Date: Fri, 21 Sep 2001 14:55:50 -0400 To: Steven_Wofsy@harvard.edu, nacp@python.as.harvard.edu, nacp@io.harvard.edu From: Michael Keller Subject: N2O Cc: harriss@ucar.edu, Patrick.Crill@unh.edu, changsheng.li@unh.edu, rbirdsey@fs.fed.us Dear Steve, At the last minute in the workshop, you put up a note on "other gases/N2O." I'm not sure where this fits into the plan. There are several linkages for the N and C cycles. For the N American situation Patrick and I see a few prominent examples: 1. Agricultural systems -- efforts to sequester carbon in agricultural soils are balanced out in part by increases in N2O emissions (e.g. Robertson et al. 2000; Science 289:1922-1925. The same effect may occur in fertilized forestry systems 2. Animal husbandry systems - N2O emissions can increase where aeration of waste is attempted to mitigate CH4 3. N-Deposition effects may lead to increased forest growth (although Caspersen says this is not so) in this case carbon sinks may also be offset by N2O releases. I'm not sure where this best fits in the current organization of the document. I think that perhaps when there is a more complete section on land sources and sinks, we should note these relations. - Michael ________________________________ Michael Keller Visiting Research Professor Complex Systems Research Center Morse Hall University of New Hampshire Durham, NH 03824 USA Voice +1 603 862 4193 Facsimile +1 603 862 0188 E-mail: michael.keller@unh.edu