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Institution

Nepal Academy of Science and Technology

EducationKathmandu, Nepal
About: Nepal Academy of Science and Technology is a education organization based out in Kathmandu, Nepal. It is known for research contribution in the topics: Climate change & Population. The organization has 187 authors who have published 390 publications receiving 6267 citations. The organization is also known as: Royal Nepal Academy of Science and Technology & NAST.


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Journal ArticleDOI
Moinuddin Ahmed1, Kevin J. Anchukaitis2, Kevin J. Anchukaitis3, Asfawossen Asrat4, H. P. Borgaonkar5, Martina Braida6, Brendan M. Buckley3, Ulf Büntgen7, Brian M. Chase8, Brian M. Chase9, Duncan A. Christie10, Duncan A. Christie11, Edward R. Cook3, Mark A. J. Curran12, Mark A. J. Curran13, Henry F. Diaz14, Jan Esper15, Ze-Xin Fan16, Narayan Prasad Gaire17, Quansheng Ge18, Joelle Gergis19, J. Fidel González-Rouco20, Hugues Goosse21, Stefan W. Grab22, Nicholas E. Graham23, Rochelle Graham23, Martin Grosjean24, Sami Hanhijärvi25, Darrell S. Kaufman26, Thorsten Kiefer, Katsuhiko Kimura27, Atte Korhola25, Paul J. Krusic28, Antonio Lara10, Antonio Lara11, Anne-Marie Lézine29, Fredrik Charpentier Ljungqvist28, Andrew Lorrey30, Jürg Luterbacher31, Valérie Masson-Delmotte29, Danny McCarroll32, Joseph R. McConnell33, Nicholas P. McKay26, Mariano S. Morales34, Andrew D. Moy12, Andrew D. Moy13, Robert Mulvaney35, Ignacio A. Mundo34, Takeshi Nakatsuka36, David J. Nash22, David J. Nash37, Raphael Neukom7, Sharon E. Nicholson38, Hans Oerter39, Jonathan G. Palmer40, Jonathan G. Palmer41, Steven J. Phipps40, María Prieto32, Andrés Rivera42, Masaki Sano36, Mirko Severi43, Timothy M. Shanahan44, Xuemei Shao18, Feng Shi, Michael Sigl33, Jason E. Smerdon3, Olga Solomina45, Eric J. Steig46, Barbara Stenni6, Meloth Thamban47, Valerie Trouet48, Chris S. M. Turney40, Mohammed Umer4, Tas van Ommen12, Tas van Ommen13, Dirk Verschuren49, A. E. Viau50, Ricardo Villalba34, Bo Møllesøe Vinther51, Lucien von Gunten, Sebastian Wagner, Eugene R. Wahl14, Heinz Wanner24, Johannes P. Werner31, James W. C. White52, Koh Yasue53, Eduardo Zorita 
Federal Urdu University1, Woods Hole Oceanographic Institution2, Columbia University3, Addis Ababa University4, Indian Institute of Tropical Meteorology5, University of Trieste6, Swiss Federal Institute for Forest, Snow and Landscape Research7, University of Bergen8, University of Montpellier9, University of Chile10, Austral University of Chile11, Australian Antarctic Division12, University of Tasmania13, National Oceanic and Atmospheric Administration14, University of Mainz15, Xishuangbanna Tropical Botanical Garden16, Nepal Academy of Science and Technology17, Chinese Academy of Sciences18, University of Melbourne19, Complutense University of Madrid20, Université catholique de Louvain21, University of the Witwatersrand22, Hydrologic Research Center23, University of Bern24, University of Helsinki25, Northern Arizona University26, Fukushima University27, Stockholm University28, Université Paris-Saclay29, National Institute of Water and Atmospheric Research30, University of Giessen31, Swansea University32, Desert Research Institute33, National Scientific and Technical Research Council34, British Antarctic Survey35, Nagoya University36, University of Brighton37, Florida State University38, Alfred Wegener Institute for Polar and Marine Research39, University of New South Wales40, University of Exeter41, Centro de Estudios Científicos42, University of Florence43, University of Texas at Austin44, Russian Academy of Sciences45, University of Washington46, National Centre for Antarctic and Ocean Research47, University of Arizona48, Ghent University49, University of Ottawa50, University of Copenhagen51, University of Colorado Boulder52, Shinshu University53
TL;DR: The authors reconstructed past temperatures for seven continental-scale regions during the past one to two millennia and found that the most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late in the nineteenth century.
Abstract: Past global climate changes had strong regional expression To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to two millennia The most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late in the nineteenth century At multi-decadal to centennial scales, temperature variability shows distinctly different regional patterns, with more similarity within each hemisphere than between them There were no globally synchronous multi-decadal warm or cold intervals that define a worldwide Medieval Warm Period or Little Ice Age, but all reconstructions show generally cold conditions between ad 1580 and 1880, punctuated in some regions by warm decades during the eighteenth century The transition to these colder conditions occurred earlier in the Arctic, Europe and Asia than in North America or the Southern Hemisphere regions Recent warming reversed the long-term cooling; during the period ad 1971–2000, the area-weighted average reconstructed temperature was higher than any other time in nearly 1,400 years

885 citations

Journal ArticleDOI
TL;DR: In this article, the cobalt-based metal-organic-frameworks (Co-MOF) was explored as a promising material for supercapacitors and a good pseudocapacitor behavior with the specific capacitance up to 206.76 F ǫ n−1.

315 citations

Journal ArticleDOI
04 Sep 2015-Science
TL;DR: GPS and interferometric synthetic aperture radar data are used to model the earthquake rupture as a slip pulse ~20 kilometers in width, ~6 seconds in duration, and with a peak sliding velocity of 1.1 meters per second, which propagated toward the Kathmandu basin at 3.3 kilometers per second over ~140 kilometers.
Abstract: Detailed geodetic imaging of earthquake ruptures enhances our understanding of earthquake physics and associated ground shaking. The 25 April 2015 moment magnitude 7.8 earthquake in Gorkha, Nepal was the first large continental megathrust rupture to have occurred beneath a high-rate (5-hertz) Global Positioning System (GPS) network. We used GPS and interferometric synthetic aperture radar data to model the earthquake rupture as a slip pulse ~20 kilometers in width, ~6 seconds in duration, and with a peak sliding velocity of 1.1 meters per second, which propagated toward the Kathmandu basin at ~3.3 kilometers per second over ~140 kilometers. The smooth slip onset, indicating a large (~5-meter) slip-weakening distance, caused moderate ground shaking at high frequencies (>1 hertz; peak ground acceleration, ~16% of Earth’s gravity) and minimized damage to vernacular dwellings. Whole-basin resonance at a period of 4 to 5 seconds caused the collapse of tall structures, including cultural artifacts.

312 citations

Journal ArticleDOI
TL;DR: This work estimated population in 195 locations by single year of age and single calendar year from 1950 to 2017 with standardised and replicable methods and used the cohort-component method of population projection, with inputs of fertility, mortality, population, and migration data.

287 citations

Journal ArticleDOI
Julien Emile-Geay1, Nicholas P. McKay2, Darrell S. Kaufman2, Lucien von Gunten, Jianghao Wang3, Kevin J. Anchukaitis4, Nerilie J. Abram5, Jason A. Addison6, Mark A. J. Curran7, Mark A. J. Curran8, Michael N. Evans9, Benjamin J. Henley10, Zhixin Hao, Belen Martrat11, Belen Martrat12, Helen McGregor13, Raphael Neukom14, Gregory T. Pederson6, Barbara Stenni15, Kaustubh Thirumalai16, Johannes P. Werner17, Chenxi Xu18, Dmitry Divine19, Bronwyn C. Dixon10, Joelle Gergis10, Ignacio A. Mundo20, Takeshi Nakatsuka, Steven J. Phipps8, Cody C. Routson2, Eric J. Steig21, Jessica E. Tierney4, Jonathan J. Tyler22, Kathryn Allen10, Nancy A. N. Bertler23, Jesper Björklund24, Brian M. Chase25, Min Te Chen26, Edward R. Cook27, Rixt de Jong14, Kristine L. DeLong28, Daniel A. Dixon29, Alexey A. Ekaykin30, Alexey A. Ekaykin31, Vasile Ersek32, Helena L. Filipsson33, Pierre Francus34, Mandy Freund10, Massimo Frezzotti, Narayan Prasad Gaire35, Narayan Prasad Gaire36, Konrad Gajewski37, Quansheng Ge, Hugues Goosse38, Anastasia Gornostaeva, Martin Grosjean14, Kazuho Horiuchi39, Anne Hormes40, Katrine Husum19, Elisabeth Isaksson19, Selvaraj Kandasamy41, Kenji Kawamura42, Kenji Kawamura43, K. Halimeda Kilbourne9, Nalan Koc19, Guillaume Leduc44, Hans W. Linderholm40, Andrew Lorrey45, Vladimir Mikhalenko46, P. Graham Mortyn47, Hideaki Motoyama43, Andrew D. Moy7, Andrew D. Moy8, Robert Mulvaney48, Philipp Munz49, David J. Nash50, David J. Nash51, Hans Oerter52, Thomas Opel52, Anais Orsi53, Dmitriy V. Ovchinnikov54, Trevor J. Porter55, Heidi A. Roop56, Casey Saenger21, Masaki Sano, David J. Sauchyn38, Krystyna M. Saunders14, Krystyna M. Saunders57, Marit-Solveig Seidenkrantz58, Mirko Severi59, Xuemei Shao, Marie-Alexandrine Sicre60, Michael Sigl61, Kate E. Sinclair, Scott St. George62, Jeannine-Marie St. Jacques63, Jeannine-Marie St. Jacques64, Meloth Thamban65, Udya Kuwar Thapa62, Elizabeth R. Thomas48, Chris S. M. Turney66, Ryu Uemura67, A. E. Viau37, Diana Vladimirova31, Diana Vladimirova30, Eugene R. Wahl68, James W. C. White69, Zicheng Yu70, Jens Zinke71, Jens Zinke72 
University of Southern California1, Northern Arizona University2, MathWorks3, University of Arizona4, Australian National University5, United States Geological Survey6, Australian Antarctic Division7, University of Tasmania8, University of Maryland, College Park9, University of Melbourne10, University of Cambridge11, Spanish National Research Council12, University of Wollongong13, University of Bern14, Ca' Foscari University of Venice15, University of Texas at Austin16, University of Bergen17, Chinese Academy of Sciences18, Norwegian Polar Institute19, National University of Cuyo20, University of Washington21, University of Adelaide22, Victoria University of Wellington23, Swiss Federal Institute for Forest, Snow and Landscape Research24, University of Montpellier25, National Taiwan Ocean University26, Columbia University27, Louisiana State University28, University of Maine29, Saint Petersburg State University30, Arctic and Antarctic Research Institute31, Northumbria University32, Lund University33, Institut national de la recherche scientifique34, Tribhuvan University35, Nepal Academy of Science and Technology36, University of Ottawa37, Université catholique de Louvain38, Hirosaki University39, University of Gothenburg40, Xiamen University41, Japan Agency for Marine-Earth Science and Technology42, National Institute of Polar Research43, Aix-Marseille University44, National Institute of Water and Atmospheric Research45, Russian Academy of Sciences46, Autonomous University of Barcelona47, British Antarctic Survey48, University of Tübingen49, University of Brighton50, University of the Witwatersrand51, Alfred Wegener Institute for Polar and Marine Research52, Université Paris-Saclay53, Sukachev Institute of Forest54, University of Toronto55, University at Buffalo56, Australian Nuclear Science and Technology Organisation57, Aarhus University58, University of Florence59, Pierre-and-Marie-Curie University60, Paul Scherrer Institute61, University of Minnesota62, Concordia University63, University of Regina64, National Centre for Antarctic and Ocean Research65, University of New South Wales66, University of the Ryukyus67, National Oceanic and Atmospheric Administration68, University of Colorado Boulder69, Lehigh University70, Free University of Berlin71, Australian Institute of Marine Science72
TL;DR: A community-sourced database of temperature-sensitive proxy records from the PAGES2k initiative, suited to investigations of global and regional temperature variability over the Common Era, and is shared in the Linked Paleo Data (LiPD) format, including serializations in Matlab, R and Python.
Abstract: Reproducible climate reconstructions of the Common Era (1 CE to present) are key to placing industrial-era warming into the context of natural climatic variability. Here we present a community-sourced database of temperature-sensitive proxy records from the PAGES2k initiative. The database gathers 692 records from 648 locations, including all continental regions and major ocean basins. The records are from trees, ice, sediment, corals, speleothems, documentary evidence, and other archives. They range in length from 50 to 2000 years, with a median of 547 years, while temporal resolution ranges from biweekly to centennial. Nearly half of the proxy time series are significantly correlated with HadCRUT4.2 surface temperature over the period 1850–2014. Global temperature composites show a remarkable degree of coherence between high- and low-resolution archives, with broadly similar patterns across archive types, terrestrial versus marine locations, and screening criteria. The database is suited to investigations of global and regional temperature variability over the Common Era, and is shared in the Linked Paleo Data (LiPD) format, including serializations in Matlab, R and Python.

260 citations


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Performance
Metrics
No. of papers from the Institution in previous years
YearPapers
20231
20228
202146
202039
201929
201821