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Regional drought assessment using improved precipitation records under auxiliary information

机译:利用辅助信息改进的降水记录进行区域干旱评估

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Changes in the climate and weather conditions, as well as rising earth’s average temperature are likely to escalate deterioration of global drought occurrence. Drought is considered an interwoven natural disaster composed by a number of different factors, as for example agricultural, meteorological or hydrological. Hydrological drought estimation with regional accuracy is the most problematic and challenging issue. In order to monitor and characterize drought conditions, using Standardized Drought Indices (SDI) is recently the most frequently used practice. In this research article, we suggest an improved hydrological drought index that incorporates upgraded monthly rainfall estimation records, which play an important role in defining regional drought conditions, with regard to the global temperature rise. Rainfall is highly changeable even at a low distance and therefore should be also considered in precipitation estimation records because temporal rainfall records play a significant role in determining long-term rainfall shortages. Thus, the integration of regional aspect to the amount of rainfall is essential for accurate regional drought assessment. This research article proposes adding auxiliary data such as regional weights in order to make monthly rainfall records more accurate in relation to the dependency characteristics of temperature and rainfall records under regression and product estimation settings. Subsequently, we propose an innovative method of hydrological drought evaluation, a so-called Regionally Improved Weighted Standardized Drought Index (RIWSDI). We evaluated hydrological drought with the usage of RIWSDI at seven various meteorological regions situated in climatologically different areas in Pakistan. We assessed and compared the results using RIWSDI, Standardized Precipitation Index (SPI) on 3 and 12-month interval period on the basis of Pearson correlation. Under both parametric and non-parametric standardization, we discovered that there is a high positive correlation between RIWSDI and current methodology (SPI). To sum up, we proved that the upgraded estimations of rainfall are able to improve systems for monitoring droughts.
机译:气候和天气条件的变化以及地球平均气温的上升可能会升级全球干旱发生的恶化。干旱被认为是由多种不同因素组成的交织自然灾害,例如农业,气象或水文。具有区域准确性的水文干旱估算是最有问题和最具挑战性的问题。为了监测和表征干旱条件,最近使用标准化的干旱指数(SDI)是最常用的练习。在本研究文章中,我们建议改进的水文干旱指数,该指数纳入了月度降雨估计记录,这在全球温度上升方面在确定区域干旱条件方面发挥着重要作用。降雨量甚至在低距离处高度变化,因此应在降水估计记录中考虑,因为时间降雨记录在确定长期降雨短缺方面发挥着重要作用。因此,区域方面与降雨量的整合对于准确的区域干旱评估至关重要。本研究文章建议添加辅助数据,如区域权重,以便每月降雨记录在回归和产品估算设置下的温度和降雨记录的依赖性特征方面更准确。随后,我们提出了一种创新的水文干旱评价方法,即所谓的区域改进的加权标准化干旱指数(RIWSDI)。我们评估了在巴基斯坦的气候上不同地区的七个各种气象区域的六种气象区的水文干旱。我们在3和12个月间隔期间使用RIWSDI,标准化降水指数(SPI)的结果进行了评估,并在Pearson相关性的基础上进行了评估。在参数和非参数标准化的情况下,我们发现RIWSDI和电流方法(SPI)之间存在高正相关性。总而言之,我们证明了降雨的升级估计能够改善监测干旱的系统。

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