993 resultados para 1600-1681.


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This layer is a georeferenced raster image of the historic paper map entitled: Fac-simile of a portion of Holme's map of the Province of Pennsylvania : with names of original purchasers from William Penn 1681. It was published by L. H. Everts & co. ca. 1884. Scale not given. Facsimile of a map published in 1681. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Pennsylvania South State Plane Coordinate System NAD83 (in Feet) (Fipszone 3702). All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. Cadastral map showing townships, landowner names, property boundaries, drainage, and more. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

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According to colophon (f. 143r), copy completed in the hand of al-Shaykh Muḥammad al-Khurāsānī towards the end of Dhū al-Ḥijjah 1008 AH [July 1600 AD].

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The current understanding of preindustrial stratospheric age of air (AoA), its variability, and the potential natural forcing imprint on AoA is very limited. Here we assess the influence of natural and anthropogenic forcings on AoA using ensemble simulations for the period 1600 to 2100 and sensitivity simulations for different forcings. The results show that from 1900 to 2100, CO₂ and ozone-depleting substances are the dominant drivers of AoA variability. With respect to natural forcings, volcanic eruptions cause the largest AoA variations on time scales of several years, reducing the age in the middle and upper stratosphere and increasing the age below. The effect of the solar forcing on AoA is small and dominated by multidecadal total solar irradiance variations, which correlate negatively with AoA. Additionally, a very weak positive relationship driven by ultraviolett variations is found, which is dominant for the 11 year cycle of solar variability.

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Includes bibliographies and index.

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Edited by C.E. Pastoret.

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Two volumes in continuation and a new edition of this first volume were published by Isak Collijn (Uppsala, 1927-38) with title: Sveriges bibliografi intill ȧr 1600.

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Anthony van Dyck; 2 ft. 9 15/64 in.x 3 ft. 3 9/64 in.; oil on canvas

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Mode of access: Internet.

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"Authorities": at end of each lecture except 1st and 78th.

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Maps on lining papers.