| 鄂尔多斯高原地区清代旱灾与气候特征 |
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| 引用本文： | 奚秀梅,赵景波.鄂尔多斯高原地区清代旱灾与气候特征[J].地理科学进展,2012,31(9):1180-1185. |
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| 作者姓名： | 奚秀梅 赵景波 |
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| 作者单位： | 1. 陕西师范大学旅游与环境学院,西安710062 石河子大学理学院,石河子832003
2. 陕西师范大学旅游与环境学院,西安,710062 |
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| 基金项目： | 国家社会科学基金重大项目 |
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| 摘 要： | 通过对鄂尔多斯高原地区文献资料的搜集整理，研究了该区清代旱灾等级、频次、周期和气候特征。结果表明，鄂尔多斯高原地区清代旱灾频次较高，约0．34次／a，以轻、中度旱灾为主。该区旱灾的发生具有明显的阶段性，1701-1780年、1821-1845年和1876-1911年为多发阶段，1644—1700年、1781-1820年和1846-1875年为低发阶段。约90％的旱灾发生在春、夏季或春夏连旱。该区清代旱灾有7a左右的短周期，23．29a左右的中周期和54a左右的长周期；各等级旱灾有准5a短周期，特大旱灾的第1主周期是17a。干冷多风的区域气候环境，以及农业活动是该区旱灾发生的两个主要原因。推测该区清代发生大旱灾和特大旱灾年份的年降水量约为200-250mm，年蒸发量约为2400-2600mm。该区清代气候可划分为6个阶段：1644-1700年→1701-1780年→1781-1820年→1821—1845年→1846-1875年→1876-1911年，对应的年降水量特征为：多→少→多→少→多→少，而蒸发量和风沙天气特征为：少→多→少→多→少→多。确定1762-1766年、1875-1878年、1899-1902年为3个干旱气候事件，推测这3个干旱气候事件期间年平均降水量为230mm左右，蒸发量为2500mm左右，大风沙尘天气频繁。
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| 关 键 词： | 旱灾 等级 干旱化 小波分析 鄂尔多斯高原 |
Characteristics of Drought Disasters and Climate in Ordos Plateau during the Qing Dynasty |
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| XI Xiumei,ZHAO Jingbo.Characteristics of Drought Disasters and Climate in Ordos Plateau during the Qing Dynasty[J].Progress in Geography,2012,31(9):1180-1185. |
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| Authors: | XI Xiumei ZHAO Jingbo |
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| Institution: | 1(1.College of Tourism and Environment,Shaanxi Normal University,Xi’an 710062,China;2.College of Science,Shihezi University,Shihezi 832003,China) |
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| Abstract: | Based on materials collection and analysis,this paper studies grades,frequency and periodicity of the drought disasters and characteristics of the climate in Ordos Plateau region during the Qing Dynasty.The results show that the drought frequency is relatively high in this region during the Qing Dynasty(averaged 0.34 times/ year,and most were mild and moderate drought events.This paper divides the Qing Dynasty into several phases according to the drought frequency in this region.The phases of frequent drought occurrences include 1701-1780,1821-1845 and 1876-1911.The phases of seldom droughts occurrence includes 1644-1700,1781-1820 and 1846-1875.About 90% of the drought disaster events were observed in spring and summer or from spring into summer.In different time scales,the cycles of drought disaster occurrences are respectively 7a,23a,29a and 54 a.Each grade of droughts has a short quasi-cycle of 5a and the extreme droughts of first principal cycle are 17a.The occurrence of the droughts had two main reasons.One was dry and windy regional climate environment,and the other was human agricultural activities leading to vegetation damage and land desertification.This paper infers that the annual rainfall is 200~250 mm,and that the annual evaporation is 2400~2600 mm in extreme and severe drought years.The Qing dynasty climate in this region can be divided into six stages which are 1644-1700,1701-1780,1781-1820,1821-1845,1846-1875 and 1876-1911,respectively,and the corresponding annual rainfall is much,little,much,little,much and little,respectively,while the characteristics of evaporation and sandstorm weathers are little,much,little,much,little and much,respectively.What’s more,this paper infers that 1762-1766,1875-1878,1899-1902 are three dry phases.During the three phases,the annual rainfall was about 230 mm,and the evaporation was about 2500 mm,with frequent windy dust weather and drying trend in the Ordos Plateau region. |
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| Keywords: | drought grade drying trend wavelet analysis Ordos Plateau |
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