Figure 3 - uploaded by Indrajit Pal
Content may be subject to copyright.
Human settlements affected by flash flood in state of Uttarakhand in June 2013, (a) Destruction of tourism infrastructure built over river bed (b) Buildings in steep hill slope in danger due to flash flood induced river bank erosion
Source publication
Many " Run of the River " projects in the North West part of Himalaya have been frequented by " Cloud Burst " induced flash flood in since 2009, which is primarily attributed to climate variability and land use pattern changes due to unregulated developmental perspectives against the rising demand of tourist related establishments. Given the ageing...
Contexts in source publication
Context 1
... damage potential of flash floods is confined to the direct neighbourhood of the river (Figure 3), where the total damage usually is not very extensive in spite of the high flow velocity. The individual damage to structures or persons in such floods is very high. ...
Context 2
... of rubble masonry is a routine practice in the hill roads ( Figure 12a) and vulnerability of such type of protection measures especially during heavy rainfall requires no special mention. However, typical soil nailing option as shown in Figure 12b or for some of the ongoing National Highways construction in the neighbouring state of Himachal Pradesh, where massive rouble masonry wall constructions are followed (Figure 13a), application of nailing technique followed elsewhere (Fig. 13b), can be adopted for the reconstruction hill slopes ravaged the flash flood in Uttarakhand. ...
Context 3
... during heavy rainfall requires no special mention. However, typical soil nailing option as shown in Figure 12b or for some of the ongoing National Highways construction in the neighbouring state of Himachal Pradesh, where massive rouble masonry wall constructions are followed (Figure 13a), application of nailing technique followed elsewhere (Fig. 13b), can be adopted for the reconstruction hill slopes ravaged the flash flood in ...
Similar publications
Extremely high precipitation is characteristic of the frontal zone of the Himalaya. In this article we study tributaries which supply huge sediment loads to the Teesta river in the Darjeeling Himalaya, India and significantly affect transportation regime downstream the junction of the Great Rangit with the main river. The material supply is also co...
Being within a geo-dynamically active Himalayan belt, the state of Uttarakhand is more susceptible to natural hazards due to inherent geology, high relief, narrow valley, thick
overburden, heavy downpour and rapid glacial melting etc. Over the past decades, these natural hazards have resulted in loss of human lives, infrastructures and properties...
Citations
... Field observations too, support the argument on the higher vulnerability of landslide prone areas than the flash floods ones, due to the higher frequency of flash flood hazards as com-pared to landslides, and the mitigation measures taken by the community based on economic status. However, even though communities in the flash flood group had more resilience, their disaster risk was still high because coordination between the government departments was absent, and disaster preparedness and mitigation programs were undertaken mostly in the landslide group [21]. In general, respondents were not aware of the hazards and risks that the landslides and flash floods could cause [22]. ...
This study's purpose is to analyze the degree of risk and vulnerability involved in landslide and flash flood prone community areas in Thepparat sub-district, Sichon district, Nakhon Si Thammarat province, Thailand. It also aims to analyze and understand the socioeconomic impacts on the community at the household level, and assess the community's risk and vulnerability by examining its risk perception. The risk perception was done using focus group discussions and a questionnaire survey with key stakehold-ers. It mainly focused on how the risk of landslides and flash floods influences the community's risk perceptions , which was tested in two parts: at the organizational and community levels by focusing on government officials and households, respectively. A correlation matrix was used to understand the relationship of the indicators selected. The Pearson correlation result has shown that the degree of risk awareness positively correlates with the income level, education level, and controllability, signifying that the risk of landslides and flash floods influences household risk perceptions. The qualitative assessment recommends community-level preparedness as being paramount to reduce the risk for a resilient community.