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Mallick, D.; Dilshad, T.; Naznin, Z.; Hassan, T. S. M.; Md. Syed, A.; Goodrich, C. G.; Udas, B. P.; Prakash, A.; Anwar, M. Z.; Habib, N.; Abbasi, S. S.; Khan, Q.; Ali, M.; Qureshi, A. H.; Batool, S.; Bhadwal, S.; Khandekar, N.; Gorti, G.; Mini, G.; Varma, N.; Sharma, G.; Luitel, M.; Nyima, K.; Tamang, D. D.
This synthesis report summarizes findings from a participatory assessment of socio-economic drivers, conditions, and climatic and environmental stresses leading to different levels of vulnerabilities in the Hindu Kush Himalayan (HKH) region
. The study sites included high mountain, mid-hill, and downstream regions of the Indus, Upper Ganga, Gandaki, and Teesta– a tributary of the Brahmaputra River – basins. An integrated and multidimensional approach was adopted to understand social drivers, conditions, climate stresses, and multiple causes of vulnerability. Community perceptions about major socio-economic drivers and conditions were collected in geographical contexts. Upstream regions are characterized by an abrupt rise in topography, extremely rugged terrain, steep slopes, and deeply cut valleys. Midstream characteristics include hills with large areas of dense broad-leaved and mixed forest and extensive agriculture, often on terraced slopes. Downstream areas are mostly flat and characterized by vast floodplains that are prone to flood and river erosion
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Vulnerability is a set of conditions of people that is derived from the historical and prevailing socio-economic, cultural, environmental and political contexts along with understanding future scenarios, especially for climate change
. This study aimed at better understanding the nature and types of socio-economic drivers and social vulnerabilities in the context of increasing climatic stresses in four river basins in the Hindu Kush Himalaya (HKH) region. A multidimensional, contextual and integrated approach has been applied using participatory qualitative tools and techniques to identify major socio-economic drivers and conditions along with climatic factors in upstream, midstream and downstream of the river basins. In upstream and midstream region, people’s livelihood is dependent on subsistent agriculture, horticulture, pastoralism and tourism while in downstream, agriculture and fisheries are the major livelihood options. Climate sensitive natural resources based livelihoods are severely affected across the river basins. Poor and marginal population are not able take adequate adaptation measures due to lack of capacities, poor access to resources, services, information, which push them into greater vulnerability. The vulnerable groups in all four river basins are marginalized sections who are conditioned by economic classes, gender and social norms and living in geographically underdeveloped areas. For instance, poor, women, religious/ ethnic minorities, subordinate caste groups, char dwellers. Poor governance and the lack of access to resources and services have made the situation worse. All these factors are enhancing social vulnerability across the basins and study sites. Social protection measures, enhancement of human capitals and livelihood diversification with pro-poor and gender responsive adaptation and socially inclusive policy are needed to address growing social vulnerability
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Pakistan Agriculture Research Council (PARC) hosted the fourth Climate Change Adaptation Policy & Science (CCAPS) conference from February 26th-27th, 2018 in Islamabad, Pakistan
. CCAPS conference is a series of events held annually by HI-AWARE. The conference aimed to build a platform for adaptation and resilience research and facilitated exchange of knowledge and ideas on science, policy and good practices related to climate change adaptation in the Hindu-Kush Himalayan (HKH) region and especially in Indus-Ganges-Brahmaputra River Basins. The first, second and third CCAPS conferences were held in Kathmandu, Nepal in 2015, Delhi, India in 2016, and Dhaka Bangladesh in 2017 respectively
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This study aims to deepen our understanding about local climate change trends, adaptation approaches and strategies of the government, NGOs, and other actors, and emerging adaptation practices in key impacted sectors in the Lower Teesta basin in Bangladesh
. This region, regarded as one of the important food baskets of the country, has been experiencing varied changes in climate variability (including temperature rises, heat stress, low and erratic rainfall, and prolonged droughts), falling groundwater levels, and climatic extremes such as frequent and devastating floods, riverbank erosion, and thunderstorms. These climate change and other stressors are hurting sectors such as agriculture, water, sanitation and health, fisheries, food security, regional infrastructure, housing, and the livelihoods of common people in general
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The purpose of this study is to present and to validate a research model that includes economic sustainability, social sustainability, environmental sustainability and corporate reputation in the context of public-sector organizations in Pakistan
. The methodological approach is survey-based, using partial least squares structural equation modelling (PLS-SEM) to assess the research model. The proposed hypotheses were tested based on a sample of 425 respondents from public-sector organizations in Pakistan. The findings of the study indicate that there is a positive relationship between economic sustainability, social sustainability, environmental sustainability and corporate reputation. Therefore, it is inferred from the results that different aspects of sustainability can create and enhance the reputation of public-sector organizations
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Groot, A.; Singh, T.; Pandey, A.; Gioli, G.; Ahmed, B.; Ishaq, S.; Raza, N.; Hassan, M.; Hassan, S. M. T.; Syed, M. A.; Mamnun, N.; Eijrond, V.
This resource kit presents a compilation of information on critical climate-stress moments in the Hindu Kush Himalaya (HKH) region
. The information is based on a literature review on critical-climate stress moments in agriculture and health due to heat stress and discusses critical moments emerging from downstream and upstream floods. The literature study was carried out by the Himalayan Adaptation, Water and Resilience (HI-AWARE) research project under the Collaborative Adaptation Research Initiative in Africa and Asia with financial support from the UK Government’s Department for International Development and the International Development Research Centre, Ottawa, Canada
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Ishaq, S.; Ahmad, B.; Kamran, A.; Raza, N.; Khan, M. A.; Virk, Z. T.; Doger, S. S.; Jamil, M. K.; Mustafa, N.; Mahmood, T.; Hassan, M.
This working paper is aimed at finding out the climate change adaptations going on across the three HI-AWARE Project Sites in Indus Basin, namely Hunza (High mountains), Soan Basin (Mid hill) and Chaj Doab ( Flood plains)
. Both autonomous and planned adaptations have been enlisted after thoroughly reviewing published and grey literature. Some focus group discus-sions and key informant interviews were also held in order to know about people experiences, perceptions and existing practices that they are carrying out to sustain their livelihood
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Recession of high-mountain glaciers in response to climatic change frequently results in the development of morainedammed glacial lakes
. Moraine dam failure is often accompanied by the release of large volumes of water and sediment, termed a Glacial Lake Outburst Flood (GLOF). Chukhung Glacier is a small (~3km2) receding valley glacier in Mt. Everest (Sagarmatha) National Park, Nepal. Unlike many Himalayan glaciers, which possess a thick mantle of supraglacial debris, its surface is relatively clean. The glacier terminus has receded 1.3 km from its maximum Holocene position, and in doing so provided the space for an icecontact moraine-dammed lake to develop. The lake had a maximum volume of 5.5 × 105m3 and drained as a result of breaching of the terminal moraine. An estimated 1.3 × 105m3 of material was removed from the terminal moraine during breach development. Numerical dam-breach modelling, implemented within a Generalised Likelihood Uncertainty Estimation (GLUE) framework, was used to investigate a range of moraine-dam failure scenarios. Reconstructed outflow peak discharges, including failure via overtopping and piping mechanisms, are in the range 146-2200m3 s-1. Results from two-dimensional hydrodynamic GLOF modelling indicate that maximum local flow depths may have exceeded 9m, with maximum flow velocities exceeding 20ms-1 within 700m of the breach. The floodwaters mobilised a significant amount of material, sourced mostly from the expanding breach, forming a 300m long and 100m wide debris fan originating at the breach exit. moraine-dam. These results also suggest that inundation of the entire floodplain may have been achieved within ten minutes of initial breach development, suggesting that debris fan development was rapid. We discuss the key glaciological and geomorphological factors that have determined the evolution of a hazardous moraine-dammed lake complex and the subsequent generation of a GLOF and its geomorphological impact
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