By Martin O'Connor
Entire biographies of all forty nine brave aces of the twin Monarchy.
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Extra resources for Air aces of the Austro-Hungarian Empire, 1914-1918
1987. Bog proﬁle evidence of ﬁre and vegetation dynamics since 3000 years BP in the Acadian Forest. Can. J. Bot. 65:1180–1186. , in press. Charcoal as a ﬁre proxy. In Tracking Environmental Change Using Lake Sediments: Terrestrial, Algal, and Siliceous Indicators, eds. P. B. M. Last, vol. 3. Dordrecht: Kluwer Academic. , and Millspaugh, S. 1996. Testing assumptions of ﬁre history studies: An examination of modern charcoal accumulation in Yellowstone National Park. Holocene 6:7–15. G. 1985. Charcoal analysis for paleoenvironmental interpretation: a chemical assay.
J. Ecol. 86:815–828. I. 1998. Relations between lake morphometry and the presence of laminated lake sediments: A reexamination of Larsen and MacDonald (1993). Quat. Sci. Rev. 17:711–717. H. 1998. A 9000-year ﬁre history from the Oregon Coast Range, based on a high-resolution charcoal study. Can. J. For. Res. 28:774–787. A. 1991. The reconstruction of boreal forest ﬁre history from lake sediments: a comparison of charcoal, pollen, sedimentological, and geochemical indices. Quat. Sci. Rev. 10:53–72.
3). A locally 1. Fire History Reconstructions 19 weighted (moving) average is used to deﬁne the background component. It is calculated by moving a “window” along the CHAR series, and at each point determining a weighted average of CHAR values for the points contained in the window. The weight assigned to each point is based on the distance of the point from the center of the window so that points near the edge of the window have less inﬂuence than those near the center. This method of locally weighted averaging is related to the “lowess” approach for smoothing scatter diagrams (Cleveland 1979), and weights are determined using a tri-cube or approximately bell-shaped function.
Air aces of the Austro-Hungarian Empire, 1914-1918 by Martin O'Connor