Proceedings of the Arctic System Science Program All-Hands Workshop
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Nutrient Availability Limits Biological Production in Arctic Sea Ice Melt Ponds
Polar Biol DOI 10.1007/s00300-017-2082-7 ORIGINAL PAPER Nutrient availability limits biological production in Arctic sea ice melt ponds Heidi Louise Sørensen1,2 · Bo Thamdrup1 · Erik Jeppesen2,3,4,7 · Søren Rysgaard2,5,6,7 · Ronnie Nøhr Glud1,2,7,8 Received: 26 February 2016 / Revised: 26 August 2016 / Accepted: 10 January 2017 © The Author(s) 2017. This article is published with open access at Springerlink.com Abstract Every spring and summer melt ponds form at addition compared with their respective controls, with the the surface of polar sea ice and become habitats where bio- largest increase occurring in the enclosures. Separate addi- 3− − logical production may take place. Previous studies report tions of PO4 and NO3 in the enclosures led to interme- a large variability in the productivity, but the causes are diate increases in productivity, suggesting co-limitation of unknown. We investigated if nutrients limit the productiv- nutrients. Bacterial production and the biovolume of cili- ity in these first-year ice melt ponds by adding nutrients to ates, which were the dominant grazers, were positively cor- 3− − 3− three enclosures ([1] PO4 , [2] NO3 , and [3] PO4 and related with primary production, showing a tight coupling − 3− − NO3 ) and one natural melt pond (PO4 and NO3 ), while between primary production and both microbial activity one enclosure and one natural melt pond acted as controls. and ciliate grazing. To our knowledge, this study is the After 7–13 days, Chl a concentrations and cumulative pri- first to ascertain nutrient limitation in melt ponds. We also mary production were between two- and tenfold higher document that the addition of nutrients, although at rela- in the enclosures and natural melt ponds with nutrient tive high concentrations, can stimulate biological produc- tivity at several trophic levels. -
Northern Sea Route Cargo Flows and Infrastructure- Present State And
Northern Sea Route Cargo Flows and Infrastructure – Present State and Future Potential By Claes Lykke Ragner FNI Report 13/2000 FRIDTJOF NANSENS INSTITUTT THE FRIDTJOF NANSEN INSTITUTE Tittel/Title Sider/Pages Northern Sea Route Cargo Flows and Infrastructure – Present 124 State and Future Potential Publikasjonstype/Publication Type Nummer/Number FNI Report 13/2000 Forfatter(e)/Author(s) ISBN Claes Lykke Ragner 82-7613-400-9 Program/Programme ISSN 0801-2431 Prosjekt/Project Sammendrag/Abstract The report assesses the Northern Sea Route’s commercial potential and economic importance, both as a transit route between Europe and Asia, and as an export route for oil, gas and other natural resources in the Russian Arctic. First, it conducts a survey of past and present Northern Sea Route (NSR) cargo flows. Then follow discussions of the route’s commercial potential as a transit route, as well as of its economic importance and relevance for each of the Russian Arctic regions. These discussions are summarized by estimates of what types and volumes of NSR cargoes that can realistically be expected in the period 2000-2015. This is then followed by a survey of the status quo of the NSR infrastructure (above all the ice-breakers, ice-class cargo vessels and ports), with estimates of its future capacity. Based on the estimated future NSR cargo potential, future NSR infrastructure requirements are calculated and compared with the estimated capacity in order to identify the main, future infrastructure bottlenecks for NSR operations. The information presented in the report is mainly compiled from data and research results that were published through the International Northern Sea Route Programme (INSROP) 1993-99, but considerable updates have been made using recent information, statistics and analyses from various sources. -
Misdemeanor Warrant List
SO ST. LOUIS COUNTY SHERIFF'S OFFICE Page 1 of 238 ACTIVE WARRANT LIST Misdemeanor Warrants - Current as of: 09/26/2021 9:45:03 PM Name: Abasham, Shueyb Jabal Age: 24 City: Saint Paul State: MN Issued Date Bail Amount Warrant Type Charge Offense Level 10/05/2020 415 Bench Warrant-fail to appear at a hearing TRAFFIC-9000 Misdemeanor Name: Abbett, Ashley Marie Age: 33 City: Duluth State: MN Issued Date Bail Amount Warrant Type Charge Offense Level 03/09/2020 100 Bench Warrant-fail to appear at a hearing False Pretenses/Swindle/Confidence Game Misdemeanor Name: Abbott, Alan Craig Age: 57 City: Edina State: MN Issued Date Bail Amount Warrant Type Charge Offense Level 09/16/2019 500 Bench Warrant-fail to appear at a hearing Disorderly Conduct Misdemeanor Name: Abney, Johnese Age: 65 City: Duluth State: MN Issued Date Bail Amount Warrant Type Charge Offense Level 10/18/2016 100 Bench Warrant-fail to appear at a hearing Shoplifting Misdemeanor Name: Abrahamson, Ty Joseph Age: 48 City: Duluth State: MN Issued Date Bail Amount Warrant Type Charge Offense Level 10/24/2019 100 Bench Warrant-fail to appear at a hearing Trespass of Real Property Misdemeanor Name: Aden, Ahmed Omar Age: 35 City: State: Issued Date Bail Amount Warrant Type Charge Offense Level 06/02/2016 485 Bench Warrant-fail to appear at a hearing TRAFF/ACC (EXC DUI) Misdemeanor Name: Adkins, Kyle Gabriel Age: 53 City: Duluth State: MN Issued Date Bail Amount Warrant Type Charge Offense Level 02/28/2013 100 Bench Warrant-fail to appear at a hearing False Pretenses/Swindle/Confidence Game Misdemeanor Name: Aguilar, Raul, JR Age: 32 City: Couderay State: WI Issued Date Bail Amount Warrant Type Charge Offense Level 02/17/2016 Bench Warrant-fail to appear at a hearing Driving Under the Influence Misdemeanor Name: Ainsworth, Kyle Robert Age: 27 City: Duluth State: MN Issued Date Bail Amount Warrant Type Charge Offense Level 11/22/2019 100 Bench Warrant-fail to appear at a hearing Theft Misdemeanor ST. -
Palynological Investigations of Miocene Deposits on the New Siberian Archipelago (U.S.S.R.)
ARCTIC VOL. 45, NO.3 (SEPTEMBER 1992) P. 285-294 Palynological Investigationsof Miocene Deposits on the New Siberian Archipelago(U.S.S.R.)’ EUGENE v. ZYRYANOV~ (Received 12 February 1990; accepted in revised form23 January 1992) ABSTRACT. New paleobotanical data (mainly palynological) are reported from Miocene beds of the New Siberian Islands. The palynoflora has a number of distinctive features: the presence of typical hypoarctic forms, the high content taxa representing dark coniferous assemblages and the con- siderable proportion of small-leaved forms. Floristic comparison with the paleofloras of the Beaufort Formation in arctic Canada allows interpreta- tion of the evolution of the Arctic as a landscape region during Miocene-Pliocene time. This paper is a preliminary analysis of the mechanisms of arctic florogenesis. The model of an “adaptive landscape” is considered in relation to the active eustaticdrying of polar shelves. Key words: palynology, U.S.S.R., NewSiberian Islands, Miocene,Arctic, florogenesis RÉSUMÉ. On rapporte de nouvelles données paléobotaniques (principalement palynologiques) venant de couches datant du miocène situées dans l’archipel de la Nouvelle-Sibérie. La palynoflore possède un nombre de caractéristiques particulières, parmi lesquelles, la présence de formes hypoarctiques typiques, la grande quantité de taxons représentant des assemblages de conifires sombres, ainsi qu’une collection considérable de formes à petites feuilles. Une comparaison floristique avec les paléoflores de la formationde Beaufort dans l’Arctique canadien permet d’interpréter I’évolution de l’Arctique en tant que zone peuplée d’espèces végetales durant le miocbne et le pliocène. Cet article est une analyse préliminaire des mécanismes de la genèse de la flore arctique. -
The Future of Continental Scientific Drilling U.S
THE FUTURE OF CONTINENTAL SCIENTIFIC DRILLING U.S. PERSPECTIVE Proceedings of a workshop | June 4-5, 2009 | Denver, Colorado DOSECC WORKSHOP PUBLICATION 1 Front Cover: Basalts and rhyolites of the Snake River Plain at Twin Falls, Idaho. Project Hotspot will explore the interaction of the Yellowstone hotspot with the continental crust by sampling the volcanic rocks underlying the plain. Two 1.5 km holes will penetrate both the surficial basalt and the underlying rhyolite caldera-fill and outflow depos- its. A separate drill hole will explore the paleoclimate record in Pliocene Lake Idaho in the western Snake River Plain. In addition to the understanding of continent-mantle interaction that develops and the paleoclimate data collected, the project will study water-rock interaction, gases emanating from the deeper curst, and the geomicro- biology of the rocks of the plain. Once scientific objectives and set, budgets are developed, and funding is granted, successful implementation of projects requires careful planning, professional on-site staff, appropriate equip- ment, effective logistics, and accurate accounting. Photo by Tony Walton The authors gratefully acknowledge support of the National Science Foundation (NSF EAR 0923056 to The University of Kansas) and DOSECC, Inc. of Salt Lake City, Utah. Anthony W. Walton, University of Kansas, Lawrence, Kansas Kenneth G. Miller, Rutgers University, New Brunswick, N.J. Christian Koeberl, University of Vienna, Vienna, Austria John Shervais, Utah State University, Logan, Utah Steve Colman, University of Minnesota, Duluth, Duluth, Minnesota edited by Cathy Evans. Stephen Hickman, US Geological Survey, Menlo Park, California covers and design by mitch favrow. Will Clyde, University of New Hampshire, Durham, New Hampshire document layout by Pam Lerow and Paula Courtney. -
TRANSIENT LUNAR PHENOMENA: REGULARITY and REALITY Arlin P
The Astrophysical Journal, 697:1–15, 2009 May 20 doi:10.1088/0004-637X/697/1/1 C 2009. The American Astronomical Society. All rights reserved. Printed in the U.S.A. TRANSIENT LUNAR PHENOMENA: REGULARITY AND REALITY Arlin P. S. Crotts Department of Astronomy, Columbia University, Columbia Astrophysics Laboratory, 550 West 120th Street, New York, NY 10027, USA Received 2007 June 27; accepted 2009 February 20; published 2009 April 30 ABSTRACT Transient lunar phenomena (TLPs) have been reported for centuries, but their nature is largely unsettled, and even their existence as a coherent phenomenon is controversial. Nonetheless, TLP data show regularities in the observations; a key question is whether this structure is imposed by processes tied to the lunar surface, or by terrestrial atmospheric or human observer effects. I interrogate an extensive catalog of TLPs to gauge how human factors determine the distribution of TLP reports. The sample is grouped according to variables which should produce differing results if determining factors involve humans, and not reflecting phenomena tied to the lunar surface. Features dependent on human factors can then be excluded. Regardless of how the sample is split, the results are similar: ∼50% of reports originate from near Aristarchus, ∼16% from Plato, ∼6% from recent, major impacts (Copernicus, Kepler, Tycho, and Aristarchus), plus several at Grimaldi. Mare Crisium produces a robust signal in some cases (however, Crisium is too large for a “feature” as defined). TLP count consistency for these features indicates that ∼80% of these may be real. Some commonly reported sites disappear from the robust averages, including Alphonsus, Ross D, and Gassendi. -
This Article Appeared in a Journal Published by Elsevier
(This is a sample cover image for this issue. The actual cover is not yet available at this time.) This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Quaternary Science Reviews 57 (2012) 26e45 Contents lists available at SciVerse ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Mammoth steppe: a high-productivity phenomenon S.A. Zimov a,*, N.S. Zimov a, A.N. Tikhonov b, F.S. Chapin III c a Northeast Science Station, Pacific Institute for Geography, Russian Academy of Sciences, Cherskii 678830, Russia b Zoological Institute, Russian Academy of Sciences, Saint Petersburg 199034, Russia c Institute of Arctic Biology, University of Alaska, Fairbanks, AK 99775, USA article info abstract Article history: At the last deglaciation Earth’s largest biome, mammoth-steppe, vanished. Without knowledge of the Received 11 January 2012 productivity of this ecosystem, the evolution of man and the glacialeinterglacial dynamics of carbon Received in revised form storage in Earth’s main carbon reservoirs cannot be fully understood. -
Nutrient Availability Limits Biological Production in Arctic Sea Ice Melt Ponds
University of Southern Denmark Nutrient availability limits biological production in Arctic sea ice melt ponds Sørensen, Heidi Louise; Thamdrup, Bo; Jeppesen, Erik; Rysgaard, Søren; Glud, Ronnie N. Published in: Polar Biology DOI: 10.1007/s00300-017-2082-7 Publication date: 2017 Document version: Final published version Document license: CC BY Citation for pulished version (APA): Sørensen, H. L., Thamdrup, B., Jeppesen, E., Rysgaard, S., & Glud, R. N. (2017). Nutrient availability limits biological production in Arctic sea ice melt ponds. Polar Biology, 40(8), 1593-1606. https://doi.org/10.1007/s00300-017-2082-7 Go to publication entry in University of Southern Denmark's Research Portal Terms of use This work is brought to you by the University of Southern Denmark. Unless otherwise specified it has been shared according to the terms for self-archiving. If no other license is stated, these terms apply: • You may download this work for personal use only. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying this open access version If you believe that this document breaches copyright please contact us providing details and we will investigate your claim. Please direct all enquiries to [email protected] Download date: 28. Sep. 2021 Polar Biol (2017) 40:1593–1606 DOI 10.1007/s00300-017-2082-7 ORIGINAL PAPER Nutrient availability limits biological production in Arctic sea ice melt ponds Heidi Louise Sørensen1,2 · Bo Thamdrup1 · Erik Jeppesen2,3,4,7 · Søren Rysgaard2,5,6,7 · Ronnie Nøhr Glud1,2,7,8 Received: 26 February 2016 / Revised: 26 August 2016 / Accepted: 10 January 2017 / Published online: 1 March 2017 © The Author(s) 2017. -
Deglacial and Postglacial Evolution of the Pingualuit Crater Lake Basin, Northern Québec (Canada)
Geomorphology 248 (2015) 327–343 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Deglacial and postglacial evolution of the Pingualuit Crater Lake basin, northern Québec (Canada) Pierre-Arnaud Desiage a,b,⁎, Patrick Lajeunesse b,c, Guillaume St-Onge a,b, Alexandre Normandeau b, Grégoire Ledoux c,HervéGuyarda,b,d, Reinhard Pienitz c a Institut des sciences de la mer de Rimouski (ISMER), Canada Research Chair in Marine Geology, Université du Québec à Rimouski, Rimouski, Canada b GEOTOP Research Center, Canada c Centre d'études Nordiques (CEN) & Département de Géographie, Université Laval, Québec, Canada d Institut de Physique du Globe de Paris, Sorbonne Paris Cité, Université Paris Diderot, UMR CNRS 7154, Paris, France article info abstract Article history: The Pingualuit Crater, located in the Ungava Peninsula (northern Québec, Canada) is a 1.4-Ma-old impact crater Received 15 January 2015 hosting a ~245-m-deep lake. The lake has a great potential to preserve unique paleoclimatic and paleoecological Received in revised form 9 July 2015 sedimentary records of the last glacial/interglacial cycles in the terrestrial Canadian Arctic. In order to investigate Accepted 10 July 2015 the stratigraphy in the lake and the late Quaternary glacial history of the Pingualuit Crater, this study compiles Available online 29 July 2015 data from three expeditions carried out in May 2007 (~9-m-long sediment core), in August 2010 (~50 km of seismic lines), and in September 2012 (high-resolution terrestrial LiDAR topography of the inner slopes). Despite Keywords: fi lake levels the weak penetration (~10 m) of the 3.5-kHz subbottom pro ling caused by the presence of boulders in the Mass movements sedimentary column, seismic data coupled with the stratigraphy established from the sediment core enabled Laurentide Ice Sheet the identification of two glaciolacustrine units deposited during the final stages of the Laurentide Ice Sheet Sedimentological processes (LIS) retreat in the crater. -
Reconstruction of Paleoclimate of Russian Arctic in the Late Pleistocene–Holocene on the Basis of Isotope Study of Ice Wedges I.D
Kriosfera Zemli, 2015, vol. XIX, No. 2, pp. 86–94 http://www.izdatgeo.ru RECONSTRUCTION OF PALEOCLIMATE OF RUSSIAN ARCTIC IN THE LATE PLEISTOCENE–HOLOCENE ON THE BASIS OF ISOTOPE STUDY OF ICE WEDGES I.D. Streletskaya1, A.A. Vasiliev2,3, G.E. Oblogov2, I.V. Tokarev4 1 Lomonosov Moscow State University, Department of Geography, 1 Leninskie Gory, Moscow, 119991, Russia; [email protected] 2 Earth Cryosphere Institute, SB RAS, 86 Malygina str., Tyumen, 625000, Russia; [email protected], [email protected] 3 Tyumen State Oil and Gas University, 38 Volodarskogo str., Tyumen, 625000, Russia 4 Resources Center “Geomodel” of Saint-Petersburg State University, 1 Ulyanovskaya str., St. Petersburg, 198504, Russia The results of paleoclimate reconstructions for the Russian Arctic on the basis of the isotope composition (δ18O) of ice wedges have been presented with the attendant analysis of all available data on isotope composition of syngenetic ice wedges with determined geologic age. Spatial distributions of δ18O values in ice wedges and elementary ice veins have been plotted for the present time and for MIS 1, MIS 2, MIS 3, and MIS 4. Trend lines of spatial distribution of δ18O for different time periods are almost parallel. Based on the data on isotope composition of ice wedges of different age, winter paleotemperatures have been reconstructed for the Russian Arctic and their spatial distribution characterized. Paleoclimate, ice wedges, isotope composition, atmospheric transfer INTRODUCTION Over the last decades numerous papers on iso- Laptev Sea region [Derevyagin et al., 2010]. These tope composition of ice wedges and its relation to pa- data allow to expand this range and to adjust Vasil- leo-geographic conditions have been published chuk’s equations for the whole Russian Arctic. -
Water on the Moon, III. Volatiles & Activity
Water on The Moon, III. Volatiles & Activity Arlin Crotts (Columbia University) For centuries some scientists have argued that there is activity on the Moon (or water, as recounted in Parts I & II), while others have thought the Moon is simply a dead, inactive world. [1] The question comes in several forms: is there a detectable atmosphere? Does the surface of the Moon change? What causes interior seismic activity? From a more modern viewpoint, we now know that as much carbon monoxide as water was excavated during the LCROSS impact, as detailed in Part I, and a comparable amount of other volatiles were found. At one time the Moon outgassed prodigious amounts of water and hydrogen in volcanic fire fountains, but released similar amounts of volatile sulfur (or SO2), and presumably large amounts of carbon dioxide or monoxide, if theory is to be believed. So water on the Moon is associated with other gases. Astronomers have agreed for centuries that there is no firm evidence for “weather” on the Moon visible from Earth, and little evidence of thick atmosphere. [2] How would one detect the Moon’s atmosphere from Earth? An obvious means is atmospheric refraction. As you watch the Sun set, its image is displaced by Earth’s atmospheric refraction at the horizon from the position it would have if there were no atmosphere, by roughly 0.6 degree (a bit more than the Sun’s angular diameter). On the Moon, any atmosphere would cause an analogous effect for a star passing behind the Moon during an occultation (multiplied by two since the light travels both into and out of the lunar atmosphere). -
Arctic Report Card 2017
Arctic Report Card 2017 Arctic Report Card 2017 Arctic shows no sign of returning to reliably frozen region of recent past decades 2017 Headlines 2017 Headlines Video Executive Summary Contacts Arctic shows no sign of returning to reliably frozen Vital Signs region of recent past decades Surface Air Temperature Despite relatively cool summer temperatures, Terrestrial Snow Cover observations in 2017 continue to indicate that the Greenland Ice Sheet Arctic environmental system has reached a 'new Sea Ice normal', characterized by long-term losses in the Sea Surface Temperature extent and thickness of the sea ice cover, the extent Arctic Ocean Primary Productivity and duration of the winter snow cover and the mass of ice in the Greenland Ice Sheet and Arctic glaciers, Tundra Greenness and warming sea surface and permafrost Other Indicators temperatures. Terrestrial Permafrost Groundfish Fisheries in the Highlights Eastern Bering Sea Wildland Fire in High Latitudes • The average surface air temperature for the year ending September 2017 is the 2nd warmest since 1900; however, cooler spring and summer temperatures contributed to a rebound in snow cover in the Eurasian Arctic, slower summer sea ice loss, Frostbites and below-average melt extent for the Greenland ice sheet. Paleoceanographic Perspectives • The sea ice cover continues to be relatively young and thin with older, thicker ice comprising only 21% of the ice cover in on Arctic Ocean Change 2017 compared to 45% in 1985. Collecting Environmental • In August 2017, sea surface temperatures in the Barents and Chukchi seas were up to 4° C warmer than average, Intelligence in the New Arctic contributing to a delay in the autumn freeze-up in these regions.