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publications > paper > estimating changes in heat energy stored within a column of wetland surface water and factors controlling their importance in the surface energy budget > appendix a

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Appendix A

[59] This appendix documents the solution of ordinary differential equation (4) to obtain equation (5) described in this paper. Equation (4) is expressed as

equation 4. D

Rearrange and integrate equation (4) so that

equation A1. (A1) D

Let x = (Tew - Tw) and then dx = d(Tew - Tw). Substitute x and dx into equation (A1) where:

equation A2, (A2) D

which equals

equation A3. (A3) D

Take the exponent of both sides so that equation (A3) equals

equation A4; (A4) D

note that C2 equals e raised to the power of C sub1.

[60] Substitute back for x so that equation (A4) equals

equation A5 (A5) D

If we solve equation (A5) at the initial condition of t = 0, then

equation A6. (A6) D

Introduce the assumption that a given air temperature change, delta symbolTa [T], eventually causes an equivalent water temperature change, where the water temperature change is expressed as the difference between the equilibrium and actual water temperatures, thus

equation A7. (A7) D

Substitute delta symbolTa in equation (A5) so that

equation A8. (A8) D

By rearranging equation (A8), the formula becomes equation (5), which is

equation 5. D

[61] Acknowledgments. The U.S. Geological Survey (USGS) and South Florida Water Management District jointly funded this study. Eric Swain (USGS, Miami, Florida) helped derive equations. Mark Zucker (USGS, Miami, Florida) provided review comments and identified statistical methods appropriate for application in this study. Robert Renken (USGS, Miami, Florida), Amy Swancar (USGS, Tampa, Florida) and three anonymous Water Resources Research reviewers provided comments that improved the manuscript quality. Review comments from Water Resources Research Associate Editor Michiaki Sugita are gratefully acknowledged for substantially improving the manuscript quality.

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