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水文气象变量的回归分析在气候变化预测中的应用:以兴都库什地区奇特拉尔流域为例。

Regression analysis of hydro-meteorological variables for climate change prediction: A case study of Chitral Basin, Hindukush region.

机构信息

Department of Statistics, University of Peshawar, Peshawar 25120, Pakistan; Department of Statistics, Abdul Wali Khan University, Mardan 23200, Pakistan; Faculty of Sciences, University of Chitral, Chitral 17200, Pakistan.

Department of Statistics, University of Peshawar, Peshawar 25120, Pakistan.

出版信息

Sci Total Environ. 2021 Nov 1;793:148595. doi: 10.1016/j.scitotenv.2021.148595. Epub 2021 Jun 21.

Abstract

In the present study, hydro-meteorological variables of Chitral Basin in Hindukush region of Pakistan were studied to predict the changes in climatic components such as temperature, precipitation, humidity and river flow based on observed data from 1990 to 2019. Uncertainties in climate change projection were studied using various statistical methods, such as trend variability analysis via stationarity test and validation of regression assumptions prior to fitting of regression estimates. Also, multiple regression models were estimated for each hydro-meteorological variables for the given 30 years of observed data. Results demonstrated that temperature and, precipitation were inversely related with one another. It was observed from the regression model that temperature is decreases by 0.309 °C on the average increases in precipitation by one unit. Temperature also decreases for the increase in humidity by average 0.086 °C. Since, precipitation is negatively related with temperature, thus for increases in temperature the annual precipitation decreases by 0.278 mm annually. Humidity on the other hand, increases by 0.207% by increasing in precipitation and the temperature that causes humidity to decrease by 0.99%. Thus, it demonstrated that the flow in Chitral river increases due to precipitation by 0.306 m/s for the change in precipitation by one unit. Findings from the present study negated the general perceptions that flow in the Chitral river has increased due to recession of glaciers with increase in the intensity of temperature.

摘要

在本研究中,研究了巴基斯坦兴都库什地区奇特拉尔盆地的水文气象变量,以根据 1990 年至 2019 年的观测数据预测气候成分(如温度、降水、湿度和河流流量)的变化。通过 stationarity 测试分析趋势变化等各种统计方法研究了气候变化预测中的不确定性,并在拟合回归估计之前验证了回归假设。此外,还针对每个水文气象变量对给定的 30 年观测数据进行了多元回归模型估计。结果表明,温度和降水呈负相关。从回归模型中可以看出,温度平均每升高 1 摄氏度,降水就会减少 0.309°C。湿度每增加 0.086°C,温度也会降低。由于降水与温度呈负相关,因此温度升高时,年降水量每年减少 0.278 毫米。另一方面,降水每增加 1 单位,湿度就会增加 0.207%,而温度会使湿度降低 0.99%。因此,这表明由于降水的变化,奇特拉尔河的流量增加了 0.306 立方米/秒。本研究的结果否定了普遍认为奇特拉尔河的流量因冰川退缩和温度升高而增加的观点。

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