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Impact of climate warming on drought characteristics of summer maize in North China Plain for 1961–2010

机译:1961 - 2010年北方夏季玉米干旱特色对夏季玉米干旱特色的影响

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North China Plain (NCP) is the major grain production region of the rain-fed summer maize and its natural climatic conditions play a decisive role in maize growth process. In this study, we focused on temporal-spatial characteristics of drought during maize growth period (June-September), and wanted to access the impact of climatic warming trend on summer maize drought during its growing season in NCP. To understand these questions, we used monthly mean air temperature and monthly precipitation data of 27 stations in NCP from 1961–2010. First, jumping points of mean temperature and precipitation in maize growth period were fixed by Mann-Kendall test method. Second, the self-calibrating Palmer Drought Severity Index (SC-PDSI) was used to calculate the drought level and the drought distribution characters were captured by empirical orthogonal function (EOF). Third, analyses of drought occurrence probability were conducted under two scenarios, i.e. one was actual observations, and another consisted of monthly actual precipitation for each year and past 50 years average of monthly mean temperature. Results showed that mean temperature and total precipitation in maize growth period were in a slightly decreasing trend before 1996, which was the jumping time point of mean temperature. After 1996, mean temperature of maize growth period was higher than the 50 years average of 0.4°C-1.0°C, while the trend of total precipitation in maize growth period was transferred from decreasing to increasing. The spatial character of drought occurrence in maize growth period showed consistency in NCP, and the most prone to drought and the hardest drought area was located in Henan Province. Drought occurrence probability increased by an average of 10.1% due to climate warming appeared since mid-1990s, and above severe drought increased in an average of 9% at the same time. These increase extent were higher than that of the decreased ones before the mid-1990s when - emperature was lower than 50 years average. In addition, the proportion of above severe drought occurrence also rose with the climate warming. Therefore, the warming trend would have a significant effect on drought occurrence of summer maize in NCP.
机译:华北平原(NCP)是雨喂养夏季玉米的主要粮食生产区及其自然气候条件在玉米生长过程中发挥着决定性作用。在这项研究中,我们专注于玉米生长期间(九月)(九月)期间干旱的时间空间特征,并希望在NCP生长季节期间进入气候变暖趋势对夏季玉米干旱的影响。要了解这些问题,我们在1961 - 2010年使用了NCP中的27个站的每月平均气温和每月降水数据。首先,通过Mann-Kendall测试方法固定玉米生长期间平均温度和沉淀的跳跃点。其次,使用自我校准的Palmer干旱严重性指数(SC-PDSI)来计算干旱水平,并且经过经验正交功能(EOF)捕获干旱分布字符。第三,在两种情况下进行干旱发生概率的分析,即一个是实际观察,另一个是每年的每月实际降水量和每月平均平均温度平均平均值。结果表明,玉米生长期的平均温度和总沉淀在1996年之前略有下降,这是平均温度的跳跃时间点。 1996年后,玉米生长期的平均温度高于50岁平均水平为0.4℃-1.0°C,而玉米生长期总沉淀的趋势从减少转移到增加。玉米生长期干旱发生的空间特征显示出NCP的一致性,最容易受干旱和最普根干旱地区。由于自20世纪90年代中期,由于气候变暖,干旱发生概率平均增长10.1%,同时平均较严重的干旱在9%上升。这些增加程度高于20世纪90年代中期的减少的程度,当水平低于50年的平均水平。此外,高于严重干旱发生的比例也随着气候变暖而上升。因此,变暖趋势将对NCP中夏季玉米的干旱发生效果显着影响。

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