904 resultados para John Simpson Kirkpatrick
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A torn scrap of paper which gives estimates of times worked for Fred Holmes, Joe Simpson, John Simpson, William Baird and William Case. Much of the text is missing. This is signed by Fred Holmes, Dec. 1857.
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On leaf preceding the t.p.: Battles of Chippawa and Lundy's Lane, by Charles Anderson, guide to the battle ground.
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On leaf preceding the t.p.: Battles of Chippawa and Lundy's Lane, by Charles Anderson, guide to the battle ground. On box: Chippawa and Lundy's Lane. Printed by John Simpson
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124 Briefe zwischen Leo Löwenthal und Max Horkheimer; 1 Brief von Leo Löwenthal an Theodor W. Adorno, 29.12.1954; 2 Briefe zwischen Max Horkheimer und Marjorie Fiske, 1954/1955; 2 Briefe zwischen Leo Löwenthal und Frederick Ungar, Oktober 1954; 2 Briefe zwischen Daniel Lerner und Leo Löwenthal, Oktober 1954; 3 Briefe zwischen Leo Löwenthal und Herbert Blumer, Oktober 1954; 1 Brief von Alice H. Maier an H. P. Edelman, 10.06.1954; 2 Briefe von Leo Löwenthal an The Trustes of Hermann Weil Memorial Foundation (New York), 27.04.1955; 1 Brief von Max Horkheimer an The Trustes of Hermann Weil Memorial Foundation (New York), Juni 1954; 4 Briefe zwischen Leo Löwenthal und Chauncy D. Harris, 1954/1955; 2 Briefe zwischen John I. Kirkpatrick und Leo Löwenthal, 1954; 3 Briefe zwischen Leo Löwenthal und R. Wendell Harrison, Mai 1954; 2 Briefe von Leo Löwenthal an Gustave E. von Grunebaum, 1954; 1 Brief von Leo Löwenthal an Morton Grodzins, 12.05.1954; 2 Briefe von Max Horkheimer an Charles Y. Glock, 1954; 1 Brief von Jeremiah Kaplan an Leo Löwenthal, 15.03.1954; 2 Briefe zwischen Leo Löwenthal und Max Rheinstein, März 1954; 1 Brief von Frederick Pollock an Max Rheinstein, [1954];
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Existing descriptions of bi-directional ammonia (NH3) land–atmosphere exchange incorporate temperature and moisture controls, and are beginning to be used in regional chemical transport models. However, such models have typically applied simpler emission factors to upscale the main NH3 emission terms. While this approach has successfully simulated the main spatial patterns on local to global scales, it fails to address the environment- and climate-dependence of emissions. To handle these issues, we outline the basis for a new modelling paradigm where both NH3 emissions and deposition are calculated online according to diurnal, seasonal and spatial differences in meteorology. We show how measurements reveal a strong, but complex pattern of climatic dependence, which is increasingly being characterized using ground-based NH3 monitoring and satellite observations, while advances in process-based modelling are illustrated for agricultural and natural sources, including a global application for seabird colonies. A future architecture for NH3 emission–deposition modelling is proposed that integrates the spatio-temporal interactions, and provides the necessary foundation to assess the consequences of climate change. Based on available measurements, a first empirical estimate suggests that 5°C warming would increase emissions by 42 per cent (28–67%). Together with increased anthropogenic activity, global NH3 emissions may increase from 65 (45–85) Tg N in 2008 to reach 132 (89–179) Tg by 2100.
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Mode of access: Internet.
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Mode of access: Internet.
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Arthur Ruppin