Iteration, like friction, is likely to generate heat instead of progress. - George Eliot
Abstract
Scintillometer measurements of the turbulence inner-scale length \(l_\mathrm{o }\) and refractive index structure function \(C_n^2\) allow for the retrieval of large-scale area-averaged turbulent fluxes in the atmospheric surface layer. This retrieval involves the solution of the non-linear set of equations defined by the Monin–Obukhov similarity hypothesis. A new method that uses an analytic solution to the set of equations is presented, which leads to a stable and efficient numerical method of computation that has the potential of eliminating computational error. Mathematical expressions are derived that map out the sensitivity of the turbulent flux measurements to uncertainties in source measurements such as \(l_\mathrm{o }\). These sensitivity functions differ from results in the previous literature; the reasons for the differences are explored.
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Notes
Global partial derivatives are those that propagate from the dependent (derived) variable down to the independent (source measurement) variable through the entire tree diagram, whereas local partial derivatives propagate as if the equation being differentiated were independent of the rest of the equations in the set. An alternative to direct evaluation of global partial derivatives via the chain rule is a total-differential expansion (where all derivatives are local) of each equation in the set. This approach can be used to solve for global partial derivatives by re-grouping all total-differential terms into one equation. Readers may refer to Sokolnikoff (1939).
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Acknowledgments
The authors thank the Geophysical Institute at the University of Alaska Fairbanks for its support, Derek Starkenburg and Peter Bieniek for assistance with editing, two anonymous reviewers, one in particular, for very helpful comments. In addition, the authors thank Flora Grabowska of the Mather library for her determination in securing funding for open access fees. GJ Fochesatto was partially supported by the Alaska Space Grant NASA-EPSCoR program award number NNX10N02A.
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Appendices
Appendix A: Relations Between \(M\) and \(\zeta \)
Appendix B: Individual Terms in \(S_{T_\star ,\epsilon }\) for Unstable Conditions (\(\zeta <0\))
Appendix C: Individual Terms in \(S_{T_\star ,z}\) for Unstable Conditions (\(\zeta <0\))
Appendix D: Individual Terms in \(S_{u_\star ,\epsilon }\) for Unstable Conditions (\(\zeta <0\))
Appendix E: Individual Terms in \(S_{u_\star ,z}\) for Unstable Conditions (\(\zeta <0\))
Appendix F: Total Differential Expansion as in Andreas (1992) for Unstable Conditions (\(\zeta <0\))
Here we reproduce the analysis of Andreas (1992). Subscripts indicate the equation that is being differentiated locally. The coupled equations are
Combining these, we obtain
where the local derivatives are given by
Thus the expansion becomes
where \(dT_\star \) and \(dq_\star \) have been expanded in Andreas (1989) as
Thus we have
which gives us
where the terms \((S_{u_\star }-2)\) and \((S_z+1)\) are \((S_{u_\star }-4)\) and \((S_z+2)\) in Andreas (1992). Equations 90 and 91 reduce to Eqs. 44 and 46. Also from Andreas (1989) we have
where \(S_{u_\star }\) would be denoted here as \(S_{T_\star ,u_\star }\) and \(S_z\) would be written here as \(S_{T_\star ,z}\) for a large-aperture scintillometer strategy not involving the derivation of \(u_\star \) from Eq. 69. Equations 92 and 93 can be derived directly from the expressions in Andreas (1989) or they can be derived using the methodology outlined in this study. An alternative to using the results from Andreas (1989) in Eqs. 87 and 88 is to perform the total-differential expansion in Andreas (1992) from all the equations including an expansion of Eqs. 70 and 71, although the results are the same as here.
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Gruber, M., Fochesatto, G.J. A New Sensitivity Analysis and Solution Method for Scintillometer Measurements of Area-Averaged Turbulent Fluxes. Boundary-Layer Meteorol 149, 65–83 (2013). https://doi.org/10.1007/s10546-013-9835-9
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DOI: https://doi.org/10.1007/s10546-013-9835-9