1. 陕西师范大学旅游与环境学院,陕西,西安,710062
2. 宁夏师范学院政法学院,宁夏,固原,756000
纸质出版:2014
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丁彩霞, 延军平, 方兴义, 等. 宁夏地区气候暖干化与旱涝灾害趋势的关系[J]. 水土保持通报, 2014,33(2):250-254.
DING Cai-xia, YAN Jun-ping, FANG Xing-yi, et al. Relation of Climatic Dry-warming and Trend of Drought and Flood Disasters in Ningxia Region[J]. Bulletin of Soiland Water Conservation, 2014, 33(2): 250-254.
丁彩霞, 延军平, 方兴义, 等. 宁夏地区气候暖干化与旱涝灾害趋势的关系[J]. 水土保持通报, 2014,33(2):250-254. DOI: 10.13961/j.cnki.stbctb.2014.02.052.
DING Cai-xia, YAN Jun-ping, FANG Xing-yi, et al. Relation of Climatic Dry-warming and Trend of Drought and Flood Disasters in Ningxia Region[J]. Bulletin of Soiland Water Conservation, 2014, 33(2): 250-254. DOI: 10.13961/j.cnki.stbctb.2014.02.052.
依据宁夏地区11个气象站点1961-2012年实测气象数据
利用趋势线法、Z指数法、Mann-Kendall突变检验法及马尔科夫模型对宁夏地区气候变化特征和旱涝趋势进行了分析和预测。结果表明:(1)近52 a来宁夏地区气候经历了冷湿-暖湿-暖干的转变
气温呈显著波动上升趋势(0.36℃/10 a)
远高于西部平均变暖率(0.2℃/10 a);降水呈波动下降趋势
下降速率为9.94 mm/10 a。(2)旱涝灾害发生频次与气温变化具有一定的同步性。20世纪60-80年代中期气温变化不明显
旱涝趋势稳定;80年代中期到2006年气温大幅上升
旱涝灾害同步增加;2006-2012年增温趋势有所减缓
旱涝灾害相应减少。(3)运用马尔可夫模型对未来5 a的旱涝状态进行了预测
结果表明
2013-2017年该地区降水处于"正常"的概率较大。在气候暖干化的大背景下
未来宁夏地区旱涝灾害发生频率有可能进一步增加。
Based on the data observed from 11 meteorological stations in Ningxia Region from 1960 to 2012
the characteristics of climate change were analyzed and the trends of droughts and floods were forecasted with methods of linear regression
Z index
Mann-Kendall mutation test and Markov model. Results indicated as follows: (1) Ningxia regional climate changes experienced the three periods of cold-wet
warm-wet and warm-dry during the recent 52 years. The temperature fluctuations showed a significant upward trend with a rate of 0.36 ℃/10 a
far higher than the average warming rate(0.2 ℃/10 a) in Western China. The precipitation fluctuations showed a downward trend with a decreasing rate of 9.94 mm/10 a. (2) The frequencies of droughts and floods and temperature changes occurred with a certain synchronicity: from the 1960s to 1980s
the change of temperature was not significant and the tendencies of droughts and floods were stable; from the mid-1980s to 2006
temperature increased substantially and droughts and floods increased simultaneously; and from 2006 to 2012
warming trend occurred and the occurrence of droughts and floods was reduced correspondingly. (3) The state of droughts and floods in the next 5 years was forecasted using the Markov model. From 2013 to 2017
the probability of normal precipitation will be larger in Ningxia Region. In the backgrounds of warming and drying climate
the frequencies of droughts and floods are likely to increase further in the future.
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