Inverse problems in atmospheric constituent studies. I. Determination of surface sources under a diffusive transport approximation
- 1 October 1988
- journal article
- Published by IOP Publishing in Inverse Problems
- Vol. 4 (4) , 1037-1054
- https://doi.org/10.1088/0266-5611/4/4/008
Abstract
The authors study inverse problems arising in atmospheric chemistry. They study the structure of the particular problem of deducing the distribution of sources and sinks of carbon dioxide over the surface of the Earth from available concentration measurements coupled with a model of transport within the atmosphere. With a simplistic but reasonable model in which transport is by diffusion only, the problem of deducing the source distribution from surface concentration data is shown to be mildly ill-posed with linear growth in error amplification (conversely with linear damping of information). However, in practice the limited nature of available data does not allow full recovery of all information that is theoretically available. In contrast the deduction of the source distribution from high-altitude concentration data is shown to be severely ill-posed with exponential growth in error amplification.Keywords
This publication has 8 references indexed in Scilit:
- Inversion relations for the deconvolution of CO 2 data from ice coresInverse Problems, 1987
- Latitudinal variation in oxygen-18 of atmospheric CO2Nature, 1987
- Carbon isotope measurements of atmospheric CO2at a coastal station in AntarcticaTellus B: Chemical and Physical Meteorology, 1987
- Time and space variations of tropospheric carbon dioxide over JapanTellus B: Chemical and Physical Meteorology, 1987
- Interannual variation of atmospheric CO2 concentrationJournal of Atmospheric Chemistry, 1986
- A classification of some inverse problems in geochemical modellingTellus B: Chemical and Physical Meteorology, 1985
- Activities of the global biosphere as reflected in atmospheric CO2 recordsJournal of Geophysical Research: Oceans, 1980
- Large-scale atmospheric mixing as deduced from the seasonal and meridional variations of carbon dioxideJournal of Geophysical Research, 1963