首页> 外文期刊>Journal of Science and Technology of Agriculture and Natural Resources >Investigating the Temporal and Spatial Variation of Snow Depth over Mountainous Region of Zagros, Iran, for the Period 1979-2010
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Investigating the Temporal and Spatial Variation of Snow Depth over Mountainous Region of Zagros, Iran, for the Period 1979-2010

机译:1979-2010年伊朗扎格罗斯山区积雪深度的时空变化调查

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In this study, the temporal and spatial variation of snow depth over the mountainous region of Zagros, in the western Iran, for the period 1979 2010 was investigated for the cold season when the probability of snow occurrences was high. For this purpose, daily gridded snow depth data relative to Era-Interim/land were retrieved from the European Centre for Medium-Range Weather Forecasts (ECMWF) and used for spatiotemporal analysis of snow in the region. Furthermore, monthly maximum, minimum and mean air temperature relative to the weather stations distributed over the region were also used to investigate the relationship between snow depth and air temperature variability in the region. In each grid point, the rate of temporal changes in the snow depth was estimated using the Sen's slope estimator, while the modified Mann-Kendall Test was applied to assess if the change identified was statistically significant. The results showed that in almost all of the studied months, especially February and March, the snow depth was significantly reduced in the region, which was statistically significant at 5% significant level. Unlike the observed statistically significant decreasing trend in the depth snow in the region, a significant increase in the maximum, minimum and average temperature was observed for all the studied months and the stations. The result suggested that the observed decrease in the snow depth in the region was related to the increasing trend in the temperature during the study period, which could be attributed to the global warming and climate change.
机译:在这项研究中,调查了伊朗西部Zagros山区1979年至2010年期间积雪发生概率较高的寒冷季节的积雪深度时空变化。为此,从欧洲中距离天气预报中心(ECMWF)检索了相对于中期/陆地的每日网格化雪深数据,并将其用于该地区雪的时空分析。此外,还使用相对于分布在该地区的气象站的每月最高,最低和平均气温来调查该地区积雪深度与气温变化之间的关系。在每个网格点,使用Sen的斜率估算器估算雪深的时间变化率,同时使用改进的Mann-Kendall检验来评估所确定的变化是否具有统计学意义。结果表明,在几乎所有研究的月份中,尤其是2月和3月,该地区的积雪深度均显着减少,在5%的显着水平上具有统计学意义。与该地区深度降雪在统计学上观察到的显着下降趋势不同,在所有研究月份和观测站中,最高,最低和平均温度均出现了显着增加。结果表明,该地区观测到的积雪深度减少与研究期间温度升高趋势有关,这可能归因于全球变暖和气候变化。

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