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Fifty-year rainfall change and its effect on droughts and floods in Wenzhou, China

机译:温州五十年来的降雨变化及其对旱涝的影响

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摘要

Based on daily, monthly, seasonal and annual precipitation, monthly duration and flood-affected area data from 1954 to 2007, we examined the absolute and relative change trends of rainfall and their effects on hazard intensity in Wenzhou city, China. The long-term trend of precipitation was studied by linear regression, moving average, cumulative anomaly and Z index methods, respectively. Our results show that there was no significant downward trend of annual precipitation. In contrast, there was significant decrease in autumn, July, mid-January and early June and significant increase in early January and late May, especially in late June. During 1954 and 2007, although significant fluctuation existed in the absolute value of precipitation, the relative changes of wet and dry were not significant compared with the average. The 10-year decrease in precipitation was 23.37 mm in autumn, 14.85 mm in July, 0.33 mm in mid-January and 6.87 mm in early June; while the 10-year increase was 0.35 mm in early January, 3.05 mm in late May and 8.57 mm in late June, respectively. Moreover, we found that 1964, 1966, 1977 and 1995 were the transition periods when the rainfall Z index was at peaks, the flood intensity was high, and the drought intensity was relatively low. On the other hand, 1958, 1968, 1971, 1980, 1989 and 1992 were the periods when the rainfall Z index was at valleys, the flood intensity was low, and the drought intensity was relatively high. Taken together, we demonstrated the obvious effects of precipitation changes on flood and drought intensities.
机译:基于1954年至2007年的日,月,季和年降水量,月持续时间和受洪灾影响的区域数据,我们研究了中国温州市降雨的绝对和相对变化趋势及其对灾害强度的影响。分别通过线性回归,移动平均,累积异常和Z指数方法研究了降水的长期趋势。我们的结果表明,年降水量没有明显的下降趋势。相反,秋季,7月,1月中旬和6月初显着下降,1月初和5月下旬(尤其是6月下旬)显着增加。在1954年至2007年期间,尽管降水绝对值存在明显的波动,但干湿的相对变化与平均值相比没有显着变化。 10年降水量的减少在秋季是23.37毫米,在7月是14.85毫米,在1月中旬是0.33毫米,在6月初是6.87毫米;而10年的增长分别是1月初的0.35毫米,5月下旬的3.05毫米和6月下旬的8.57毫米。此外,我们发现1964、1966、1977和1995年是降雨Z指数达到峰值,洪水强度高,干旱强度相对较低的过渡时期。另一方面,1958、1968、1971、1980、1989和1992年是降雨Z指数处于谷地,洪水强度低,干旱强度相对较高的时期。两者合计,我们证明了降水变化对洪水和干旱强度的明显影响。

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