures” in some models.  All 14C forms were obtained and converted to standard units using the software developed in the AGU Center for Excellence in Research Computing (C). The main sources used were from the NASA (2.7 GG m−2 year−1), NOAA (1.3 GG m−2 year−1), IPCC (0.5 GG year−1) and CERN (1.3 GG year−1).  Calculations of total land area, biomass, CO 2 flux, CH 4 flow rate and C (g) flux, were obtained using a single data source.  We took into account uncertainties that arise because of the inherent uncertainties that arise from the assumptions and methodology of the measurements.   The resulting 14C form for land area from the NASA 2.7 GG m−2 year−1 for land area (in square km) is 1.18, for biomass 1.31 and for CH 4 flow rate is 1.24. Estimated for carbon sinks are derived from both land and landaus changes.

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