Country Case Study – Nepal

human development, climate change

Preservation of geochemical characteristics in Permo-Triassic mudstones by metagenesis and low-grade metamorphism in the Tethys Himalaya, Central Nepal

Abstract HKT-ISTP 2013 A

Caesarean Section rates in South Asian cities: Can midwifery help stem the rise?

Introduction: Caesarean section (CS) is a life-saving surgical intervention for delivering a baby when complications arisein childbirth. World Health Organization recommends a rate of CS from 10% to 15%. However, CS rates increased steadily in recent decades and have almost doubled from 12.1% in 2000 to 21.1% in 2015. Therefore, this has become a global public health problem. The main purpose of the scoping review article is to give an overview and analysis of the rising CS use in four South Asian countries: Bangladesh, India, Nepal and Pakistan. Methods: A scoping review was carried-out using several bibliographic electronic databases (MEDLINE, EMBASE, SCOPUS, CINAHL and Web of Science), organizational websites and open access journal databases. Literature was searched from December 2011 to December 2018 for articles reporting hospital-based CS rates.Inclusion criteria were primary studies conducted ininstitutional setting in Bangladesh, India, Nepal and Pakistan and published in the English language. Results: We have included 43 studies. Together these studies show that the rate of CS is increasing in all four countries: Nepal, Bangladesh, Pakistan and India. However, this isuneven with very low rates in rural and very high rates in urban settings, theco-existence of ‘Too Little Too Late & Too Much Too Soon’. Hospital based studies have shown that the CS rate is higher in urban and private hospitals. Age, education andsocio-economic status of women, urban residence and distance from health facility are associated with CSs. CS is higher among highlyeducated affluent urban women in private hospitals in South Asian Countries. Conclusion: Rising CS rates in South Asian cities, particularly in specific groups of women, present a challenge to hospital staff and managers and policy-makers. The challenge is to avoid ‘Too Much Too Soon’ in otherwise healthy urban women and avoid ‘Too Little Too Late’ in women living in remote and rural area and in poor urban women

Climate change and the global pattern of moraine-dammed glacial lake outburst floods

This is the author accepted manuscript. The final version is available from EGU via the DOI in this recordThe published version, as published in The Cryosphere, is in ORE: http://hdl.handle.net/10871/32433Despite recent research identifying a clear anthropogenic impact on glacier recession, the effect of recent climate change on glacier-related hazards is at present unclear. Here we present the first global spatio-temporal assessment of glacial lake outburst floods (GLOFs) focusing explicitly on lake drainage following moraine dam failure. These floods occur as mountain glaciers recede and downwaste and many have an enormous impact on downstream communities and infrastructure. Our assessment of GLOFs associated with the collapse of moraine-dammed lakes provides insights into the historical trends of GLOFs and their distributions under current and future global climate change. We observe a clear global increase in GLOF frequency and their regularity around 1930, which likely represents a lagged response to post-Little Ice Age warming. Notably, we also show that GLOF frequency and their regularity – rather unexpectedly – has declined in recent decades even during a time of rapid glacier recession. Although previous studies have suggested that GLOFs will increase in response to climate warming and glacier recession, our global results demonstrate that this has not yet clearly happened. From assessment of the timing of climate forcing, lag times in glacier recession, lake formation and moraine dam failure, we predict increased GLOF frequencies during the next decades and into the 22nd century.SH was funded by a Leverhulme Research Fellowship. SH, RAB and AW acknowledge funding under the HELIX (European Union Seventh Framework Programme FP7/2007-2013 under grant agreement n° 603864). AW and RAB acknowledge funding from the Joint UK DECC/Defra Met Office Hadley Centre Climate Programme (GA01101)

Climate Change and the Global Pattern of Moraine-Dammed Glacial Lake Outburst Floods

Despite recent research identifying a clear anthropogenic impact on glacier recession, the effect of recent climate change on glacier-related hazards is at present unclear. Here we present the first global spatio-temporal assessment of glacial lake outburst floods (GLOFs) focusing explicitly on lake drainage following moraine dam failure. These floods occur as mountain glaciers recede and downwaste. GLOFs can have an enormous impact on downstream communities and infrastructure. Our assessment of GLOFs associated with the rapid drainage of moraine-dammed lakes provides insights into the historical trends of GLOFs and their distributions under current and future global climate change. We observe a clear global increase in GLOF frequency and their regularity around 1930, which likely represents a lagged response to post-Little Ice Age warming. Notably, we also show that GLOF frequency and regularity – rather unexpectedly – have declined in recent decades even during a time of rapid glacier recession. Although previous studies have suggested that GLOFs will increase in response to climate warming and glacier recession, our global results demonstrate that this has not yet clearly happened. From an assessment of the timing of climate forcing, lag times in glacier recession, lake formation and moraine-dam failure, we predict increased GLOF frequencies during the next decades and into the 22nd century

A rockfall-induced glacial lake outburst flood, Upper Barun Valley, Nepal

On April 20, 2017, a flood from the Barun River, Makalu-Barun National Park, eastern Nepal formed a 2&ndash;3-km-long lake at its confluence with the Arun River as a result of blockage by debris. Although the lake drained spontaneously the next day, it caused nationwide concern and triggered emergency responses. We identified the primary flood trigger as a massive rockfall from the northwest face of Saldim Peak (6388&nbsp;m) which fell approximately 570&nbsp;m down to the unnamed glacier above Langmale glacial lake, causing a massive dust cloud and hurricane-force winds. The impact also precipitated an avalanche, carrying blocks of rock and ice up to 5&nbsp;m in diameter that plummeted a further 630&nbsp;m down into Langmale glacial lake, triggering a glacial lake outburst flood (GLOF). The flood carved steep canyons, scoured the river&rsquo;s riparian zone free of vegetation, and deposited sediment, debris, and boulders throughout much of the river channel from the settlement of Langmale to the settlement of Yangle Kharka about 6.5&nbsp;km downstream. Peak discharge was estimated at 4400&thinsp;&plusmn;&thinsp;1800&nbsp;m3&nbsp;s&minus;1, and total flood volume was estimated at 1.3&thinsp;&times;&thinsp;106&nbsp;m3 of water. This study highlights the importance of conducting integrated field studies of recent catastrophic events as soon as possible after they occur, in order to best understand the complexity of their triggering mechanisms, resultant impacts, and risk reduction management options. </div