396 resultados para 1286


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[ʻAbd al-Muḥsin al-Qayṣarī].

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li-Abī al-Thanāʼ Shams al-Dīn ibn Maḥmūd ibn ʻAbd al-Raḥmān al-Iṣfahānī. Maʻa matnihi Ṭawāliʻ al-anwār / li-ʻAbd Allāh ibn ʻUmar al-Bayḍāwī. wa-bi-hāmishihimā Ḥāshiyat al-Sayyid al-Sharīf al-Jurjānī.

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taʼlīf Rifāʻah Rāfiʻ.

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History of Indian Muslim kings and rulers, 12th to 19th century.

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[Aḥmad Khalīl al-Fawzī ibn Muṣṭafá al-Filibawī].

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1. Risālah fī ādāb al-muṭālaʻah / Ḥāmid ibn Burhān ibn Abī Dharr al-Ghifārī (ff. 1r-6v) -- 2. Ādāb ʻUthmānīyah (ff. 7r-14r) -- 3. Ādāb Sharīfīyah fī al-munāẓarah / al-Sayyid al-Sharīf al-Jurjānī (ff. 15r-27r) -- 4. Sharḥ ādāb al-baḥth fī ʻilm al-munāẓarah lil-ʻAḍudī (ff. 28r-46v) -- 5. Ḥāshiyah ʻalá Sharḥ Ādāb al-Ḥanafī (ff. 47r-55v).

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Written in one column, 21 lines per page, in black and red.

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Copyright © 2016 by the American College of Sports Medicine

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The permanent exhibition of the Staatliches Museum für Naturkunde Stuttgart, Schloss Rosenstein, contains the cross section of a California coast redwood tree (Sequoia sempervirens) from Humboldt County, California, felled in 1966 reveals 1285 annual tree-rings. The measured thicknesses of tree-rings comprise a time series with distinct thickness variations, which are the expression of changing environmental conditions such as precipitation and fog. These factors are controlled by nearby coastal upwelling, which is again influenced by El Nino-Southern Oscillation (ENSO), and which in turn can be influenced by variations of solar radiance. In fact, the tree-ring time series comprises evidence for three orders of solar cycles that may have indirectly controlled tree growth: Hale cycle (21.9 yr), Gleissberg cycle (88.6 yr) and De Vries cycle (209.8 yr). These interpretations should, however, be treated with caution, because it is the only cross section known and the acquirement of reliable data requires cross dating of several sections. (was: The cross section of a California coast redwood tree (Sequoia sempervirens) felled in 1966 reveals 1285 annual tree-rings. The measured thicknesses of tree-rings comprise a time series with distinct thickness variations, which are the expression of changing environmental conditions such as precipitation and fog. These factors are controlled by nearby coastal upwelling, which is again influenced by El Nino-Southern Oscillation (ENSO), and which in turn can be influenced by variations of solar radiance. In fact, the tree-ring time series comprises evidence for three orders of solar cycles that may have indirectly controlled tree growth: Hale cycle (21.9 yr), Gleissberg cycle (88.6 yr) and De Vries cycle (209.8 yr).

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Published also under title: al-Mukhtaṣar fī akhbār al-bashar.

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Supplementum Historiae dynastiarum in quo orientalis series ..., con port. propia, 368 p.