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W.L. Anderson

Publications and source records attributed to W.L. Anderson.

At least 19 recordsLinked to original sources

Evidence of recent warming and El Nino-related variations in ice breakup of Wisconsin lakes

Ice breakup dates from 1968 to 1988 were examined for 20 Wisconsin lakes to determine whether consistent interannual and long-term changes exist. Each ice record had a trend toward earlier breakup dates, as demonstrated by a negative slope with time, indicating a recent warming trend. The average change in breakup dates was 0.82 d earlier per year for the lakes in southern Wisconsin, which was more extreme than that for the northern Wisconsin lakes (0.45 d yr-1). Interannual variation in breakup dates was related to the warm phase of El Nino/Southern Oscillation (ENSO) episodes. El Nino events occurred five times during this period (1965, 1972, 1976, 1982, and 1986). Average breakup dates were significantly earlier than average (5-14 d) during the mature phase of El Nino. This variability was affected by the location of the lake: El Nino-related variation was more evident for the southern lakes than the northern lakes. This difference was caused by the average date of breakup for the southern lakes being in late March directly following the period when air temperatures were strongly related to El Nino events, whereas the average dates of breakup of the northern lakes was in mid- to late April following a period when air temperatures were not significantly related to El Nino events. Overall, the interannual and long-term patterns across Wisconsin were relatively consistent, indicating that recent warming and El Nino- related variation are regional climatic responses.

Limnology and Oceanography↗

Interactive inversion of dipole loop-loop electromagnetic data for layered earth models using numerical integration and complex image theory (version 1.0)

This report is provided as a reference guide to define the basic graphical user interface (GUI) responses needed to perform interactive forward or inverse modeling of dipole loop-loop electromagnetic (EM) data using an IBM compatible personal computer (PC). The underlying model used is a one-dimensional (1-D) horizontal layered earth with parameters being the layer resistivities and thicknesses below the earth's surface. Mathematical details of the layered earth modeling are summarized below and in Appendix 1 that describes two general methods: numerical integration and complex image theory to compute forward or inverse sounding curves in the frequency-domain. Any combination of 5-different dipole loop-loop geometries can be selected in the modeling. The program in this report is named INVDP (for INVersion of DiPole data).

Open-File Report↗

A hybrid fast Hankel transform algorithm for electromagnetic modeling

A hybrid fast Hankel transform algorithm has been developed that uses several complementary features of two existing algorithms: Anderson's digital filtering or fast Hankel transform (FHT) algorithm and Chave's quadrature and continued fraction algorithm. A hybrid FHT subprogram (called HYBFHT) written in standard Fortran-77 provides a simple user interface to call either subalgorithm. The hybrid approach is an attempt to combine the best features of the two subalgorithms to minimize the user's coding requirements and to provide fast execution and good accuracy for a large class of electromagnetic problems involving various related Hankel transform sets with multiple arguments. Special cases of Hankel transforms of double-order and double-argument are discussed, where use of HYBFHT is shown to be advantageous for oscillatory kernel functions.

Geophysics↗