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Drought dynamics of Northwestern Teesta Floodplain of Bangladesh: a remote sensing approach to ascertain the cause and effect

机译:孟加拉国西北北部的干旱动态:一种确定原因和效果的遥感方法

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摘要

Drought is an affliction for a region that primarily depends on agriculture as economic activity. Commonly monitoring and characterizing of drought is performed by only analyzing the meteorological aspect, assuming precipitation as the primary source of water. However, in riverine Bangladesh, this can lead to an erroneous conclusion, as there is a multitude of available water sources. Consequently, in this study, vegetation condition (Standard Vegetation Index), soil moisture (Soil Moisture Index), and precipitation (Standard Precipitation Index) are separately investigated from 2003 to 2019, in the Northwestern Teesta floodplain. Subsequently, statistical regression analysis is performed to determine the relationships between different aspects of drought. In addition, information obtained from field visits and expert opinions has also been assimilated. Analysis of vegetation and soil moisture condition presents a progressively improving scenario. However, SPI shows an incessant decline in meteorological drought conditions, especially after 2007. Evidently, regression analysis does not provide any indication of an interrelationship between the studied agricultural and meteorological parameters. Presumably, this absence is instigated because the study area is highly irrigated as the groundwater table is suitably near the surface and the existence of nearby Teesta river allows for the utilization of surface water. Moreover, the cropping pattern is shifting toward crops that require much less water and to places where soil moisture is scarce. Thus, this study addresses the gap in knowledge regarding the nature of agricultural drought and the dynamics of different aspects of drought which will be invaluable for the water management and agricultural policy in the study area as well as other regions with a similar backdrop.
机译:干旱是一个主要取决于农业作为经济活动的地区的痛苦。通过仅分析气象方面,假设沉淀为主要水源,通过常见监测和表征干旱。然而,在河道孟加拉国,这可能导致错误的结论,因为有多种可用的水源。因此,在本研究中,从2003年至2019年,在西北部的洪泛区,植被条件(标准植被指数),土壤水分(土壤湿度指数)和降水(标准降水指数)分别调查。随后,执行统计回归分析以确定干旱的不同方面之间的关系。此外,从现场访问和专家意见获得的信息也已被同化。植被及土壤水分状况分析呈现出逐步改善情景。然而,SPI显示了气象干旱条件的不断下降,特别是在2007年之后。显然,回归分析不提供所研究的农业和气象参数之间的相互关系的任何指示。据推测,这种缺失是煽动的,因为在地下水表适合靠近地面和附近的Teesta河流的情况下,研究区域允许利用地表水的存在。此外,种植模式转向需要更少的水的作物和土壤水分稀缺的地方。因此,本研究解决了关于农业干旱性质的知识的差距以及对研究区域的水管理和农业政策以及其他有类似背景的其他地区的水流和农业政策的不同方面的动态。

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