Ellenblum, Ronnie, 1952-2021
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- ספר: הישוב הכפרי הפראנקי בארץ-ישראל בתקופה הצלבנית, תשנ"א 1991.
- Author's The walls of Jerusalem, c1995:t.p. (Roni Ellenblum)
- Frankish rural settlement in the Latin Kindon of Jerusalem, 1997:t.p. (Ronnie Ellenblum; Hebrew Univ. of Jerusalem)
- The collapse of the eastern Mediterranean, 2012:ECIP t.p. (Ronnie Ellenblum; The Hebrew University of Jerusalem) data view (b. June 21, 1952)
- רוני אלנבלום; אהרן רוני אלנבלום; נולד ב-21 ביוני 1952 בבאר-שבע; נפטר ב-7 בינואר 2021; פרופסור מן המניין באוניברסיטה העברית בירושלים. גאוגרף והיסטוריון ישראלי שהתמחה בחקר ממלכת הצלבנים, בחקר הערים ההיסטוריות ובהיסטוריה סביבתית אקלימית. אלנבלום היה חבר האקדמיה הלאומית הישראלית למדעים, והיה עמית בקולג' קלייר הול בקיימברידג' ( (אתר: ויקיפדיה, נצפה ב-7 לינואר, 2021) )
Ronnie Ellenblum (Hebrew: רוני אלנבלום; born June 21, 1952, Haifa, Israel; died January 7, 2021, Jerusalem, Israel) was an Israeli professor at the department of geography at the Hebrew University of Jerusalem, and a member of the Israel Academy of Sciences and Humanities, specializing in Medieval geographies, the history of the Levant in the Middle Ages, and the history of the Crusades. His latest studies deal also with environmental and climatic history, the history of Jerusalem, and the development of historic cities in general. Ellenblum headed the Vadum Iacob Research Project and was involved in the creation of several databases dealing with the history of Jerusalem (together with al-Quds University); with the maps of Jerusalem and with English translations of documents and charters of the Crusader Period. Ellenblum has developed a comprehensive theoretical approach to 'Fragility,' claiming that a decade or two of climatic disturbance (droughts, untimely rains and severely cold winters) could lead to severe societal effects, and that the amelioration and even stabilization of climatic conditions for several decades can lead to a period of affluence. His theory of Fragility is based on a thorough reading of a wealth of well-dated textual and archaeological evidence, pointing to periods of collapse (in the eastern Mediterranean and northern China during the Medieval Climate Anomaly), and affluence in the entire Mediterranean Basin during the Roman Optimum, and describing these processes yearly, monthly and even daily.
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