Bibliographies thématiques / East and North-East Himalayas

Littérature scientifique sur le sujet « East and North-East Himalayas »

Auteur : Grafiati
Publié le 18 mai 2024

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Articles de revues sur le sujet "East and North-East Himalayas"

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Bahali, D., M. Sanjappa et S. Rath. « Geographical distribution of Iridaceae in India ». Indian Journal of Forestry 27, no 3 (1 septembre 2004) : 251–56. http://dx.doi.org/10.54207/bsmps1000-2004-4hx573.

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India is represented by only 34 species and 5 varieties under 14 genera of Iridaceae. The wild and naturalised species are distributed in 5 phytogeographical regions, viz., Trans-Himalaya, West Himalaya, Eastern Himalaya, North East India and Western Ghats. The wild species are restricted to the Himalayas. The regionwise, taxonwise and altitudewise distribution of Indian Iridaceae is given in this paper.
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BAKALIN, VADIM, ANNA VILNET, WEN ZHANG MA et KSENIA KLIMOVA. « The differentiation and speciation of Scapania javanica and S. undulata complexes in the Eastern Sino-Himalayas and perimeters for Scapania Sect. Stephania (Scapaniaceae, Hepaticae) ». Phytotaxa 400, no 3 (5 avril 2019) : 123. http://dx.doi.org/10.11646/phytotaxa.400.3.2.

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Three taxa of Scapania with Sino-Himalayan and meta-Himalayan distribution are described as new to science: S. pseudojavanica from the southern portion of the eastern spur of the Tibetan Plateau in southern China and North Vietnam, S. metahimalayana with a disjunct distribution that ranges from Nepal (where its distribution is questionable) to North Vietnam, and S. sichuanica from high elevation in Sichuan in SW China. Each species is morphologically similar to taxa distributed in the more humid and warmer climates of East and South-East amphi-oceanic Asia. The differentiation is presumably the result of recent speciation in the Sino-Himalayas and adjacent lands and the observed differentiation and distribution patterns are in support of the geographic approach in splitting hepatic species. The initial differentiation of these Scapania in sect. Stephania was the specialization into two groups: with brown and colorless gemmae, both being predominantly unicellular.
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Zgorzelski, Marek. « Ladakh and Zanskar ». Miscellanea Geographica 12, no 1 (1 décembre 2006) : 13–24. http://dx.doi.org/10.2478/mgrsd-2006-0002.

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Abstract The Himalayan mountain chain is orographically fragmented, both in the east-west and in the north-south directions. The latter area is characterised by a greater landscape diversity, owing to its zonality and the vertical zonation of both climate and vegetation. In terms of tectonics and orography, and taking into account the prevalent influence of the monsoon and continental climates, the Himalayan mountain system can be divided into two parts – the external arc (southern), that is the Higher (or Great) Himalayas and the internal arc (northern), that is the so-called Trans-Himalayas. Similarly to the external arc of the Himalayas, the post-glacial relief in the Trans-Himalayas is marginal only. It is an area with a prevalence of denudation (nival, frost, gravitation and eolian) processes. Slopes of tectonic valleys or basins, covered with colourful surface deposits rising as high as even two thirds of their altitude, dominate the landscape. The Zanskar ridges and the Ladakh range represent a transitional zone between the Trans-himalayas and Eastern Karakoram.
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SHAH, ZAHIDA, Tabasum Ali et Sabeeha Shafi. « Phytopharmacological review of Bunium persicum (Boiss)B. fedtsch. » Journal of Drug Delivery and Therapeutics 9, no 2 (15 mars 2019) : 458–60. http://dx.doi.org/10.22270/jddt.v9i2.2509.

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Bunium persicum(BOISS)B.Fedtsch belonging to family Apiaceae is native to the region of the limited zones of the West Asia, Kherman and grows to the areas of North Khorasan and Kheraman, East of the Zagros range to Bandar Abbaas and south area of the Albroz range in Iran. It is also found in North western parts of Himalayas. Bunium persicum is found growing naturally in sub-alpine and alpine habitats of North Western Himalayas. It is a perennial herb, dwarf 30cm to tall 80cm and its flowers are small, white in color. Keywords: Bunium persicum, Apiaceae, North-Western Himalayas, Perrenial Herb
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Taye, Ritu Ranjan, Ataur Rahman, Priyabrata Sen, Shimantini Borkataki et Manha Bathari. « Molecular Characterization of Bumble Bees Species from North East Himalayas ». International Journal of Current Microbiology and Applied Sciences 9, no 5 (10 mai 2020) : 2010–16. http://dx.doi.org/10.20546/ijcmas.2020.905.227.

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Yoshida, Toshio, Rinchen Yangzom et David Long. « Dancing Butterflies of the East Himalayas ». Sibbaldia : the International Journal of Botanic Garden Horticulture, no 14 (17 janvier 2017) : 69–96. http://dx.doi.org/10.24823/sibbaldia.2016.193.

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The region from eastern Bhutan to Arunachal Pradesh of India and the adjacent south-eastern Tibet and northern Myanmar seems to be one of the last frontiers not only for Meconopsis hunting but also for other botanical exploration. Although there remain political difficulties for foreigners to approach the unsettled border between India and China, including the famous Tsari valley with its prominently rich flora, which was visited by Frank Ludlow, George Sherriff, Frank Kingdon-Ward and a few other plant hunters before 1950, some botanical and horticultural treasures in this region have gradually been revealed to recent travellers. As a result of examining the photographs taken by these travellers and our own botanical field research in eastern Bhutan in 2014, accompaniedby subsequent herbarium studies, two species new to science are described. The first, from eastern Bhutan and adjacent Arunachal Pradesh and Tibet, has long been cultivated under the names M. grandis or M. grandis GS600, and has recently been described as M. grandis subsp. orientalis (Grey-Wilson, 2010). It is the national flower of Bhutan. However, the type of M. grandis from Sikkim belongs to a species quite distinct from the eastern populations and the latter is now described as a new species, Meconopsis gakyidiana. The second novelty, Meconopsis merakensis,is newly described from eastern Bhutan and adjacent Arunachal Pradesh. In the past this species was confused with the closely allied M. prainiana. The two species are isolated geographically, M.prainiana being found only much further to the north-east, in south-eastern Tibet, including theTsari valley. The title of this article is based on a comparison made by Frank Kingdon-Ward of Meconopsis flowers with butterflies in Tibet (see below).
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Kumar, Susheel, et Nitin Sharma. « The seismicity of central and north-east Himalayan region ». Contributions to Geophysics and Geodesy 49, no 3 (1 septembre 2019) : 265–81. http://dx.doi.org/10.2478/congeo-2019-0014.

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Abstract The Himalayan range extends upto 2400 km arc from Indus river valley in the west to Brahmaputra river valley in the east of India. Due to distinct geological structures of Himalayan seismic belt, seismicity in Himalaya is inhomogeneous. The inhomogeneity in seismicity is responsible for a number of seismic gaps in the Himalayan seismic belt. Thus Iin the present study, we proposed the study of spatial and temporal evolution of seismicity in entire central and north-east Himalayan region by using Gutenberg-Richter relationship. A detailed study on the behavior of natural seismicity in and around the seismic gap regions is carried out. The study region is segmented in four meridional regions (A) 80°E to 83.5°E, (B) 83.5°E to 87.5°E, (C) 87.5°E to 90°E and (D) 90°E to 98°E along with a fixed latitude belt. The homogeneous catalogue with 3 ≤ Mb ≤ 6.5 is used for the spatial and temporal analysis of seismicity in terms of b-value. It is find out that pockets of lower b-values are coinciding over and around stress accumulated regions. The observed low b-value before occurrence of the Nepal earthquake of 25th April, 2015 supports the argument of impending occurrence of moderate to large magnitude earthquake in Sikkim and north-east Himalayan region in future.
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Pang, H., S. Hou, S. Kaspari et P. A. Mayewski. « Influence of regional precipitation patterns on stable isotopes in ice cores from the central Himalayas ». Cryosphere Discussions 7, no 3 (2 mai 2013) : 1871–905. http://dx.doi.org/10.5194/tcd-7-1871-2013.

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Abstract. Several ice cores have been recovered from the Dasuopu Glacier and the East Rongbuk (ER) Glacier in the central Himalayas since the 1990s. Although the distance between the ER and the Dasuopu ice core drilling sites is only ∼125 km, the stable isotopic record (δ18O or δD) of the ER core is interpreted as a precipitation proxy while the Dasuopu core as a temperature proxy. Thus, the climatological significance of the stable isotopic records of these Himalayan ice cores remains a subject of debate. Based on analysis of regional precipitation patterns over the region, we find that the different interpretations of the Dasuopu and Everest isotopic records may not be contradictive. The north–south and west–east seesaws of the Indian Summer Monsoon (ISM) precipitation are primarily responsible for precipitation falling at the ER site, which results in a negative correlation between the ER δ18O or δD record and precipitation amount along the southern slope of the central Himalayas, corresponding to the "amount effect". In addition to the ISM precipitation, non-summer monsoonal precipitation associated with winter westerlies also significantly contributes to precipitation falling at the Dasuopu site, which may cause a positive correlation between the Dasuopu stable isotopic record and temperature, in response to the "temperature effect". Our results have important implications for interpreting the stable isotopic ice core records recovered from different climatological regimes of the Himalayas.
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singh, Devandra, et Dinesh Sharma. « New distribution record of the Greater False Vampire Bat (Megaderma lyra, Geoffroy 1810) from North-Western Himalaya ». Journal of Tropical Life Science 13, no 2 (25 mai 2023) : 377–82. http://dx.doi.org/10.11594/jtls.13.02.16.

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India has been stated to have 10% of the world's total bat's diversity. The present survey was aimed to study the bat species diversity, distribution and activity patterns in north-western Himalayan region of India. Field surveys were conducted and echolocation calls were recorded using bat detector, Echometer touch 2 in Shiwalik ranges of Himalaya. The Greater False Vampire Bat (Megaderma lyra) has a broad distribution range that stretches from south to south east Asia. In India the distribution of the species was mostly recorded from southern subtropical coastal regions and north-eastern subtropical moist evergreen forests. In the present study The Greater False Vampire Bat (Megaderma lyra) has been recorded for the first time from Garhwal region of north-western Himalayas. Greater False Vampire Bat (Megaderma lyra) having long forearm (>6.63 ± 0.03cm) and lengthy ear (>3.66 ± 0.08cm), which is a distinguishable feature of the family Megadermatidae. The peak frequency (FMaxE) of echolocation was recorded as 50.295 ± 9.18 kHz. This frequency was initiated at 108.20 ± 2.51 kHz and terminated at 30.76 ± 1.37 kHz. The call structure recorded was very distinguishable and specific to this family.
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Nikol’skii, Alexander, Elena Vanisova et Konstantin Belovezhets. « Sound signal of the Himalayan marmot in its insular range ». E3S Web of Conferences 265 (2021) : 01006. http://dx.doi.org/10.1051/e3sconf/202126501006.

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The range of Himalayan marmot (Marmota himalayana Hodgson, 1841) has an insular character, as it is limited by ecological and geographical barriers: in the north, northeast and east, these are deserts and the Loess Plateau, in the west - mountain peaks covered with glaciers and rivers, in the south - forests of the southern macro slope of the Himalayas. Only in the northwest of the range there is an ecological corridor. The geographical isolation of populations of marmots provokes the divergence of alarm call, which is one of the obvious genetically determined features. The results of cluster analysis based on a complex of features of the sound signal coincide with the results of analysis using nuclear and mitochondrial DNA. The projection of variability on the structure and history of the landscape contributes to understand the ecological and geographical factors of divergence as the basis for the process of speciation.
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Thèses sur le sujet "East and North-East Himalayas"

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Banerjee, Rajyasree. « Problems and prospects of flori culture in selected regions of East and North-East Himalayas ». Thesis, University of North Bengal, 2017. http://ir.nbu.ac.in/handle/123456789/2589.

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Dalrymple, Nolan. « North-east childhoods : regional identity in children's novels of the North East of England ». Thesis, University of Newcastle Upon Tyne, 2009. http://hdl.handle.net/10443/890.

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This thesis explores how children's writers have participated in the process of representing and constructing the identity of the North East of England. It argues that there exists a dominant North-East aesthetic which has become deeply embedded within British children's fiction, and that several of its key motifs (labour, industry and decline; traditional gender roles and landscape) recur frequently within portrayals of the region in writing for the young. This aesthetic contributes to a perception of the region as both marginal and marginalised, and masks realities about the North East. Following an overview of children's literature set in the region, from the late nineteenth to the early twenty-first centuries, the focus moves to the work of Robert Westall, a major children's writer who was born in Tyneside and set much of h'is fiction within the region. The Westall chapters draw on the Robert Westall Collection at Seven Stories: The Centre for Children's Books. The more recent work of North-East writer David Almond is considered in the closing chapters which also draw on unpublished material and interviews for this thesis. Key works discussed: Robert Westall, Falling into Glory, Fathom Five, The Kingdom by the Sea, The Machine Gunners, A Time of Fire, The Wind Eye, The Watch House; David Almond, Clay, The Fire-Eaters, Heaven Eyes, Kit's Wilderness, My Dad's a Birdman, The Savage, Secret Heart, Skellig.
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Jex, Catherine Nancy. « Speleothem palaeoclimate reconstructions from North East Turkey ». Thesis, University of Birmingham, 2008. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.757605.

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Jordan, Richard William. « Coccolithophorid communities in the North-East Atlantic ». Thesis, University of Surrey, 1988. http://epubs.surrey.ac.uk/814123/.

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Caccolithopliorids are important members of phytoplankton communities in most parts of the world's oceans. The formation, release and flux of the calcite scales (coccoliths) of these organisms over millions of years, has led to sedimentary deposits of great geological significance. The reporting of immense blooms of coccolithophorids by satellite photography and their passible involvement in atmospheric sulphur emissions has emphasised the necessity for further information on their distribution and ecology. During an extensive sampling programme in the N.E. Atlantic, water samples were collected throughout the photic zone at 30 stations. Scanning electron microscopy of filtered water samples enabled coccolithophorid family and species distributions to be compiled. It was found that certain species assemblages could be assigned to distinct biogeographic zones and that these zones closely conformed to the movements of the N. Atlantic surface currents. However, at the Azores Front it was shown that a transitional region existed between the cold and warm water masses, where the flora of each zone could be found. Detailed studies of coccolithophorid vertical distribution has shown that most species can be assigned to discrete depth bands within the euphotic zone. Furthermore, it was noticed that in two species which have no depth preference, the degree of calcification increased with depth. One of these species, E. huxleyi, displayed two ecomorphotypic variants differing in their calcification, size and morphology. During two east to west transects it was noticed that the halocaccolitiiophorid numbers increased towards the Mid-Atlantic Ridge. A number of new species are described and current taxonomic problems reviewed.
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Fantin, Shaneen Rae. « Housing Aboriginal culture in North-East Arnhem Land / ». [St. Lucia, Qld.], 2003. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe17564.pdf.

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Skovsted, Christian B. « The Early Cambrian Fauna of North-East Greenland ». Doctoral thesis, Uppsala University, Department of Earth Sciences, 2003. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-3910.

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Small shelly fossils are common in sediments of Early Cambrian age and include the earliest common representatives of metazoan animals with mineralized hard parts. The group includes fossils of very different morphology, composition and ultrastructure. They seem to represent skeletal remains of numerous animal groups, the biological affinities of which are largely unresolved. However, the wide geographic range of many forms has the potential to enhance biostratigraphic and palaeogeographic resolution in the Early Cambrian.

The late Early Cambrian sequence of North-East Greenland has yielded an assemblage of more than 88 species of small shelly fossils, brachiopods and trilobites, indicative of a middle Dyeran age (Botoman equivalent). The recovered fossils include a number of species that are known from other Early Cambrian palaeocontinents, and particularly strong ties to late Early Cambrian faunas of Australia are documented. The many cosmopolitan taxa thus identified suggests a close juxtaposition of palaeocontinents at this time.

The systematic affinity of many of these small shelly fossils is poorly understood, partly because of their fragmentary nature and poor preservation. However, new data from North-East Greenland improves our understanding of the function and biological affinity of certain taxa. Collections of the problematic fossil Mongolitubulus from North and North-East Greenland exhibit characters indicative of a defensive function as spines of bivalved arthropods, while species of the problematic genus Triplicatella represent the opercula of an unknown tubular shell, probably related to orthothecid hyoliths. The bivalved fossil Mickwitzia from North-East Greenland combines characters of linguliform brachiopods and sclerites of Micrina, a non-bivalved problematic form (halkieriid) from Australia. The combination suggests that Mickwitzia is a stem group brachiopod and strengthens arguments for a halkieriid ancestry of the brachiopod phylum.

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Adderley, William Paul. « Vertisolic soils under agroforestry in north east Nigeria ». Thesis, Bangor University, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.263176.

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Barrow, Anthony. « The North-East coast whale fishery 1750-1850 ». Thesis, Northumbria University, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.328595.

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Pattinson, Sarah N. « Denitrification within riverine systems of north-east England ». Thesis, Durham University, 1999. http://etheses.dur.ac.uk/4558/.

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This study was undertaken to investigate denitrification and nitrous oxide production in sediments and the key environmental factors influencing these within selected river systems of the LOIS (Land-Ocean Interaction Study) area in North-East England and southern Scotland. Seasonal and spatial trends were evident in both environmental and denitrification data measured monthly for 1.5 years along the Swale-Ouse system from source to tidal limits. Denitrification, measured in sediment cores using acetylene inhibition and expressed by unit area of sediment, increased with distance from source down to freshwater tidal limits. Results from a supplementary survey of the freshwater tidal reaches of the Yorkshire Ouse showed a decrease from the tidal limits. Denitrification activity showed a spring (March to May) peak, particularly in the lowland sites. The highest rate (883±134 µmol N m(^-2) h(^-1)) was measured on the River Wiske, a highly eutrophic lowland tributary to the Swale. A high degree of colinearity was evident between environmental variables, although a significant relationship between denitrification, nitrate and temperature was found through multiple regression. For comparison, measurements were made in the less populated Tweed river system. The seasonal and spatial trends evident in both the environmental and denitrification data from the River Tweed, under a more limited sampling programme, were generally consistent with those observed in the Swale-Ouse system. An intensive field investigation of 50 river sites showed that both potential denitrification rate and N(_2)O production in sediment slurries were positively correlated with nitrate water concentration, sediment water content and percentage of fine (<100 µm) sediment particles. An experimental study investigating the kinetic parameters for denitrification, found that sediment cores taken along the Swale-Ouse exhibited a saturation type curve with added nitrate. Apparent affinity and estimates of apparent maximum velocity for mixed populations of denitrifying bacteria showed an increase on moving downstream and were highest on the Wiske.
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Hart, J. K. « The genesis of the North East Norfolk Drift ». Thesis, University of East Anglia, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.379812.

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Livres sur le sujet "East and North-East Himalayas"

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Sharma, A. K. Early man in eastern Himalayas : North-East India and Nepal. New Delhi : Aryan Books International, 1996.

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Lucksom, S. Z. The Orchids of Sikkim and North East Himalaya. Siliguri : S.Z. Lucksom, 2007.

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Crossette, Barbara. So close to heaven : The vanishing Buddhist kingdoms of the Himalayas. New York : A.A. Knopf, 1995.

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Dutta, H. N., et Imotemsu Ao. Eastern Himalayan domestic architecture : With special reference to the North East India. Dimapur, Nagaland : Heritage Publishing House, 2017.

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Indian Institute of Remote Sensing. et India. Dept. of Biotechnology., dir. Biodiversity characterisation at landscape level using satellite remote sensing and geographic information system : North East India, Western Ghats, Western Himalayas and Andaman & Nicobar Islands. Dehradun : Indian Institute of Remote Sensing, Dept. of Space, 2003.

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Edwards, D. M. The marketing of non-timber forest products from the Himalayas : The trade between east Nepal and India.. London : ODI, 1993.

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Sengupta, Sunil. Multilingualism and multilingual communication field in east and north-eastern Himalayan region : A study in the linguistic underdevelopment. Raja-Rammohunpur, Dt. Darjeeling : University of North Bengal, 1990.

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Mukhopadhaya, Gautam. North East, act east. New Delhi : India International Centre, 2017.

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Reutlingen, Kunstverein, Kunststiftung Erich Hauser et Museum Art.Plus (Donaueschingen, Germany), dir. North East. Berlin : Distanz Verlag, 2018.

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Languages of the Himalayas : An ethnolinguistic handbook of the greater Himalayan Region : containing an introduction to the symbiotic theory of language. Leiden : Brill, 2001.

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Chapitres de livres sur le sujet "East and North-East Himalayas"

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Das, Balai Chandra, Suman Deb Barman et Aznarul Islam. « Influence of Neotectonics on Channel Evolution of Kameng River, North–East Himalaya ». Dans Himalayan Neotectonics and Channel Evolution, 397–417. Cham : Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-95435-2_15.

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Singh, Huidrom Birkumar. « Folklore, Traditional Beliefs, Taboo and Practices on Climate and Weather Forecasting by the Meitei Community of Manipur, North East India ». Dans Addressing the Climate Crisis in the Indian Himalayas, 281–91. Cham : Springer Nature Switzerland, 2024. http://dx.doi.org/10.1007/978-3-031-50097-8_11.

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Modak, Kingshuk, Nibedita Guru, Gaurav Mishra et Abhishek Jangir. « AFOLU Sectors of North East India and Their Potential for Soil Carbon Storage ». Dans Soil Carbon Dynamics in Indian Himalayan Region, 171–88. Singapore : Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-99-3303-7_9.

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Nath, Panna Chandra, Arun Jyoti Nath et Ashesh Kumar Das. « Vegetation and Recalcitrant Soil Carbon Recovery Along an Age Chronosequence of Jhum Fallows in North East India ». Dans Soil Carbon Dynamics in Indian Himalayan Region, 235–44. Singapore : Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-99-3303-7_13.

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Bradbury, Dominic. « North East ». Dans 21st Century Houses, 190–201. London : RIBA Publishing, 2022. http://dx.doi.org/10.4324/9781003325864-9.

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Sutherland, D. G., J. E. Gordon, A. M. Hall, J. Jarvis et D. E. Smith. « North-east Scotland ». Dans Quaternary of Scotland, 211–54. Dordrecht : Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-1500-1_8.

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Xie, Lei, et Shaofeng Jia. « North-East Asia ». Dans China's International Transboundary Rivers, 160–82. Abingdon, Oxon ; New York, NY : Routledge, 2018. | Series : Earthscan studies in water resource management : Routledge, 2017. http://dx.doi.org/10.4324/9781315537900-8.

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Bugini, Roberto, et Luisa Folli. « North-east sector ». Dans Building Stones of Milan and Lombardy, 333–80. London : CRC Press, 2023. http://dx.doi.org/10.1201/9781003361022-15.

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Rutter, Owen. « The State of North Borneo ». Dans South East Asia, 282–87. London : Routledge, 2021. http://dx.doi.org/10.4324/9781003101673-25.

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Clark, Robert L. A. « South of North : Carmen and French Nationalisms ». Dans East of West, 187–216. New York : Palgrave Macmillan US, 2000. http://dx.doi.org/10.1007/978-1-349-62624-3_11.

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Actes de conférences sur le sujet "East and North-East Himalayas"

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Siddique, Sabbir, et Faria Sharmin. « Seismic demand assessment for 20km long Elevated Expressway in Chattogram, Bangladesh ». Dans IABSE Congress, New Delhi 2023 : Engineering for Sustainable Development. Zurich, Switzerland : International Association for Bridge and Structural Engineering (IABSE), 2023. http://dx.doi.org/10.2749/newdelhi.2023.0150.

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<p>Bangladesh is surrounded by 2500km long Himalayan Frontal Thrust at North and by Indo-Myanmar Subduction zone at the East. These two fault zones are primary source of many large historic earthquakes that had occurred along the border of Bangladesh extended from North and wrapping East. The Chattogram region of Bangladesh is hilly and experiences frequent smaller earthquake shaking compare to other area of the country.</p><p>The Elevated Expressway (EEW) project being constructed from Airport to Lalkhan Bazar in Chattogram city by Chattogram Development Authority (CDA) is almost 20km long elevated bridge structure made of Concrete and partly of Steel that runs through a much-crowed habitat. Due to scarcity of land at grade, the EEW is supported on single pier thus with no redundancy in Earthquake Resistance System (ERS).</p><p>Bangladesh National Building Code (BNBC) provides only Peak Ground Acceleration (PGA) for 2475 years return period. The Country is divided into four seismic zones with PGA varies from 0.12g to 0.36g. Data required for seismic analysis of a bridge using AASHTO Code requires PGA associated with 1000 years return period, horizontal response spectral acceleration coefficients for different structural periods are not readily available in BNBC. Interpolation of data from only two available data [225yrs. from BNBC/93 and 2475 yrs. from BNBC/2020] may not reflect the correct risk scenario.</p><p>To calculate the seismic risk for EEW Project, Probabilistic Seismic Hazard Analysis [PSHA] was done and compared with the data available in the Code to finalize seismic risk parameters for the EEW Project.</p>
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Wong, Kaufui V., et Sarmad Chaudhry. « Climate Change Aggravates the Energy-Water-Food Nexus ». Dans ASME 2014 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2014. http://dx.doi.org/10.1115/imece2014-36502.

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There are regions in the world experiencing the energy-food-water nexus problems. These regions tend to have high population density, economy that depends on agriculture and climates with lower annual rainfall that may have been adversely affected by climate change. A case in point is the river basin of the Indus. The Indus River is a large and important river running through four countries in East Asia and South Asia: China, India, Afghanistan, and Pakistan. The region is highly dependent on water for both food and energy. The interlinkage of these three components is the cause for the energy-water-food nexus. The difficulty in effectively managing the use of these resources is their very interdependence. For instance, water availability and policies may influence food production, which is governed by agricultural policies, which will further affect energy production from both water and biofuel sources, which will in turn require the usage of water. The situation is further complicated when climate change is taken into account. On the surface, an increase in temperatures would be devastating during the dry season for a region that uses up to 70% of the total land for agriculture. There are predictions that crop production in the region would decrease; the Threedegreeswarmer organization estimated that crop production in the region could decrease by up to 30% come 2050. Unfortunately, the suspected effects of climate change are more than just changes in temperature, precipitation, monsoon patterns, and drought frequencies. A huge concern is the accelerating melting of glaciers in the Himalayas. Some models predict that a global increase in temperature of just 1°C can decrease glacial volume by 50%. The loss of meltwaters from the Himalayan glaciers during the dry season will be crippling for the Indus River and Valley. In a region where up to 90% of accessible water is used for agriculture, there will be an increased strain on food supply. This will further deteriorate the current situation in the region, where almost half of the world’s hungry and undernourished people reside. While the use of hydropower to generate electricity is already many times lower than the potential use, future scarcity of water will limit the potential ability of hydropower to supply energy to people who already experience less than 50% access to electricity. In the current work, suggestions have been put forward to save the increased glacier melt for current and future use where necessary, improve electricity generation efficiency, use sea water for Rankine power cycle cooling and combined cycle cooling, and increase use desalination for drinking water. Energy conservation practices should also be practiced. All of these suggestions must be considered to address the rising issues in the energy-water-food nexus.
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Ralston, William T. « Service overlays on North American standard cellular ». Dans Photonics East '95, sous la direction de Eileen McGrath-Hadwen, Howard S. Babbitt III, Michael L. Gulledge et James Madsen. SPIE, 1996. http://dx.doi.org/10.1117/12.229453.

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Moskowitz, Jean-Paul, Didier Dupre, Claude Andlauer et Philippe Nau. « Singapore North East Line Project ». Dans Eighth International Conference on Automated People Movers. Reston, VA : American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40582(2001)8.

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Willetts, J. M., et R. A. M. Hogarth. « Lekhwair Pilot Waterflood, North Oman ». Dans Middle East Oil Show. Society of Petroleum Engineers, 1987. http://dx.doi.org/10.2118/15761-ms.

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Johnson, H. A. « North Sea Reservoir Simulation : Practical Considerations ». Dans Middle East Oil Show. Society of Petroleum Engineers, 1989. http://dx.doi.org/10.2118/19039-ms.

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Moretti, I., Y. Kerdraon, M. Sami, M. Said et H. Ali. « North-east Western Desert Petroleum System ». Dans 4th EAGE North African/Mediterranean Petroleum and Geosciences Conference and Exhibition Tunis 2009. European Association of Geoscientists & Engineers, 2009. http://dx.doi.org/10.3997/2214-4609.20145832.

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Bony, G., C. Dumazy et G. Lebas. « North East Frigg Articulated Column Behaviour ». Dans Offshore Technology Conference. Offshore Technology Conference, 1987. http://dx.doi.org/10.4043/5543-ms.

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Meling, L. M., et K. A. Lehne. « Description and Interpretation of North Sea Fractured Chalk Formations ». Dans Middle East Oil Show. Society of Petroleum Engineers, 1993. http://dx.doi.org/10.2118/25640-ms.

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Adams, S. J. « Gas Saturation Monitoring in North Oman Reservoir Using a Borehole Gravimeter ». Dans Middle East Oil Show. Society of Petroleum Engineers, 1991. http://dx.doi.org/10.2118/21414-ms.

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Rapports d'organisations sur le sujet "East and North-East Himalayas"

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Jordan, Matthew J. Multilateralism in North East Asia. Fort Belvoir, VA : Defense Technical Information Center, février 2003. http://dx.doi.org/10.21236/ada415621.

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See, Geoffrey K. An East Asian development fund for North Korea ? East Asia Forum, juillet 2010. http://dx.doi.org/10.59425/eabc.1280095227.

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Chakraborty, Debashree. Partition lives on in north-east Indian literature. Sous la direction de Bharat Bhushan et Suzannah Lyons. Monash University, juin 2023. http://dx.doi.org/10.54377/bdba-cca0.

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James, Randal K. The Islamist Challenge in the Middle East and North Africa. Fort Belvoir, VA : Defense Technical Information Center, avril 1996. http://dx.doi.org/10.21236/ada388242.

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Kleffmann, Johanna, Francesca Batault, Juan Armando Torres Munguia, Siobhan O'Neil, Jente Althuis, Rabby Shakur, Anna Hallahan, Hana Salama et Mohammed Coulibaly. Factors Driving Weapons Holding in the North East of Nigeria. UNIDIR, décembre 2023. http://dx.doi.org/10.37559/meac/23/11.

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Schultz, C. A., H. J. Patton et P. Goldstein. Status report of propagation models : Middle East and North Africa (S5.3). Office of Scientific and Technical Information (OSTI), novembre 1995. http://dx.doi.org/10.2172/231386.

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Penning de Vries, F., et S. Ruaysoongnern. Multiple sources of water for multiple purposes in north east Thailand. International Water Management Institute (IWMI), 2010. http://dx.doi.org/10.5337/2010.208.

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Humphrey-Newell, Diane. Henna, Uses of it in the Middle East and North Africa. Portland State University Library, janvier 2000. http://dx.doi.org/10.15760/etd.5450.

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Zeynep, Kaya. Feminist Peace and Security in the Middle East and North Africa. Oxfam, septembre 2020. http://dx.doi.org/10.21201/2020.6478.

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Morang, Andrew, et Jeffrey Melton. Beach Erosion and Sediment Processes Study, North East Marina, Erie County, Pennsylvania. Fort Belvoir, VA : Defense Technical Information Center, juin 2001. http://dx.doi.org/10.21236/ada396033.

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