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Institution

University of Maine

EducationOrono, Maine, United States
About: University of Maine is a education organization based out in Orono, Maine, United States. It is known for research contribution in the topics: Population & Ice sheet. The organization has 8637 authors who have published 16932 publications receiving 590124 citations. The organization is also known as: University of Maine at Orono.


Papers
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Journal ArticleDOI
TL;DR: In this article, a case was made for the stability of the East Antarctic Ice Sheet during Pliocene time from landscape development and surficial sediments in the Dry Valleys sector of the Transantarctic Mountains.
Abstract: A case is made for the stability of the East Antarctic Ice Sheet during Pliocene time from landscape development and surficial sediments in the Dry Valleys sector of the Transantarctic Mountains. T...

203 citations

Journal ArticleDOI
Thomas Lecocq1, Stephen Hicks2, Koen Van Noten1, Kasper van Wijk3, Paula Koelemeijer4, Raphael S. M. De Plaen5, Frédérick Massin6, Gregor Hillers7, Robert E. Anthony8, Maria-Theresia Apoloner9, Mario Arroyo-Solórzano10, Jelle Assink11, Pınar Büyükakpınar12, Pınar Büyükakpınar13, Andrea Cannata14, Andrea Cannata15, Flavio Cannavò14, Sebastián Carrasco16, Corentin Caudron17, Esteban J. Chaves, Dave Cornwell18, David Craig19, Olivier F. C. den Ouden11, Olivier F. C. den Ouden20, Jordi Diaz21, Stefanie Donner22, Christos Evangelidis, Läslo Evers20, Läslo Evers11, Benoit Fauville, Gonzalo A. Fernandez, Dimitrios Giannopoulos23, Steven J. Gibbons24, Társilo Girona25, Bogdan Grecu, Marc Grunberg26, György Hetényi27, Anna Horleston28, Adolfo Inza, Jessica C. E. Irving28, Jessica C. E. Irving29, Mohammadreza Jamalreyhani13, Mohammadreza Jamalreyhani30, Alan L. Kafka31, Mathijs Koymans20, Mathijs Koymans11, C. R. Labedz32, Eric Larose17, Nathaniel J. Lindsey33, Mika McKinnon34, Mika McKinnon35, T. Megies36, Meghan S. Miller37, William G. Minarik38, Louis Moresi37, Victor H. Márquez-Ramírez5, Martin Möllhoff19, Ian M. Nesbitt39, Shankho Niyogi40, Javier Ojeda41, Adrien Oth, Simon Richard Proud42, Jay J. Pulli31, Jay J. Pulli43, Lise Retailleau44, Annukka E. Rintamäki7, Claudio Satriano44, Martha K. Savage45, Shahar Shani-Kadmiel20, Reinoud Sleeman11, Efthimios Sokos46, Klaus Stammler22, Alexander E. Stott2, Shiba Subedi27, Mathilde B. Sørensen47, Taka'aki Taira48, Mar Tapia49, Fatih Turhan12, Ben A. van der Pluijm50, Mark Vanstone, Jérôme Vergne26, Tommi Vuorinen7, Tristram Warren42, Joachim Wassermann36, Han Xiao51 
Royal Observatory of Belgium1, Imperial College London2, University of Auckland3, Royal Holloway, University of London4, National Autonomous University of Mexico5, Swiss Seismological Service6, University of Helsinki7, United States Geological Survey8, Central Institution for Meteorology and Geodynamics9, University of Costa Rica10, Royal Netherlands Meteorological Institute11, Kandilli Observatory and Earthquake Research Institute12, University of Potsdam13, National Institute of Geophysics and Volcanology14, University of Catania15, University of Cologne16, University of Savoy17, King's College, Aberdeen18, Dublin Institute for Advanced Studies19, Delft University of Technology20, Spanish National Research Council21, Institute for Geosciences and Natural Resources22, Mediterranean University23, Norwegian Geotechnical Institute24, University of Alaska Fairbanks25, University of Strasbourg26, University of Lausanne27, University of Bristol28, Princeton University29, University of Tehran30, Boston College31, California Institute of Technology32, Stanford University33, Search for extraterrestrial intelligence34, University of British Columbia35, Ludwig Maximilian University of Munich36, Australian National University37, McGill University38, University of Maine39, University of California, Riverside40, University of Chile41, University of Oxford42, BBN Technologies43, Institut de Physique du Globe de Paris44, Victoria University of Wellington45, University of Patras46, University of Bergen47, University of California, Berkeley48, Institut d'Estudis Catalans49, University of Michigan50, University of California, Santa Barbara51
11 Sep 2020-Science
TL;DR: The 2020 seismic noise quiet period is the longest and most prominent global anthropogenic seismic noise reduction on record and suggests that seismology provides an absolute, real-time estimate of human activities.
Abstract: Human activity causes vibrations that propagate into the ground as high-frequency seismic waves. Measures to mitigate the coronavirus disease 2019 (COVID-19) pandemic caused widespread changes in human activity, leading to a months-long reduction in seismic noise of up to 50%. The 2020 seismic noise quiet period is the longest and most prominent global anthropogenic seismic noise reduction on record. Although the reduction is strongest at surface seismometers in populated areas, this seismic quiescence extends for many kilometers radially and hundreds of meters in depth. This quiet period provides an opportunity to detect subtle signals from subsurface seismic sources that would have been concealed in noisier times and to benchmark sources of anthropogenic noise. A strong correlation between seismic noise and independent measurements of human mobility suggests that seismology provides an absolute, real-time estimate of human activities.

202 citations

Journal ArticleDOI
TL;DR: The Gulf of Maine Coastal Current (GMCC) was investigated from 1998 to 2001 by means of extensive hydrographic surveys, current meter moorings, tracked drifters, and satellite-derived thermal imagery as discussed by the authors.
Abstract: The Gulf of Maine Coastal Current (GMCC), which extends from southern Nova Scotia to Cape Cod Massachusetts, was investigated from 1998 to 2001 by means of extensive hydrographic surveys, current meter moorings, tracked drifters, and satellite-derived thermal imagery. The study focused on two principal branches of the GMCC, the Eastern Maine Coastal Current (EMCC) that extends along the eastern coast of Maine to Penobscot Bay, and the Western Maine Coastal Current (WMCC) that extends westward from Penobscot Bay to Massachusetts Bay. Results confirm that GMCC is primarily a pressure gradient-driven system with both principal branches increasing their transport in the spring and summer due to fresh-water inflows, and flowing southwestward against the mean wind forcing during this period. In the spring and summer the subtidal surface currents in the EMCC range from 0.15 to 0.30 ms 1 while subtidal WMCC currents range from 0.05 to 0.15 ms 1 . The reduction of southwestward transport near Penobscot Bay is accomplished via an offshore veering of a variable portion of the EMCC, some of which recirculates cyclonically within the eastern Gulf of Maine. The degree of summer offshore veering, versus leakage into the WMCC, varied strongly over the three study years, from nearly complete disruption in 1998 to nearly continuous through-flow in 2000. Observations show strong seasonal and interannual variability in both the strength of the GMCC and the degree of connectivity of its principal branches. r 2005 Elsevier Ltd. All rights reserved.

202 citations

Journal ArticleDOI
TL;DR: Formation and accumulation of monitored compounds in hydrolysates is demonstrated to be a function of both the feedstock and pretreatment conditions utilized, which are representative of leading pretreatment processes.
Abstract: A variety of potentially inhibitory degradation products are produced during pretreatment of lignocellulosic biomass. Qualitative and quantitative interrogation of pretreatment hydrolysates is paramount to identifying potential correlations between pretreatment chemistries and microbial inhibition in downstream bioconversion processes. In the present study, corn stover, poplar, and pine feedstocks were pretreated under eight different chemical conditions, which are representative of leading pretreatment processes. Pretreatment processes included: 0.7% H(2)SO(4), 0.07% H(2)SO(4), liquid hot water, neutral buffer solution, aqueous ammonia, lime, lime with oxygen pressurization, and wet oxidation. Forty lignocellulosic degradation products resulting from pretreatment were analyzed using high performance liquid chromatography in combination with UV spectroscopy or tandem mass spectrometry detection (HPLC-PDA-MS/MS) and ion chromatography (IC). Of these compounds, several have been reported to be inhibitory, including furfural, hydroxymethyl furfural, ferulic acid, 3,4-dihydroxybenzaldehyde, syringic acid among others. Formation and accumulation of monitored compounds in hydrolysates is demonstrated to be a function of both the feedstock and pretreatment conditions utilized.

201 citations

Journal ArticleDOI
TL;DR: McLachlan et al. as mentioned in this paper framed the debate around two considerations (perception of risk and confidence in ecological understanding) that can be construed to generate an axis or continuum from scientists who would strongly support assisted migration to those who would oppose it.
Abstract: With global climate change looming large in the public psyche, the recent paper by McLachlan et al. (2007) and its popular accompaniment (Fox 2007) are timely indeed. Of course some conservation biologists will not wish to think about the prospect of actively moving species that are threatened with extinction by climate change. For them this would be almost analogous to handing out placebos in the midst of an epidemic and worse yet, these placebos may have serious unintended consequences if translocated species become invasive. They will probably argue that we should focus almost exclusively on two central roles for conservation biology: (1) facilitating natural range shifts by redoubling efforts to maintain or restore large-scale connectivity (Hunter et al. 1988; Hannah et al. 2002) and (2) working with our fellow environmental professionals to avoid carbon-management solutions that will have unacceptable consequences for biodiversity (e.g., by directing biofuel production away from sites that would involve the conversion of native vegetation into fuel farms; Cook & Beyea 2000). These two roles will be very demanding, but I believe we should allocate a small portion of our attention to the issue of assisted colonization that McLachlan et al. (2007) have brought to the fore. McLachlan et al. propose framing the debate around two considerations—perception of risk and confidence in ecological understanding—that can be construed to generate an axis or continuum from scientists who would strongly support assisted colonization to those who would oppose it. I think it is useful to advance this exercise by considering three issues that can also be construed as continua: species that are more or less acceptable to translocate, sites that are more or less acceptable for receiving translocations, and projects that are more or less acceptable because of their socioeconomic ramifications and feasibility. I have used the term assisted colonization in contrast to assisted migration used by McLachlan et al.

201 citations


Authors

Showing all 8729 results

NameH-indexPapersCitations
Clifford J. Rosen11165547881
Juan S. Bonifacino10830346554
John D. Aber10720448500
Surendra P. Shah9971032832
Charles T. Driscoll9755437355
Samuel Madden9538846424
Lihua Xiao9349532721
Patrick G. Hatcher9140127519
Pedro J. J. Alvarez8937834837
George R. Pettit8984831759
James R. Wilson89127137470
Steven Girvin8636638963
Peter Marler8117422070
Garry R. Buettner8030429273
Paul Andrew Mayewski8042029356
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Performance
Metrics
No. of papers from the Institution in previous years
YearPapers
202332
2022134
2021834
2020756
2019738
2018725