首页> 外文期刊>Arabian journal of geosciences >Spatio-temporal analysis of temperature variability, trend, and magnitude in the Hindu Kush region using Monte Carlo and Sen's slope approaches
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Spatio-temporal analysis of temperature variability, trend, and magnitude in the Hindu Kush region using Monte Carlo and Sen's slope approaches

机译:使用Monte Carlo和Sen的斜坡方法,印度苏珊区温度变异性,趋势和幅度的时空分析

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The present study explores the spatial and temporal deviations in temperature using Monte Carlo (MC) and Sen's slope (SS) approaches in the Hindu Kush (HK) region. Climate change holds sturdy association against the temperature trend that has generated adverse impacts in the form of floods. In this attempt, for trend analysis, temperature has been selected as a meteorological parameter. This study mainly focuses on exploring the tendency in average temperature with respect to time and the consequential flood recurrences in the region. For the current study, data regarding temperature were typically collected from Pakistan Meteorological Department. In the study region, there are a total of seven meteorological station falls namely Dir. Chitral, Drosh, Saidu, Malam Jabba, Kalam, and Timergara. The temperature time series data was calculated and analyzed using MC and SS approaches for trend detection in order to demonstrate the kind of fluctuation in the Hindu Kush region. The resultant analysis further revealed that in the meteorological station of Dir, a more significant positive trend (alpha = 0.0001) was found in mean monthly maximum, minimum, and monthly normal temperature. Likewise, at Drosh, a positive trend is detected in mean monthly maximum (alpha = 0.04), monthly minimum (alpha = 0.003), and monthly average (alpha = 0.0005). Moreover, at Saidu met station, there is also a trend detected in temperature sub-variables such as monthly maximum (alpha = 0.0001) and monthly minimum (alpha = 0.001). In addition to these, at Kalam, there is a temperature trend noted for monthly minimum (alpha= 0.01) and monthly average (alpha= 0.02). Furthermore, the analysis demonstrates that there is no trend detected in the remaining stations, i.e., Chitral, Malam Jabba, Drosh, and Timergara. The overall analysis discovered that there is a sturdy relationship between climate change phenomenon and temperature variability. After using SS test to the temperature data of mean monthly maximum (TMMMax), the results explored that Kalam station grips the highest magnitude, i.e., Q = 0.76; however, Timergara shows the lowermost, i.e., Q = -0.34. For the monthly minimum temperature (TMIVLMin), at Kalam again, the highest value (Q = 0.005) was detected; however, other stations revealed a negative trend, except Drosh which express no change in terms of magnitude. Similarly, in terms of monthly normal temperature (TMNor), Timergara station (Q = - 0.4) verified a negative trend magnitude and Malam Jabba station again trendless. Among all, the met station of Malam Jabba which holds an altitude of 2591 m is a hilly station just followed by Kalam having 2103 m height; however, Dir holds 1375 m height and the rest of the met stations show low elevation. The main reason for the temperature difference is the altitude of the study region.
机译:本研究探讨了使用印度科河(HK)区域的蒙特卡罗(MC)和SEN的斜坡(SS)方法温度的空间和时间偏差。气候变化持有坚固的抗于温度趋势的趋势,这些趋势产生了洪水形式产生不利影响。在这种尝试中,对于趋势分析,已经选择了温度作为气象参数。本研究主要侧重于探索与该地区的时间和相应的洪水复发的平均气温趋势。对于目前的研究,通常从巴基斯坦气象部门收集温度的数据。在研究区,共有七个气象站落下即行。十四行,德罗什,撒但,摩拉姆·贾巴,卡拉姆和Timergara。使用MC和SS方法计算和分析温度时间序列数据,以便展示印度苏豪地区的波动。所得到的分析进一步揭示了在DIR的气象站中,在平均每月最大,最小和每月常温下发现更显着的正趋势(α= 0.0001)。同样地,在Drosh,在平均月度最大(alpha = 0.04),月度最小(alpha = 0.003)和月平均值(alpha = 0.0005)中检测到正趋势。此外,在SEDU MET站,在温度子变量(例如月度最大值)和月度最小值(alpha = 0.001)中也存在一个趋势。除此之外,在Kalam,每月最小(alpha = 0.01)和月平均值(alpha = 0.02)的温度趋势。此外,分析表明,剩余站中没有检测到的趋势,即克里克,哈拉姆Jabba,Drosh和Timergara。整体分析发现,气候变化现象和温度变化之间存在坚固的关系。在使用SS测试到平均月度最大值(TMMMAX)的温度数据后,结果探索了卡拉姆站夹持最高幅度,即Q = 0.76;然而,Timergara显示最低原,即Q = -0.34。对于每月最低温度(TMIVLMIN),再次在KALAM时,检测到最高值(Q = 0.005);然而,其他车站揭示了消极趋势,除了讨论,表达幅度没有变化。同样,就每月常温(TMNOR)而言,TIMERGARA站(Q = - 0.4)验证了负趋势幅度和摩尔姆JABBA站的不起作用。其中,拥有海拔2591米的Malam Jabba的MAT站是一个丘陵站,刚刚接下来是哈拉姆,高度为2103米;然而,DIR容纳1375米的高度,其余的Met站显示出低升高。温差的主要原因是研究区的高度。

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