The 0.2 Climatic Event in the Levant During the Holocene Using Arehacoclimate Modeling and Archacological Synthesis
| المصدر: | أنباء |
|---|---|
| الناشر: | جامعة اليرموك - كلية الآثار والانثربولوجيا |
| المؤلف الرئيسي: | Al Shorman, Abdulla Alakkam (Author) |
| المجلد/العدد: | ع31 |
| محكمة: | نعم |
| الدولة: |
الأردن |
| التاريخ الميلادي: |
2011
|
| الصفحات: | 11 - 16 |
| ISSN: |
1021-5174 |
| رقم MD: | 878131 |
| نوع المحتوى: | بحوث ومقالات |
| اللغة: | الإنجليزية |
| قواعد المعلومات: | HumanIndex |
| مواضيع: | |
| رابط المحتوى: |
الناشر لهذه المادة لم يسمح بإتاحتها. |
| المستخلص: |
This study reconstructs the amount of precipitation in Jordan during the Holocene especially the cities of Damascus, Jericho and Beirut. Archaeoclimate modeling after Reid Bryson, which was designed based on Milankovitch principles and specially gathered data, was used to reconstruct the Holocene precipitation and temperature in these localities. The results indicated wetter climatic conditions at the beginning of the Holocene and four major and prolonged droughts at around 8200, 5200, 4200 and 2200 years PB (the 0.2 event). The archaeoloclimate model proves ifs full accordance with other paleoclimatic studies of the Levant. |
|---|---|
| ISSN: |
1021-5174 |
عناصر مشابهة
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The middle and late bronze age climate of Ya'amoun in northern Jordan using oxygen isotope analysis from human tooth enamel
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